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Metrics and Delta-Forms in Non-Archimedean Analytic Geometry Klaus Künnemann Universität Regensburg Non-Archimedean Analytic Geometry: Theory and Practice August 24-28, 2015 Papeete

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Page 1: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Metrics and Delta-Forms inNon-Archimedean Analytic Geometry

Klaus Künnemann

Universität Regensburg

Non-Archimedean Analytic Geometry: Theory and PracticeAugust 24-28, 2015 Papeete

Page 2: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Report on joint work with Walter Gubler (Regensburg)

Literature:[GK] Walter Gubler and Klaus Künnemann. A tropical approach

to non-archimedean Arakelov geometry.arXiv:1406.7637

[CD] Antoine Chambert-Loir and Antoine Ducros. Formesdifférentielles réelles et courants sur les espaces deBerkovich. arXiv:1204.6277

[Gu] Walter Gubler: Forms and currents on the analytification ofan algebraic variety (after Chambert–Loir and Ducros).arXiv:1303.7364

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 2 / 29

Page 3: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Report on joint work with Walter Gubler (Regensburg)

Literature:[GK] Walter Gubler and Klaus Künnemann. A tropical approach

to non-archimedean Arakelov geometry.arXiv:1406.7637

[CD] Antoine Chambert-Loir and Antoine Ducros. Formesdifférentielles réelles et courants sur les espaces deBerkovich. arXiv:1204.6277

[Gu] Walter Gubler: Forms and currents on the analytification ofan algebraic variety (after Chambert–Loir and Ducros).arXiv:1303.7364

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 2 / 29

Page 4: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Report on joint work with Walter Gubler (Regensburg)

Literature:[GK] Walter Gubler and Klaus Künnemann. A tropical approach

to non-archimedean Arakelov geometry.arXiv:1406.7637

[CD] Antoine Chambert-Loir and Antoine Ducros. Formesdifférentielles réelles et courants sur les espaces deBerkovich. arXiv:1204.6277

[Gu] Walter Gubler: Forms and currents on the analytification ofan algebraic variety (after Chambert–Loir and Ducros).arXiv:1303.7364

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 2 / 29

Page 5: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Report on joint work with Walter Gubler (Regensburg)

Literature:[GK] Walter Gubler and Klaus Künnemann. A tropical approach

to non-archimedean Arakelov geometry.arXiv:1406.7637

[CD] Antoine Chambert-Loir and Antoine Ducros. Formesdifférentielles réelles et courants sur les espaces deBerkovich. arXiv:1204.6277

[Gu] Walter Gubler: Forms and currents on the analytification ofan algebraic variety (after Chambert–Loir and Ducros).arXiv:1303.7364

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 2 / 29

Page 6: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Table of contents

1 Classical Arakelov theory

2 Tropical geometry and Lagerberg’s superforms

3 Delta-forms and delta-currents

4 First Chern delta-forms

5 Non-archimedean Arakelov theory

6 Positivity properties of metrics (work in progress)

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 3 / 29

Page 7: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Classical Arakelov theory

Let X be a smooth, projective variety over number field K .

Algebraic intersection theory gives geometric informationabout X , e.g. degree of varieties.Arithmetic intersection theory gives arithmetic informationabout X , e.g. heights finiteness results.

dim X = 1: Arakelov, Faltingsdim X ≥ 2: Gillet-Soulé,. . .

Arithmetic intersection numbers can often be localized i.e.they are given as a sum of contributions from thearchimedean and the non-archimedean places of K .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 4 / 29

Page 8: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Classical Arakelov theory

Let X be a smooth, projective variety over number field K .

Algebraic intersection theory gives geometric informationabout X , e.g. degree of varieties.

Arithmetic intersection theory gives arithmetic informationabout X , e.g. heights finiteness results.

dim X = 1: Arakelov, Faltingsdim X ≥ 2: Gillet-Soulé,. . .

Arithmetic intersection numbers can often be localized i.e.they are given as a sum of contributions from thearchimedean and the non-archimedean places of K .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 4 / 29

Page 9: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Classical Arakelov theory

Let X be a smooth, projective variety over number field K .

Algebraic intersection theory gives geometric informationabout X , e.g. degree of varieties.Arithmetic intersection theory gives arithmetic informationabout X , e.g. heights finiteness results.

dim X = 1: Arakelov, Faltingsdim X ≥ 2: Gillet-Soulé,. . .

Arithmetic intersection numbers can often be localized i.e.they are given as a sum of contributions from thearchimedean and the non-archimedean places of K .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 4 / 29

Page 10: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Classical Arakelov theory

Let X be a smooth, projective variety over number field K .

Algebraic intersection theory gives geometric informationabout X , e.g. degree of varieties.Arithmetic intersection theory gives arithmetic informationabout X , e.g. heights finiteness results.

dim X = 1: Arakelov, Faltingsdim X ≥ 2: Gillet-Soulé,. . .

Arithmetic intersection numbers can often be localized i.e.they are given as a sum of contributions from thearchimedean and the non-archimedean places of K .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 4 / 29

Page 11: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .

Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 12: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .

Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 13: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).

Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 14: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)).

Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 15: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.

Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 16: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).

An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 17: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 18: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Basic idea of arithmetic intersection theory

Let OK denote the ring of integers in K .Assume X has a regular, projective model X over Spec OK .Get complex manifold X (C).Algebraic cycle Z ∈ Z p(X ) determines current of integrationδZ ∈ Dp,p(X (C)). Put ddc := −(2πi)−1∂∂.Call gZ ∈ Dp−1,p−1(X (C)) a Green current for Z iff

ddcgZ + δZ = [ωZ ]

for a differential form ωZ ∈ Ap,p(X (C)).An arithmetic cycle (Z,gZ ) is given by a cycle Z on X withgeneric fibre Z and a Green current gZ for Z .

f ∈ K (X )× gives arithmetic cycle div(f ) := (div(f ),− log |f |).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 5 / 29

Page 19: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Arithmetic intersection theoryArithmetic intersection product for (Y,gY ) and (Z,gZ ) suchthat Y intersects Z properly in X is given as

(Z,gZ ) · (Y,gY ) := (Y · Z,gY ∧ δZ + ωY ∧ gZ︸ ︷︷ ︸=:gY ∗gZ

).

Problems:Need proper, regular models (however resolution ofsingularities is often unknown)Canonical heights (e.g. Néron-Tate heights on abelianvarieties) cannot be described as arithmetic intersectionnumbers in the sense above.

Aim of non-archimedean Arakelov theoryUse analytic spaces over Kv for non-archimedean v instead ofmodels and a similar analytic theory of currents.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 6 / 29

Page 20: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Arithmetic intersection theoryArithmetic intersection product for (Y,gY ) and (Z,gZ ) suchthat Y intersects Z properly in X is given as

(Z,gZ ) · (Y,gY ) := (Y · Z,gY ∧ δZ + ωY ∧ gZ︸ ︷︷ ︸=:gY ∗gZ

).

Problems:

Need proper, regular models (however resolution ofsingularities is often unknown)Canonical heights (e.g. Néron-Tate heights on abelianvarieties) cannot be described as arithmetic intersectionnumbers in the sense above.

