summer synthesis institute

17
Summer Synthesis Institute Vancouver, British Columbia June 22 – August 5 Overview of Synthesis Project Synthesis Project Descriptions Summer Institute Logistics

Upload: hans

Post on 24-Feb-2016

50 views

Category:

Documents


0 download

DESCRIPTION

Summer Synthesis Institute. Vancouver, British Columbia June 22 – August 5. Overview of Synthesis Project Synthesis Project Descriptions Summer Institute Logistics. Water Cycle Dynamics in a Changing Environment: Advancing Hydrologic Science through Synthesis. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Summer Synthesis Institute

Summer Synthesis Institute

Vancouver, British ColumbiaJune 22 – August 5

Overview of Synthesis ProjectSynthesis Project Descriptions

Summer Institute Logistics

Page 2: Summer Synthesis Institute

Water Cycle Dynamics in a Changing Environment:

Advancing Hydrologic Science through Synthesis

Murugesu SivapalanPraveen Kumar, Bruce Rhoads, Don Wuebbles

University of IllinoisUrbana, Illinois

Page 3: Summer Synthesis Institute

Session 2

Suresh RaoPurdue University

Nandita BasuUniversity of Iowa

Contaminant Dynamics across Scales: Temporal and Spatial Patterns

Aaron PackmanNorthwestern University

Page 4: Summer Synthesis Institute

Non linear filters create emergent patterns/signatures across scales

Signatures integrate ecosystem structure and function

Relationship of water flow and water quality to stream ecosystems

Examining signatures using data analysis and models

Conceptual Model

Climate(rainfall, ET)

Landscape (non-linear

filter)

Streamflow

Biogeochemistry (non-

linear filter)

Contaminant Loads

Aquatic Habitat and Biodiversity

Cascading Controls

Page 5: Summer Synthesis Institute

Overall HypothesisDespite process complexity at the local scale, non-linear interactions in the cascade of filters and buffers generate emergent spatio-temporal patterns or signatures that can be expressed as simple functions of the hydrologic and biogeochemical drivers of the system.

5

Page 6: Summer Synthesis Institute

Emergent Patterns: Runoff Coefficient (RC) and Flow Duration Curve

6Exceedance Probability

flow

Budyko Curve describes the mean annual streamflow across the climatic gradient

Botter et al. (2009) showed that FDC can be predicted as a simple analytical function of λ/k

- λ (runoff frequency) - k (catchment mean residence time)

Runoff frequency can be expressed in terms of underlying soil vegetation and rainfall properties

Catchment mean residence time estimated from hydrograph recession curve analysis

Able to describe pdfs of streamflows across several catchments in US

mean annual P

mea

n an

nual

Q

?

Inter-annual

Intra-annual

Slope = RC

Page 7: Summer Synthesis Institute

7

Example 1: Emergent Pattern: LAPU and Load Duration Curve (LDC)

Exceedance Probability

load

1. Formulate Hypotheses

LDC is a function of FDC since water carries the chemical

Chemical Properties (sorption, degradation, etc.)

Chemical input functions (atmospheric deposition vs. fertilizer application)

Landscape Biogeochemical Filter

Chemical Input

Chem

ical

Expo

rt

?

LAPU: Load as a Percent Used (analogous to RC)

Slope = LAPU

Inter-annual

Intra-annual

Page 8: Summer Synthesis Institute

Emergent Pattern: Load Duration Curve (LDC)

2. Run Model to explore dominant controls on LDC

Two available transient hillslope-network coupled models

- Model A (Reggiani et al.) Sheng Ye and Hongyi Li- Model B (Rinaldo et al.) Stefano Zanardo

3. Analyze data to explore dominant controls on LDC

4. Develop simple analytical approaches5. Response to change

Page 9: Summer Synthesis Institute

Hydrologic and Biogeochemical Filters

Two Functions of Filters:

1. Decrease in mass - Hydrologic Filter: runoff coefficient- Biogeochemical Filter: load as a percent

used

2. Alteration of the distribution: - relationship between flow distribution curve and rainfall duration curve (Hydrologic Filter)- relationship between load distribution curve and flow duration curve (Biogeochemical

Filter)

Page 10: Summer Synthesis Institute

Example 2: Biogeochemical Filter:Dual Duration Curve (DDC)

1

11

1

normalized flow

norm

alize

d lo

ad

exceedanceprobability

exce

edan

cepr

obab

ility

?

