future climate scenarios for phosphorus and nitrogen dynamics in the gulf of riga
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Future climate scenarios for phosphorus and nitrogen dynamics in the Gulf of Riga. Bärbel Müller-Karulis , Latvian Institute of Aquatic Ecology Juris Aigars , Latvian Institute of Aquatic Ecology - PowerPoint PPT PresentationTRANSCRIPT
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Future climate scenarios for phosphorus and nitrogen dynamics in the Gulf of Riga
Bärbel Müller-Karulis, Latvian Institute of Aquatic EcologyJuris Aigars, Latvian Institute of Aquatic Ecology
In colaboration with Juris Seņņikovs, Laboratory for Mathematical Modelling of Environmental and Technological Processes, Faculty of Physics and Mathematics, University of Latvia
Latvian Institute of Aquatic Ecology
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Gulf of Riga characteristics
• Semi-enclosed basin• Connected to Eastern Gotland
basin surface waters• Salinity 5.5 – 6.2 PSU• Shallow: average depth 22 m,
maximum 56 m• no permament halocline,
seasonal thermocline, monomictic circulation
• High freshwater and riverine nutrient input
• Regular monitoring since 1973
Response to climate change
?
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Mean temperature (period 1973-2008)
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Mean oxygen (period 1973-2008)
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Model setup• Biogeochemical model
– phytoplankton, zooplankton and nutrients
– NPZD Box model based on Savchuk 2002
– 2 boxes (pelagic, demersal) + sediments
– 3 phytoplankton groups– Zooplankton– NO3, NH4, PO4, O2
– Calibrated to 28-year observation series
• Physical model (1D)– vertical temperature
distribution in the GoR– General Ocean Turbulence
Model (GOTM)– Coefficients of second
order model: Cheng (2002)– Dynamic equation (k-ε
style) for TKE– Dynamic dissipation rate
equation
Temperature changeEcosystem response
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Ins titute Model Driving data Ac ronym E xperiment
S MHI R C AO high res . HadAM3H A2 HC C T L _22 control
S MHI R C AO high res . HadAM3H A2 HC A2_22 scenario
Ins titute Model Driving data Ac ronym E xperiment
S MHI R C AO high res . HadAM3H A2 HC C T L _22 control
S MHI R C AO high res . HadAM3H A2 HC A2_22 scenario
Climate data from PRUDENCE. Control: 1961-1990, Scenario A2: 2070-2100
Extra downscaling of RCM data (bias correction via histogram equalisation):
relative humidity (used variable td2m) air temperature (used variable t2m)
Original RCM data:sea level pressure (used variable MSLP)cloudiness (used variable clcov)wind speed (used variable w10m)wind direction (used variable w10dir)
Calculations made for Gulf of Riga (50 m), 30 year period, daily output data – water temperature
Climate change scenario
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Physical model results – I(mean temperature distribution over depth)
-50
-45
-40
-35
-30
-25
-20
-15
-10
-5
0
0 1 2 3 4 5 6 7 8 9 10 11 12
Temperature, degC
Dep
th, m
Water 1961-1990
Water 2071-2100
Air 1961-1990
Air 2071-2100
T increase by 1,5 (bottom) to 3 (surface) degrees
Surface T increase close to air T increase
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Physical model results – II(mean daily pycnocline depth and its
variation)
-60
-50
-40
-30
-20
-10
0
Jan Feb Mar Apr Mai Jūn Jūl Aug Sep Okt Nov Dec
Dep
th, m
1961-1990
2071-2100
Pycnocline develops earlier...
... stratification lasts longer
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Physical model results – III(mean time-depth plots of temperature)
Contemporary climate
Climate change scenario A2
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0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
md-1
Vertical water exchange
CTL
A2
Vertical water exchange
decreased vertical water exchange
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Demersal oxygen – GR mean
4
5
6
7
8
9
10
11
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
ml l
-1
Demersal oxygen CTL
A2
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Species succession
0
20
40
60
80
100
120
140
160
180
200
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mg
C m
-3
Spring phytoplankton CTL
A2
earlier and more vigorous spring bloom
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Species succession
0
50
100
150
200
250
300
350
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mg
C m
-3
Summer phytoplankton CTL
A2
larger biomass of summer species
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0
2
4
6
8
10
12
14
16
18
20
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mg
C m
-3
Nfixing phytoplankton CTL
A2
Species succession
more cyanobacteria
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0
2
4
6
8
10
12
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mm
ol m
-3
Pelagic NO3
CTL
A2
Pelagic nutrients
larger winter pool
earlier depletion
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0
2
4
6
8
10
12
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mm
ol m
-3
Demersal NO3
CTL
A2
Demersal nutrients
larger demersal nutrient concentrations in summer
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0
2
4
6
8
10
12
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mm
ol m
-2 d
-1
net vertical DIN fluxCTL
A2
Vertical nutrient flux
increased demersal concentrations compensate stratification effect
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0
2
4
6
8
10
12
14
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan
mm
ol m
-2 d
-1
Pelagic DIN regeneration CTL
A2
Nutrient regeneration
Pronounced increase in nutrient recycling!
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Denitrification
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Nitrate uptake/release (oxygen control)
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Ammonium versus nitraterelease
-500 0 500 1000 1500 2000 2500 3000-800
-600
-400
-200
0
200
400
R² = 0.843512645722358
NH4 µmol m-²d-¹
NO
3 µm
ol m
-² d-
¹
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Mean nitrate (period 1973-2008)
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Conclusions
• Increase in phytoplankton growth and primary productivity caused by increased nutrient regeneration
• Slightly increased winter nutrient concentrations• Earlier spring bloom (earlier stratification, no ice cover)• Larger summer phytoplankton biomass, more
cyanobacteria because of more intensive nutrient regeneration
• Lower demersal oxygen concentration caused by more stable and longer stratification
• Denitrification – open question for future research