Aim of non-archimedean Arakelov theoryUse analytic spaces over Kv for non-archimedean v instead ofmodels and a similar analytic theory of currents.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 6 / 29

Page 21: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Arithmetic intersection theoryArithmetic intersection product for (Y,gY ) and (Z,gZ ) suchthat Y intersects Z properly in X is given as

(Z,gZ ) · (Y,gY ) := (Y · Z,gY ∧ δZ + ωY ∧ gZ︸ ︷︷ ︸=:gY ∗gZ

).

Problems:Need proper, regular models (however resolution ofsingularities is often unknown)

Canonical heights (e.g. Néron-Tate heights on abelianvarieties) cannot be described as arithmetic intersectionnumbers in the sense above.

Aim of non-archimedean Arakelov theoryUse analytic spaces over Kv for non-archimedean v instead ofmodels and a similar analytic theory of currents.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 6 / 29

Page 22: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Arithmetic intersection theoryArithmetic intersection product for (Y,gY ) and (Z,gZ ) suchthat Y intersects Z properly in X is given as

(Z,gZ ) · (Y,gY ) := (Y · Z,gY ∧ δZ + ωY ∧ gZ︸ ︷︷ ︸=:gY ∗gZ

).

Problems:Need proper, regular models (however resolution ofsingularities is often unknown)Canonical heights (e.g. Néron-Tate heights on abelianvarieties) cannot be described as arithmetic intersectionnumbers in the sense above.

Aim of non-archimedean Arakelov theoryUse analytic spaces over Kv for non-archimedean v instead ofmodels and a similar analytic theory of currents.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 6 / 29

Page 23: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Arithmetic intersection theoryArithmetic intersection product for (Y,gY ) and (Z,gZ ) suchthat Y intersects Z properly in X is given as

(Z,gZ ) · (Y,gY ) := (Y · Z,gY ∧ δZ + ωY ∧ gZ︸ ︷︷ ︸=:gY ∗gZ

).

Problems:Need proper, regular models (however resolution ofsingularities is often unknown)Canonical heights (e.g. Néron-Tate heights on abelianvarieties) cannot be described as arithmetic intersectionnumbers in the sense above.

Aim of non-archimedean Arakelov theoryUse analytic spaces over Kv for non-archimedean v instead ofmodels and a similar analytic theory of currents.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 6 / 29

Page 24: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Some notions from tropical geometry

Recall that an (integral, R-affine) polyhedron ∆ in Rr is a set

∆ :=N⋂

i=1

ω ∈ Rr

∣∣〈ui , ω〉 ≥ γi, ui ∈ Zr , γi ∈ R.

A polyhedral complex Σ in Rr consists of a finite set Σ ofpolyhedra in Rr such that

∆ ∈ Σ ⇒ every face of ∆ is in Σ,∆,∆′ ∈ Σ ⇒ ∆ ∩∆′ is empty or a face of ∆ and ∆′.

A weighted polyhedral complex (Σ,m) of pure dimension nconsists of a polyhedral complex Σ of pure dimension n anda weight function

m : Σn := ∆ ∈ Σ|dim(∆) = n → Z.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 7 / 29

Page 25: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Some notions from tropical geometry

Recall that an (integral, R-affine) polyhedron ∆ in Rr is a set

∆ :=N⋂

i=1

ω ∈ Rr

∣∣〈ui , ω〉 ≥ γi, ui ∈ Zr , γi ∈ R.

A polyhedral complex Σ in Rr consists of a finite set Σ ofpolyhedra in Rr such that

∆ ∈ Σ ⇒ every face of ∆ is in Σ,∆,∆′ ∈ Σ ⇒ ∆ ∩∆′ is empty or a face of ∆ and ∆′.

A weighted polyhedral complex (Σ,m) of pure dimension nconsists of a polyhedral complex Σ of pure dimension n anda weight function

m : Σn := ∆ ∈ Σ|dim(∆) = n → Z.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 7 / 29

Page 26: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Some notions from tropical geometry

Recall that an (integral, R-affine) polyhedron ∆ in Rr is a set

∆ :=N⋂

i=1

ω ∈ Rr

∣∣〈ui , ω〉 ≥ γi, ui ∈ Zr , γi ∈ R.

A polyhedral complex Σ in Rr consists of a finite set Σ ofpolyhedra in Rr such that

∆ ∈ Σ ⇒ every face of ∆ is in Σ,∆,∆′ ∈ Σ ⇒ ∆ ∩∆′ is empty or a face of ∆ and ∆′.

A weighted polyhedral complex (Σ,m) of pure dimension nconsists of a polyhedral complex Σ of pure dimension n anda weight function

m : Σn := ∆ ∈ Σ|dim(∆) = n → Z.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 7 / 29

Page 27: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Lagerberg’s superforms

Following Lagerberg we define for U ⊆ Rn open

Ap,q(U) := Ap(U)⊗C∞(U) Aq(U) = Ap(U)⊗Z

q∧Zr

bigraded differential alternating algebra (A·,·,d ′,d ′′).

In local coordinates and with multi-index notation

α =∑

|I|=p,|J|=q

fIJd ′xI ∧ d ′′xJ ,

d ′α =r∑

i=1

∑I,J

∂fIJ∂xi

d ′xi ∧ d ′xI ∧ d ′′xJ ,

d ′′α =r∑

j=1

∑I,J

∂fIJ∂xj

d ′′xj ∧ d ′xI ∧ d ′′xJ .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 8 / 29

Page 28: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Lagerberg’s superforms

Following Lagerberg we define for U ⊆ Rn open

Ap,q(U) := Ap(U)⊗C∞(U) Aq(U) = Ap(U)⊗Z

q∧Zr

bigraded differential alternating algebra (A·,·,d ′,d ′′).In local coordinates and with multi-index notation

α =∑

|I|=p,|J|=q

fIJd ′xI ∧ d ′′xJ ,

d ′α =r∑

i=1

∑I,J

∂fIJ∂xi

d ′xi ∧ d ′xI ∧ d ′′xJ ,

d ′′α =r∑

j=1

∑I,J

∂fIJ∂xj

d ′′xj ∧ d ′xI ∧ d ′′xJ .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 8 / 29

Page 29: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical geometry and superforms

Integration of α ∈ An,nc (Rr ) over n-dimensional polyhedron ∆

is well defined current δ∆ ∈ Dn,n(Rr ) =: Dr−n,r−n(Rr )

For a weighted polyhedral complex (Σ,m) of puredimension n current δ(Σ,m) =

∑∆∈Σn

m∆δ∆ ∈ Dn,n(Rr )

A weighted polyhedral complex (Σ,m) is called a tropicalcycle if and only if d ′(δ(Σ,m)) = 0 = d ′′(δ(Σ,m)).(Mikhalkin, Allermann, Rau, ...) There is a well-definedintersection product for tropical cycles on Rr (noequivalence relation is needed).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 9 / 29

Page 30: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical geometry and superforms

Integration of α ∈ An,nc (Rr ) over n-dimensional polyhedron ∆

is well defined current δ∆ ∈ Dn,n(Rr ) =: Dr−n,r−n(Rr )