What does the DDC depend on?

Page 11: Summer Synthesis Institute

0

0.2

0.4

0.6

0.8

1

0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1

norm

alize

d lo

ad

normalized flow

1994 - A

1994 - B

1995 -A

1995 - B

1996 - A

1996 - B

1997 - A

1997 - B

Biogeochemical Filter:Dual Duration Curve (DDC)

A – nitrateB – atrazine

Why is nitrate so different from atrazine?

How can we classify chemicals or watersheds based on such signatures?

Page 12: Summer Synthesis Institute

y = 0.0087xR² = 0.8826

0

100

200

300

400

500

600

0 20000 40000 60000 80000

Nitr

ate l

oad

(kg/

d)

Flow (m3/d)

Mean Annual Patterns: Flow vs. Load

Intra-annual patterns observed in DDC persists in the mean annual behavior…

y = 2E-06xR² = 0.1505

00.020.040.060.08

0.10.120.140.160.18

0.2

0 20000 40000 60000 80000

Atra

zine

load

(kg/

d)

Flow (m3/d)

Page 13: Summer Synthesis Institute

13

Network Models: Spatial PatternsNitrogen Yield

kg/km2

y = 1.22x-0.09

R² = 0.97

y = 2.31x-0.29

R² = 0.94

y = 1.52x-0.16

R² = 0.97

0.3

0.4

0.5

0.6

0.7

0.8

0.9

110 100 1000

LAPU

area (km2)

Q^0.4Q^0Q^0.2

0

0.2

0.4

0.6

0.8

1

0 200 400 600 800

ke (p

er d

ay)

area (km2)

no Q dependence

Q^0.2

Q^0.4

Page 14: Summer Synthesis Institute

Objectives/Tasks(1) Identify relevant hydrologic, biogeochemical and ecological

signatures

(2) Understand the functioning of the hydrologic and biogeochemical filters that modify the forcing functions (rainfall and chemical application)

- Formulate hypotheses- Run model- Analyze Data

(3) Develop simple analytical approaches to predict the signatures as a function of the key parameters of the filters and forcings

(4) Identify how land use or climate change would alter the attributes of the filters, and thus change the signatures.

Page 15: Summer Synthesis Institute

Data based SignaturesHumid: Little Vermilion Watershed in Illinois:

tile-drained agricultural watershed, approximately 480 km2 Arid: Avon River Basin in Western Australia:

agricultural watershed of size 120,000 km2

We are searching for other catchments with water quality data --- suggest your favorite catchment

Chemicals of interest: Dissolved (Nitrate, pesticides etc)

Page 16: Summer Synthesis Institute

Key preparation work required1. Read the papers and familiarize yourself with the primary

assumptions in the two models

2. Question the assumptions and think what they would mean in terms of the observed signatures

3. Start thinking about the signatures and filters --- other interesting signatures or questions that you may want to explore

4. Read the questions/hypotheses in the framework and think about additional ones that you want to explore.

5. Contact me if you have or know of contrasting watersheds with water quality data

More thinking than doing….

Page 17: Summer Synthesis Institute

Exceedance Probability

flow

Exceedance Probability

load

Intra-annual Variability Inter-annual Variability

1

Time

Q

Time

C

area

RC

area

LAPU

Ep/P

E/Q

Budyko

Time

Smal

lest

scal

e ph

ysio

logi

c res

pons

e

Exceedance Probability

Body

bur

den

Ep/P

LAPU

Watershed ClassificationGuide Management DecisionsPrediction in Un-gauged Basins