For a weighted polyhedral complex (Σ,m) of puredimension n current δ(Σ,m) =

∑∆∈Σn

m∆δ∆ ∈ Dn,n(Rr )

A weighted polyhedral complex (Σ,m) is called a tropicalcycle if and only if d ′(δ(Σ,m)) = 0 = d ′′(δ(Σ,m)).(Mikhalkin, Allermann, Rau, ...) There is a well-definedintersection product for tropical cycles on Rr (noequivalence relation is needed).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 9 / 29

Page 31: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical geometry and superforms

Integration of α ∈ An,nc (Rr ) over n-dimensional polyhedron ∆

is well defined current δ∆ ∈ Dn,n(Rr ) =: Dr−n,r−n(Rr )

For a weighted polyhedral complex (Σ,m) of puredimension n current δ(Σ,m) =

∑∆∈Σn

m∆δ∆ ∈ Dn,n(Rr )

A weighted polyhedral complex (Σ,m) is called a tropicalcycle if and only if d ′(δ(Σ,m)) = 0 = d ′′(δ(Σ,m)).

(Mikhalkin, Allermann, Rau, ...) There is a well-definedintersection product for tropical cycles on Rr (noequivalence relation is needed).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 9 / 29

Page 32: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical geometry and superforms

Integration of α ∈ An,nc (Rr ) over n-dimensional polyhedron ∆

is well defined current δ∆ ∈ Dn,n(Rr ) =: Dr−n,r−n(Rr )

For a weighted polyhedral complex (Σ,m) of puredimension n current δ(Σ,m) =

∑∆∈Σn

m∆δ∆ ∈ Dn,n(Rr )

A weighted polyhedral complex (Σ,m) is called a tropicalcycle if and only if d ′(δ(Σ,m)) = 0 = d ′′(δ(Σ,m)).(Mikhalkin, Allermann, Rau, ...) There is a well-definedintersection product for tropical cycles on Rr (noequivalence relation is needed).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 9 / 29

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δ-preforms

DefinitionA current in Dp,q(Rr ) is a δ-preform of type (p,q) if and only if itis of the form

N∑i=1

αi ∧ δCi

with αi ∈ Api ,qi (Rr ) and Ci = (Σi ,mi) tropical cycles ofcodimension ki with (p,q) = (pi + ki ,qi + ki)

Get bigraded differential algebra (P•,•(Rr ),d ′,d ′′), where

(αi ∧ δCi ) ∧ (α′j ∧ δC′j) := (αi ∧ α′j) ∧ δCi ·C′

j

using the tropical intersection product.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 10 / 29

Page 34: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-preforms

DefinitionA current in Dp,q(Rr ) is a δ-preform of type (p,q) if and only if itis of the form

N∑i=1

αi ∧ δCi

with αi ∈ Api ,qi (Rr ) and Ci = (Σi ,mi) tropical cycles ofcodimension ki with (p,q) = (pi + ki ,qi + ki)

Get bigraded differential algebra (P•,•(Rr ),d ′,d ′′), where

(αi ∧ δCi ) ∧ (α′j ∧ δC′j) := (αi ∧ α′j) ∧ δCi ·C′

j

using the tropical intersection product.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 10 / 29

Page 35: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Non-archimedean analytification

From now on, K denotes an algebraically closed fieldcomplete with respect to a non-trivial non-archimedeanabsolute value | | : K → [0,∞) with valuation ring K andresidue class field K .

Let X be a projective variety over K and X an the associatedBerkovich analytic space.For closed subvariety U of a torus T = Gr

m over K , consider

trop : T an −→ Rr , p 7−→ (− log p(t1), . . . ,− log p(tr ))

and put Trop(U) := trop(Uan).

Theorem (Bieri, Groves, Speyer, Sturmfels)Trop(U) has a canonical structure of a tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 11 / 29

Page 36: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Non-archimedean analytification

From now on, K denotes an algebraically closed fieldcomplete with respect to a non-trivial non-archimedeanabsolute value | | : K → [0,∞) with valuation ring K andresidue class field K .Let X be a projective variety over K and X an the associatedBerkovich analytic space.

For closed subvariety U of a torus T = Grm over K , consider

trop : T an −→ Rr , p 7−→ (− log p(t1), . . . ,− log p(tr ))

and put Trop(U) := trop(Uan).

Theorem (Bieri, Groves, Speyer, Sturmfels)Trop(U) has a canonical structure of a tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 11 / 29

Page 37: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Non-archimedean analytification

From now on, K denotes an algebraically closed fieldcomplete with respect to a non-trivial non-archimedeanabsolute value | | : K → [0,∞) with valuation ring K andresidue class field K .Let X be a projective variety over K and X an the associatedBerkovich analytic space.For closed subvariety U of a torus T = Gr

m over K , consider

trop : T an −→ Rr , p 7−→ (− log p(t1), . . . ,− log p(tr ))

and put Trop(U) := trop(Uan).

Theorem (Bieri, Groves, Speyer, Sturmfels)Trop(U) has a canonical structure of a tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 11 / 29

Page 38: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Non-archimedean analytification

From now on, K denotes an algebraically closed fieldcomplete with respect to a non-trivial non-archimedeanabsolute value | | : K → [0,∞) with valuation ring K andresidue class field K .Let X be a projective variety over K and X an the associatedBerkovich analytic space.For closed subvariety U of a torus T = Gr

m over K , consider

trop : T an −→ Rr , p 7−→ (− log p(t1), . . . ,− log p(tr ))

and put Trop(U) := trop(Uan).

Theorem (Bieri, Groves, Speyer, Sturmfels)Trop(U) has a canonical structure of a tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 11 / 29

Page 39: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Very affine open subsets

Let U be an open subset of X .

If U is affine then MU := O(U)×/K× is a free Z-module offinite rank r (Samuel 1966).Put NU = HomZ(MU ,Z) and NU,R = NU ⊗Z R ∼= Rr .Choosing a Z-basis f1, . . . , fr of MU , we obtain (up totranslation in T ) a canonical map

ϕU = (f1, . . . , fr ) : U → Grm = TU = Spec K [MU ].

Call U very affine, if it satisfies the equivalent conditionsU admits closed embedding into a torus,O(U) is generated as a K -algebra by O(U)×,ϕU is a closed embedding.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 12 / 29

Page 40: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Very affine open subsets

Let U be an open subset of X .If U is affine then MU := O(U)×/K× is a free Z-module offinite rank r (Samuel 1966).

Put NU = HomZ(MU ,Z) and NU,R = NU ⊗Z R ∼= Rr .Choosing a Z-basis f1, . . . , fr of MU , we obtain (up totranslation in T ) a canonical map

ϕU = (f1, . . . , fr ) : U → Grm = TU = Spec K [MU ].

Call U very affine, if it satisfies the equivalent conditionsU admits closed embedding into a torus,O(U) is generated as a K -algebra by O(U)×,ϕU is a closed embedding.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 12 / 29

Page 41: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Very affine open subsets

Let U be an open subset of X .If U is affine then MU := O(U)×/K× is a free Z-module offinite rank r (Samuel 1966).Put NU = HomZ(MU ,Z) and NU,R = NU ⊗Z R ∼= Rr .

Choosing a Z-basis f1, . . . , fr of MU , we obtain (up totranslation in T ) a canonical map

ϕU = (f1, . . . , fr ) : U → Grm = TU = Spec K [MU ].

Call U very affine, if it satisfies the equivalent conditionsU admits closed embedding into a torus,O(U) is generated as a K -algebra by O(U)×,ϕU is a closed embedding.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 12 / 29

Page 42: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Very affine open subsets

Let U be an open subset of X .If U is affine then MU := O(U)×/K× is a free Z-module offinite rank r (Samuel 1966).Put NU = HomZ(MU ,Z) and NU,R = NU ⊗Z R ∼= Rr .Choosing a Z-basis f1, . . . , fr of MU , we obtain (up totranslation in T ) a canonical map

ϕU = (f1, . . . , fr ) : U → Grm = TU = Spec K [MU ].

Call U very affine, if it satisfies the equivalent conditionsU admits closed embedding into a torus,O(U) is generated as a K -algebra by O(U)×,ϕU is a closed embedding.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 12 / 29

Page 43: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Very affine open subsets

Let U be an open subset of X .If U is affine then MU := O(U)×/K× is a free Z-module offinite rank r (Samuel 1966).Put NU = HomZ(MU ,Z) and NU,R = NU ⊗Z R ∼= Rr .Choosing a Z-basis f1, . . . , fr of MU , we obtain (up totranslation in T ) a canonical map

ϕU = (f1, . . . , fr ) : U → Grm = TU = Spec K [MU ].

Call U very affine, if it satisfies the equivalent conditionsU admits closed embedding into a torus,O(U) is generated as a K -algebra by O(U)×,ϕU is a closed embedding.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 12 / 29

Page 44: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical chartsVery affine open subsets form basis for Zariski toplogy on X .

DefinitionA tropical chart (V , ϕU) on X consists of

a very affine open subset U of Xan associated closed immersion ϕU : U → TU = Gr

m,an open subset Ω of Trop(U) such that V is the open subsettrop−1

U (Ω) in Uan where

tropU : Uan ϕanU−→ T an = (Gr

m)an trop−→ NU,R = Rr .

Tropical charts form a basis for the topology on X an.Be careful: A tropical chart (V , ϕU) will not give completelocal ’information’ about V !

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 13 / 29

Page 45: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical chartsVery affine open subsets form basis for Zariski toplogy on X .

DefinitionA tropical chart (V , ϕU) on X consists of

a very affine open subset U of Xan associated closed immersion ϕU : U → TU = Gr

m,an open subset Ω of Trop(U) such that V is the open subsettrop−1

U (Ω) in Uan where

tropU : Uan ϕanU−→ T an = (Gr

m)an trop−→ NU,R = Rr .

Tropical charts form a basis for the topology on X an.Be careful: A tropical chart (V , ϕU) will not give completelocal ’information’ about V !

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 13 / 29

Page 46: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical chartsVery affine open subsets form basis for Zariski toplogy on X .

DefinitionA tropical chart (V , ϕU) on X consists of

a very affine open subset U of Xan associated closed immersion ϕU : U → TU = Gr

m,an open subset Ω of Trop(U) such that V is the open subsettrop−1

U (Ω) in Uan where

tropU : Uan ϕanU−→ T an = (Gr

m)an trop−→ NU,R = Rr .

Tropical charts form a basis for the topology on X an.

Be careful: A tropical chart (V , ϕU) will not give completelocal ’information’ about V !

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 13 / 29

Page 47: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Tropical chartsVery affine open subsets form basis for Zariski toplogy on X .

DefinitionA tropical chart (V , ϕU) on X consists of

a very affine open subset U of Xan associated closed immersion ϕU : U → TU = Gr

m,an open subset Ω of Trop(U) such that V is the open subsettrop−1

U (Ω) in Uan where

tropU : Uan ϕanU−→ T an = (Gr

m)an trop−→ NU,R = Rr .

Tropical charts form a basis for the topology on X an.Be careful: A tropical chart (V , ϕU) will not give completelocal ’information’ about V !

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 13 / 29

Page 48: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-forms and δ-currents

DefinitionA δ-form α on X an is given by tropical charts (Vi , ϕUi )i∈I coveringX an and a family α = (α)i∈I where αi ∈ P•,•(NUi ,R) such that

α = α′ ⇔ αi∣∣Vi∩V ′

j= α′j

∣∣Vi∩V ′

jin a tropical sense (see [GK]).

get bigraded differential algebra (B•,•(X an),d ′,d ′′).Topological dual B•,•c (X an) is space of δ-currents E•,•(X an).Observe that no smoothness assumption on X is required.Consider δ-forms as analogs of complex differential formswith logarithmic singularities.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 14 / 29

Page 49: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-forms and δ-currents

DefinitionA δ-form α on X an is given by tropical charts (Vi , ϕUi )i∈I coveringX an and a family α = (α)i∈I where αi ∈ P•,•(NUi ,R) such that

α = α′ ⇔ αi∣∣Vi∩V ′

j= α′j

∣∣Vi∩V ′

jin a tropical sense (see [GK]).

get bigraded differential algebra (B•,•(X an),d ′,d ′′).

Topological dual B•,•c (X an) is space of δ-currents E•,•(X an).Observe that no smoothness assumption on X is required.Consider δ-forms as analogs of complex differential formswith logarithmic singularities.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 14 / 29

Page 50: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-forms and δ-currents

DefinitionA δ-form α on X an is given by tropical charts (Vi , ϕUi )i∈I coveringX an and a family α = (α)i∈I where αi ∈ P•,•(NUi ,R) such that

α = α′ ⇔ αi∣∣Vi∩V ′

j= α′j

∣∣Vi∩V ′

jin a tropical sense (see [GK]).

get bigraded differential algebra (B•,•(X an),d ′,d ′′).Topological dual B•,•c (X an) is space of δ-currents E•,•(X an).

Observe that no smoothness assumption on X is required.Consider δ-forms as analogs of complex differential formswith logarithmic singularities.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 14 / 29

Page 51: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-forms and δ-currents

DefinitionA δ-form α on X an is given by tropical charts (Vi , ϕUi )i∈I coveringX an and a family α = (α)i∈I where αi ∈ P•,•(NUi ,R) such that

α = α′ ⇔ αi∣∣Vi∩V ′

j= α′j

∣∣Vi∩V ′

jin a tropical sense (see [GK]).

get bigraded differential algebra (B•,•(X an),d ′,d ′′).Topological dual B•,•c (X an) is space of δ-currents E•,•(X an).Observe that no smoothness assumption on X is required.

Consider δ-forms as analogs of complex differential formswith logarithmic singularities.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 14 / 29

Page 52: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

δ-forms and δ-currents

DefinitionA δ-form α on X an is given by tropical charts (Vi , ϕUi )i∈I coveringX an and a family α = (α)i∈I where αi ∈ P•,•(NUi ,R) such that

α = α′ ⇔ αi∣∣Vi∩V ′

j= α′j

∣∣Vi∩V ′

jin a tropical sense (see [GK]).

get bigraded differential algebra (B•,•(X an),d ′,d ′′).Topological dual B•,•c (X an) is space of δ-currents E•,•(X an).Observe that no smoothness assumption on X is required.Consider δ-forms as analogs of complex differential formswith logarithmic singularities.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 14 / 29

Page 53: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Smooth forms after Chambert-Loir, DucrosUsing Lagerberg’s superforms and skipping tropical cyclessimilarly smooth (p,q)-forms of Chambert-Loir and Ducros

(see [CD], [Gu]) leading to subalgebra A•,•(X an) of B•,•(X an).

Chambert-Loir, Ducros work more generally on analyticspaces with boundary (no balancing condition is known atthe boundary).Given a tropical chart (V , ϕU), f1, . . . , fm ∈ O(U)× andg : Rm → R smooth, the function

g(− log |f1|, . . . ,− log |fm|) : V → R

is smooth. Not all functions in A0(V ) are of this form!Stone-Weierstraß Theorem (Chambert-Loir, Ducros):A0

c(W ) is dense in C0c (W ) if W is open in X an.

Cohomology of (A0,·(X an),d ′′) computes singularcohomology of X an (Philipp Jell, arXiv:1409.0676).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 15 / 29

Page 54: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Smooth forms after Chambert-Loir, DucrosUsing Lagerberg’s superforms and skipping tropical cyclessimilarly smooth (p,q)-forms of Chambert-Loir and Ducros

(see [CD], [Gu]) leading to subalgebra A•,•(X an) of B•,•(X an).Chambert-Loir, Ducros work more generally on analyticspaces with boundary (no balancing condition is known atthe boundary).

Given a tropical chart (V , ϕU), f1, . . . , fm ∈ O(U)× andg : Rm → R smooth, the function

g(− log |f1|, . . . ,− log |fm|) : V → R

is smooth. Not all functions in A0(V ) are of this form!Stone-Weierstraß Theorem (Chambert-Loir, Ducros):A0

c(W ) is dense in C0c (W ) if W is open in X an.

Cohomology of (A0,·(X an),d ′′) computes singularcohomology of X an (Philipp Jell, arXiv:1409.0676).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 15 / 29

Page 55: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Smooth forms after Chambert-Loir, DucrosUsing Lagerberg’s superforms and skipping tropical cyclessimilarly smooth (p,q)-forms of Chambert-Loir and Ducros

(see [CD], [Gu]) leading to subalgebra A•,•(X an) of B•,•(X an).Chambert-Loir, Ducros work more generally on analyticspaces with boundary (no balancing condition is known atthe boundary).Given a tropical chart (V , ϕU), f1, . . . , fm ∈ O(U)× andg : Rm → R smooth, the function

g(− log |f1|, . . . ,− log |fm|) : V → R

is smooth. Not all functions in A0(V ) are of this form!

Stone-Weierstraß Theorem (Chambert-Loir, Ducros):A0

c(W ) is dense in C0c (W ) if W is open in X an.

Cohomology of (A0,·(X an),d ′′) computes singularcohomology of X an (Philipp Jell, arXiv:1409.0676).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 15 / 29

Page 56: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Smooth forms after Chambert-Loir, DucrosUsing Lagerberg’s superforms and skipping tropical cyclessimilarly smooth (p,q)-forms of Chambert-Loir and Ducros

(see [CD], [Gu]) leading to subalgebra A•,•(X an) of B•,•(X an).Chambert-Loir, Ducros work more generally on analyticspaces with boundary (no balancing condition is known atthe boundary).Given a tropical chart (V , ϕU), f1, . . . , fm ∈ O(U)× andg : Rm → R smooth, the function

g(− log |f1|, . . . ,− log |fm|) : V → R

is smooth. Not all functions in A0(V ) are of this form!Stone-Weierstraß Theorem (Chambert-Loir, Ducros):A0

c(W ) is dense in C0c (W ) if W is open in X an.

Cohomology of (A0,·(X an),d ′′) computes singularcohomology of X an (Philipp Jell, arXiv:1409.0676).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 15 / 29

Page 57: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Smooth forms after Chambert-Loir, DucrosUsing Lagerberg’s superforms and skipping tropical cyclessimilarly smooth (p,q)-forms of Chambert-Loir and Ducros

(see [CD], [Gu]) leading to subalgebra A•,•(X an) of B•,•(X an).Chambert-Loir, Ducros work more generally on analyticspaces with boundary (no balancing condition is known atthe boundary).Given a tropical chart (V , ϕU), f1, . . . , fm ∈ O(U)× andg : Rm → R smooth, the function

g(− log |f1|, . . . ,− log |fm|) : V → R

is smooth. Not all functions in A0(V ) are of this form!Stone-Weierstraß Theorem (Chambert-Loir, Ducros):A0

c(W ) is dense in C0c (W ) if W is open in X an.

Cohomology of (A0,·(X an),d ′′) computes singularcohomology of X an (Philipp Jell, arXiv:1409.0676).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 15 / 29

Page 58: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Integration

Let W be an open subset of X an.

There is a well-defined integral∫

W : Bn,nc (W )→ R.

Every α ∈ Bn,n(W ) induces continuous map

A0c(W ) −→ R, f 7→

∫W

f · α

which extends to continuous map C0c (X )→ R and induces

a signed Borel measure on W (by the Riesz representationTheorem).Get C0

c (W )→ E0,0(W ), f 7→ [f ].

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 16 / 29

Page 59: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Integration

Let W be an open subset of X an.There is a well-defined integral

∫W : Bn,n

c (W )→ R.

Every α ∈ Bn,n(W ) induces continuous map

A0c(W ) −→ R, f 7→

∫W

f · α

which extends to continuous map C0c (X )→ R and induces

a signed Borel measure on W (by the Riesz representationTheorem).Get C0

c (W )→ E0,0(W ), f 7→ [f ].

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 16 / 29

Page 60: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Integration

Let W be an open subset of X an.There is a well-defined integral

∫W : Bn,n

c (W )→ R.Every α ∈ Bn,n(W ) induces continuous map

A0c(W ) −→ R, f 7→

∫W

f · α

which extends to continuous map C0c (X )→ R and induces

a signed Borel measure on W (by the Riesz representationTheorem).

Get C0c (W )→ E0,0(W ), f 7→ [f ].

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 16 / 29

Page 61: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Integration

Let W be an open subset of X an.There is a well-defined integral

∫W : Bn,n

c (W )→ R.Every α ∈ Bn,n(W ) induces continuous map

A0c(W ) −→ R, f 7→

∫W

f · α

which extends to continuous map C0c (X )→ R and induces

a signed Borel measure on W (by the Riesz representationTheorem).Get C0

c (W )→ E0,0(W ), f 7→ [f ].

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 16 / 29

Page 62: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Metrics on line bundles

Let L be a line bundle on X .

Fix an open covering (Ui)i∈I of X , a family (si)i∈I of framessi ∈ Γ(Ui ,L), and the 1-cocyle (hij)ij determined by sj = hijsi .A (continuous) metric ‖ ‖ on L is given by a family (ρi)i ofcontinuous functions ρi : Uan

i → R such that ρj = |hij | · ρi onUan

i ∩ Uanj for all i , j ∈ I.

Let W ⊆ X an be open. Given sections s ∈ Γ(W ,Lan), themetric ‖ ‖ determines continuous functions

‖s‖ : X an −→ R

such that ‖si‖ = ρi .

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Metrics on line bundles

Let L be a line bundle on X .Fix an open covering (Ui)i∈I of X , a family (si)i∈I of framessi ∈ Γ(Ui ,L), and the 1-cocyle (hij)ij determined by sj = hijsi .

A (continuous) metric ‖ ‖ on L is given by a family (ρi)i ofcontinuous functions ρi : Uan

i → R such that ρj = |hij | · ρi onUan

i ∩ Uanj for all i , j ∈ I.

Let W ⊆ X an be open. Given sections s ∈ Γ(W ,Lan), themetric ‖ ‖ determines continuous functions

‖s‖ : X an −→ R

such that ‖si‖ = ρi .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 17 / 29

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Metrics on line bundles

Let L be a line bundle on X .Fix an open covering (Ui)i∈I of X , a family (si)i∈I of framessi ∈ Γ(Ui ,L), and the 1-cocyle (hij)ij determined by sj = hijsi .A (continuous) metric ‖ ‖ on L is given by a family (ρi)i ofcontinuous functions ρi : Uan

i → R such that ρj = |hij | · ρi onUan

i ∩ Uanj for all i , j ∈ I.

Let W ⊆ X an be open. Given sections s ∈ Γ(W ,Lan), themetric ‖ ‖ determines continuous functions

‖s‖ : X an −→ R

such that ‖si‖ = ρi .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 17 / 29

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Metrics on line bundles

Let L be a line bundle on X .Fix an open covering (Ui)i∈I of X , a family (si)i∈I of framessi ∈ Γ(Ui ,L), and the 1-cocyle (hij)ij determined by sj = hijsi .A (continuous) metric ‖ ‖ on L is given by a family (ρi)i ofcontinuous functions ρi : Uan

i → R such that ρj = |hij | · ρi onUan

i ∩ Uanj for all i , j ∈ I.

Let W ⊆ X an be open. Given sections s ∈ Γ(W ,Lan), themetric ‖ ‖ determines continuous functions

‖s‖ : X an −→ R

such that ‖si‖ = ρi .

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First Chern delta-current

Let L be line bundle on X and ‖ ‖ continuous metric on Lan.

For a local frame s of L over an open subset U of X ,

[c1(L, ‖ ‖)] := d ′d ′′ [− log ‖s‖] ∈ E1,1(Uan)

is a δ-current independent of the choice s.By partition of unity argument, we get a well-definedδ-current [c1(L, ‖ ‖)] called the first Chern δ-current.

Similarly as in [CD], we get

Poincaré-Lelong formula

d ′d ′′ [− log ‖s‖] + δdiv(s) = [c1(L, ‖ ‖)] in E1,1(X an)

for any meromorphic section s of L over X .

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First Chern delta-current

Let L be line bundle on X and ‖ ‖ continuous metric on Lan.For a local frame s of L over an open subset U of X ,

[c1(L, ‖ ‖)] := d ′d ′′ [− log ‖s‖] ∈ E1,1(Uan)

is a δ-current independent of the choice s.

By partition of unity argument, we get a well-definedδ-current [c1(L, ‖ ‖)] called the first Chern δ-current.

Similarly as in [CD], we get

Poincaré-Lelong formula

d ′d ′′ [− log ‖s‖] + δdiv(s) = [c1(L, ‖ ‖)] in E1,1(X an)

for any meromorphic section s of L over X .

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First Chern delta-current

Let L be line bundle on X and ‖ ‖ continuous metric on Lan.For a local frame s of L over an open subset U of X ,

[c1(L, ‖ ‖)] := d ′d ′′ [− log ‖s‖] ∈ E1,1(Uan)

is a δ-current independent of the choice s.By partition of unity argument, we get a well-definedδ-current [c1(L, ‖ ‖)] called the first Chern δ-current.

Similarly as in [CD], we get

Poincaré-Lelong formula

d ′d ′′ [− log ‖s‖] + δdiv(s) = [c1(L, ‖ ‖)] in E1,1(X an)

for any meromorphic section s of L over X .

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First Chern delta-current

Let L be line bundle on X and ‖ ‖ continuous metric on Lan.For a local frame s of L over an open subset U of X ,

[c1(L, ‖ ‖)] := d ′d ′′ [− log ‖s‖] ∈ E1,1(Uan)

is a δ-current independent of the choice s.By partition of unity argument, we get a well-definedδ-current [c1(L, ‖ ‖)] called the first Chern δ-current.

Similarly as in [CD], we get

Poincaré-Lelong formula

d ′d ′′ [− log ‖s‖] + δdiv(s) = [c1(L, ‖ ‖)] in E1,1(X an)

for any meromorphic section s of L over X .

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).

Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .

Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .

Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 19 / 29

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.

Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 19 / 29

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.

Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 19 / 29

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 19 / 29

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Smooth and algebraic metrics

A metric ‖ ‖ on L is called smooth if and only if− log ‖s‖ ∈ A0,0(U) for any local frame s ∈ Γ(U,L).Let K = valuation ring of K .Let X be a proper flat model of X over Spec K .Let L be a line bundle on X with isomorphism L|X = L.Get a unique continuous metric ‖ ‖L on L such that localframes s of L over X satisfy ‖s‖L = 1.Such a metric is called an algebraic metric.In a similar way get formal metrics from formal models.

Problem: Algebraic and formal metrics are not always smooth!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 19 / 29

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.Smooth metrics are δ-metrics.Algebraic metrics are δ-metrics.Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.

Smooth metrics are δ-metrics.Algebraic metrics are δ-metrics.Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.Smooth metrics are δ-metrics.

Algebraic metrics are δ-metrics.Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.Smooth metrics are δ-metrics.Algebraic metrics are δ-metrics.

Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.Smooth metrics are δ-metrics.Algebraic metrics are δ-metrics.Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).

Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Delta-metrics

DefinitionA δ-metric on L is a piecewise smooth metric ‖ ‖ such that theδ-current [c1(L, ‖ ‖)] is represented in an functorial way by aδ-form c1(L, ‖ ‖).

δ-metrics are stable under tensor products and pullback.Smooth metrics are δ-metrics.Algebraic metrics are δ-metrics.Canonical metrics on line bundles over abelian varieties areδ-metrics (use Mumford’s non-archimedean uniformizationof abelian varieties).Canonical metrics on line bundles algebraically equivalentto zero are δ-metrics.

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Measures associated with metrized linebundles

Chambert-Loir measure: Let X be projective and ‖ ‖L analgebraic metric on Lan given by (X,L) such that the specialfibre Xs is reduced.

There is a unique (discrete) measure µon X an such that the projection formula holds and

µ =∑

Y

degL(Y )δξY

where Y ranges over the irreducible components of Xs andξY is the unique point of X an whose reduction is the genericpoint of Y .Monge-Ampère measure: Let ‖ ‖ be a δ-metric on Lan, i.e.c1(L, ‖ ‖) is a δ-form. Then c1(L, ‖ ‖)∧n ∈ Bn,n(X an) and itinduces a measure on X an.

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Measures associated with metrized linebundles

Chambert-Loir measure: Let X be projective and ‖ ‖L analgebraic metric on Lan given by (X,L) such that the specialfibre Xs is reduced. There is a unique (discrete) measure µon X an such that the projection formula holds and

µ =∑

Y

degL(Y )δξY

where Y ranges over the irreducible components of Xs andξY is the unique point of X an whose reduction is the genericpoint of Y .

Monge-Ampère measure: Let ‖ ‖ be a δ-metric on Lan, i.e.c1(L, ‖ ‖) is a δ-form. Then c1(L, ‖ ‖)∧n ∈ Bn,n(X an) and itinduces a measure on X an.

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Measures associated with metrized linebundles

Chambert-Loir measure: Let X be projective and ‖ ‖L analgebraic metric on Lan given by (X,L) such that the specialfibre Xs is reduced. There is a unique (discrete) measure µon X an such that the projection formula holds and

µ =∑

Y

degL(Y )δξY

where Y ranges over the irreducible components of Xs andξY is the unique point of X an whose reduction is the genericpoint of Y .Monge-Ampère measure: Let ‖ ‖ be a δ-metric on Lan, i.e.c1(L, ‖ ‖) is a δ-form. Then c1(L, ‖ ‖)∧n ∈ Bn,n(X an) and itinduces a measure on X an.

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Chambert-Loir measure = Monge-AmpèremeasureLet (L, ‖ ‖) be an algebraic metric.

Theorem (GK)Chambert-Loir measure = Monge-Ampère measure c1(L, ‖ ‖)∧n.

A variant of this following Theorem was proved before byChambert-Loir and Ducros.

Difference to [CD]:Chambert-Loir and Ducros use an approximation processby smooth metrics as in Bedford-Taylor theory to define[c1(L, ‖ ‖)]∧n as a wedge product of currents.We obtain c1(L, ‖ ‖)∧n directly as a wedge product ofδ-forms. This simplifies the proof.

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Chambert-Loir measure = Monge-AmpèremeasureLet (L, ‖ ‖) be an algebraic metric.

Theorem (GK)Chambert-Loir measure = Monge-Ampère measure c1(L, ‖ ‖)∧n.

A variant of this following Theorem was proved before byChambert-Loir and Ducros.

Difference to [CD]:Chambert-Loir and Ducros use an approximation processby smooth metrics as in Bedford-Taylor theory to define[c1(L, ‖ ‖)]∧n as a wedge product of currents.We obtain c1(L, ‖ ‖)∧n directly as a wedge product ofδ-forms. This simplifies the proof.

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Non-archimedean Arakelov theoryLet X be (as before) a projective variety over K of dimension n.

DefinitionA δ-current gZ ∈ Ep−1,p−1(X an) is called a Green current for acycle Z ∈ Z p(X ) :⇔

d ′d ′′gZ + δZ = [ωZ ]

holds for some δ-form ω(Z ,gZ ) := ωZ ∈ Bp,p(X an).

Let (L, ‖ ‖) be a line bundle with a δ-metric.Let s be a meromorphic section of L over X with Weildivisor D = div (s).Poincaré-Lelong equation⇒ gD = [− log ‖s‖] ∈ E1,1(X an)is a Green current for D with ωD = c1(L, ‖ ‖).

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Non-archimedean Arakelov theoryLet X be (as before) a projective variety over K of dimension n.

DefinitionA δ-current gZ ∈ Ep−1,p−1(X an) is called a Green current for acycle Z ∈ Z p(X ) :⇔

d ′d ′′gZ + δZ = [ωZ ]

holds for some δ-form ω(Z ,gZ ) := ωZ ∈ Bp,p(X an).

Let (L, ‖ ‖) be a line bundle with a δ-metric.Let s be a meromorphic section of L over X with Weildivisor D = div (s).Poincaré-Lelong equation⇒ gD = [− log ‖s‖] ∈ E1,1(X an)is a Green current for D with ωD = c1(L, ‖ ‖).

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Non-archimedean Arakelov theoryLet X be (as before) a projective variety over K of dimension n.

DefinitionA δ-current gZ ∈ Ep−1,p−1(X an) is called a Green current for acycle Z ∈ Z p(X ) :⇔

d ′d ′′gZ + δZ = [ωZ ]

holds for some δ-form ω(Z ,gZ ) := ωZ ∈ Bp,p(X an).

Let (L, ‖ ‖) be a line bundle with a δ-metric.

Let s be a meromorphic section of L over X with Weildivisor D = div (s).Poincaré-Lelong equation⇒ gD = [− log ‖s‖] ∈ E1,1(X an)is a Green current for D with ωD = c1(L, ‖ ‖).

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Non-archimedean Arakelov theoryLet X be (as before) a projective variety over K of dimension n.

DefinitionA δ-current gZ ∈ Ep−1,p−1(X an) is called a Green current for acycle Z ∈ Z p(X ) :⇔

d ′d ′′gZ + δZ = [ωZ ]

holds for some δ-form ω(Z ,gZ ) := ωZ ∈ Bp,p(X an).

Let (L, ‖ ‖) be a line bundle with a δ-metric.Let s be a meromorphic section of L over X with Weildivisor D = div (s).

Poincaré-Lelong equation⇒ gD = [− log ‖s‖] ∈ E1,1(X an)is a Green current for D with ωD = c1(L, ‖ ‖).

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Non-archimedean Arakelov theoryLet X be (as before) a projective variety over K of dimension n.

DefinitionA δ-current gZ ∈ Ep−1,p−1(X an) is called a Green current for acycle Z ∈ Z p(X ) :⇔

d ′d ′′gZ + δZ = [ωZ ]

holds for some δ-form ω(Z ,gZ ) := ωZ ∈ Bp,p(X an).

Let (L, ‖ ‖) be a line bundle with a δ-metric.Let s be a meromorphic section of L over X with Weildivisor D = div (s).Poincaré-Lelong equation⇒ gD = [− log ‖s‖] ∈ E1,1(X an)is a Green current for D with ωD = c1(L, ‖ ‖).

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The star product of Green currents

Let Z ∈ Z p(X ) be a prime cycle with a Green current gZ .

Let s be meromorphic section of line bundle (L, ‖ ‖) withδ-metric such that D = div (s) intersects Z properly.

Another application of the Poincaré-Lelong formula gives:

Proposition [GK]If D intersects Z property, then

gD ∗ gZ := gD ∧ δZ + c1(L, ‖ ‖) ∧ gZ

is a Green current for the intersection D · Z ∈ Z p+1(X ) with

ω(D · Z ,gD ∗ gZ ) = ω(D,gD) ∧ ω(Z ,gZ ).

The ∗-product is commutative modulo Im (d ′) + Im (d ′′).

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The star product of Green currents

Let Z ∈ Z p(X ) be a prime cycle with a Green current gZ .Let s be meromorphic section of line bundle (L, ‖ ‖) withδ-metric such that D = div (s) intersects Z properly.

Another application of the Poincaré-Lelong formula gives:

Proposition [GK]If D intersects Z property, then

gD ∗ gZ := gD ∧ δZ + c1(L, ‖ ‖) ∧ gZ

is a Green current for the intersection D · Z ∈ Z p+1(X ) with

ω(D · Z ,gD ∗ gZ ) = ω(D,gD) ∧ ω(Z ,gZ ).

The ∗-product is commutative modulo Im (d ′) + Im (d ′′).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 24 / 29

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The star product of Green currents

Let Z ∈ Z p(X ) be a prime cycle with a Green current gZ .Let s be meromorphic section of line bundle (L, ‖ ‖) withδ-metric such that D = div (s) intersects Z properly.

Another application of the Poincaré-Lelong formula gives:

Proposition [GK]If D intersects Z property, then

gD ∗ gZ := gD ∧ δZ + c1(L, ‖ ‖) ∧ gZ

is a Green current for the intersection D · Z ∈ Z p+1(X ) with

ω(D · Z ,gD ∗ gZ ) = ω(D,gD) ∧ ω(Z ,gZ ).

The ∗-product is commutative modulo Im (d ′) + Im (d ′′).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 24 / 29

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The star product of Green currents

Let Z ∈ Z p(X ) be a prime cycle with a Green current gZ .Let s be meromorphic section of line bundle (L, ‖ ‖) withδ-metric such that D = div (s) intersects Z properly.

Another application of the Poincaré-Lelong formula gives:

Proposition [GK]If D intersects Z property, then

gD ∗ gZ := gD ∧ δZ + c1(L, ‖ ‖) ∧ gZ

is a Green current for the intersection D · Z ∈ Z p+1(X ) with

ω(D · Z ,gD ∗ gZ ) = ω(D,gD) ∧ ω(Z ,gZ ).

The ∗-product is commutative modulo Im (d ′) + Im (d ′′).

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 24 / 29

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Local heights

Definition: Let D0, . . . ,Dn be Cartier divisors intersectingproperly on X . Let O(D0), . . . ,O(Dn) be equipped with δ-metrics‖ ‖i and associated Green currents gDi = [− log ‖sDi‖i ] then

λ(X ) := 〈gD0 ∗ · · · ∗ gDn ,1〉

is called the local height of X .

Theorem (GK)If we use algebraic metrics on O(D0), . . . ,O(Dn), then λ(X ) isthe usual local height of X in arithmetic geometry given as theintersection number of the Cartier divisors on a correspondingmodel.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 25 / 29

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Local heights

Definition: Let D0, . . . ,Dn be Cartier divisors intersectingproperly on X . Let O(D0), . . . ,O(Dn) be equipped with δ-metrics‖ ‖i and associated Green currents gDi = [− log ‖sDi‖i ] then

λ(X ) := 〈gD0 ∗ · · · ∗ gDn ,1〉

is called the local height of X .

Theorem (GK)If we use algebraic metrics on O(D0), . . . ,O(Dn), then λ(X ) isthe usual local height of X in arithmetic geometry given as theintersection number of the Cartier divisors on a correspondingmodel.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 25 / 29

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Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.

Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 100: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ).

They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 101: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.

This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 102: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.

A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 103: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 104: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 105: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Positive forms and plurisubharmonic metrics

Let W be open in X an and ‖ ‖ a continuous metric on Lan.Chambert-Loir, Ducros define cones of positive elements inAp,p(W ) and Dp,p(W ). They call ‖ ‖ psh if [c1(L, ‖| ‖)] inD1,1(W ) is positive.This extends to Bp,p(W ) and Ep,p(W )⇒ δ-psh metrics.A formal metric ‖ ‖ on Lan is called semipositive in x ∈ X an ifx has a neighbourhood V in X an such that

(i) V is a compact strictly K -analytic domain;(ii) (V ,Lan|V ) has a formal K -model (V,L);(iii) For any closed curve Y in the special fibre Vs with Y proper

over K , we have degL(Y ) ≥ 0.

Call ‖ ‖ semipositive on W if it is semipositive at x ∀x ∈W .

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 26 / 29

Page 106: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .

(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

Page 108: Metrics and Delta-Forms in Non-Archimedean Analytic Geometry · 1 Classical Arakelov theory 2 Tropical geometry and Lagerberg’s superforms 3 Delta-forms and delta-currents 4 First

Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.

(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.

(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .

(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curveC of X .

The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .

The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Psh and semipositive formal metrics

Theorem (GK): Let (L, ‖ ‖) be a formally metrized line bundleon a proper variety X and let W be an open subset of X an. Thenthe following properties are equivalent:

(i) The formal metric ‖ ‖ is semipositive over W .(ii) The restriction of the metric to W is functorial δ-psh.(iii) The restriction of the metric ‖ ‖ to W is functorial psh.(iv) The δ-form c1(L|W , ‖ ‖) is positive on W .(v) The restriction of ‖ ‖ to W ∩ Can is psh for any closed curve

C of X .The proof is based on a lifting theorem which allows to lift curvesfrom the special to the generic fibre of an algebraic model.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 27 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open. Then ‖ ‖ is psh if and only if for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have(i) the restriction of φ to each maximal face of Trop(U), where

φ is smooth, is a convex function and(ii) the corner locus φ · Trop(U) is effective tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open.

Then ‖ ‖ is psh if and only if for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have(i) the restriction of φ to each maximal face of Trop(U), where

φ is smooth, is a convex function and(ii) the corner locus φ · Trop(U) is effective tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open. Then ‖ ‖ is psh if and only if

for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have(i) the restriction of φ to each maximal face of Trop(U), where

φ is smooth, is a convex function and(ii) the corner locus φ · Trop(U) is effective tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open. Then ‖ ‖ is psh if and only if for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have

(i) the restriction of φ to each maximal face of Trop(U), whereφ is smooth, is a convex function and

(ii) the corner locus φ · Trop(U) is effective tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open. Then ‖ ‖ is psh if and only if for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have(i) the restriction of φ to each maximal face of Trop(U), where

φ is smooth, is a convex function and

(ii) the corner locus φ · Trop(U) is effective tropical cycle.

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Piecewise smooth psh metricsCorollary: Let the metric ‖ ‖ on Lan be uniformly approximableby semipositive formal metrics on Lan.

(i) If ‖ ‖ is formal then it is semipositive.(ii) Pullback of ‖ ‖ to any (not necessarily proper) curve is psh.

Theorem (GK): Let ‖ ‖ be a piecewise smooth metric on Lan

over W ⊆ X an open. Then ‖ ‖ is psh if and only if for eachtropical chart (V , ϕU) with V ⊆W and Ω := tropU(V ) convexsuch that there exist a frame s of L over U and a piecewisesmooth function φ : Ω→ R with

− log ‖s‖|V = φ tropU |V ,

we have(i) the restriction of φ to each maximal face of Trop(U), where

φ is smooth, is a convex function and(ii) the corner locus φ · Trop(U) is effective tropical cycle.Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 28 / 29

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Thank you for your attention!

Klaus Künnemann (Regensburg) Metrics and delta-forms Papeete 2015 29 / 29