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Gabriela Bucini & AIM Team
Climate Variables for Water Quality Modeling: Downscaling and a Weather Generator Gabriela Bucini & AIM Team May 27, 2015
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IAM TEAM Asim Zia Carol Adair Ibrahim Mohammed Patrick Clemins
Lesley-Ann Dupigny-Giroux Steve Scheinert Christopher Koliba Gillian Galford Linyuan Shang Andrew Schroth Scott Turnbull Jody Stryker Brian Beckage Gabriela Bucini Yushiou Tsai Arne Bomblies Sarah Coleman Kristen Underwood Donna Rizzo Justin Guilbert Yaoyang Xu Jonathan Winter Peter Isles Ahmed Hamed Alan Betts Scott Hamshaw
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Study area General circulation models
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IAM GENERAL CIRCULATION MODELS REGIONAL CLIMATE CHANGE SCENARIOS
DOWNSCALING GRASS & RHESSYS HYDROLOGIC MODEL FLOW LimnoTech LAKE MODEL Integrated Assessment Model Downscaling: from 100 km to 1 km LAND USE MODEL LAND USE CHANGE SCENARIOS WATER QUALITY LAND USE
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PEGASUS WORKFLOW Processing of vast amounts of data
Organizing the process Allows users to automate multi-step computational tasks Defines a sequence of operations. Pegasus workflow system is used to connect of the elements of the model and automate the sequence of operations. It connects the data files to thei models and runs the oprations under the various initial conditions (scenarios). Source: Pegasus workflow management system University of Southern California
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Challenge: GCM projections only provide T and P, but our lake model needs other climate variables as well.
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GENERAL CIRCULATION MODELS
P, Tmin, Tmax REGIONAL CLIMATE CHANGE SCENARIOS DOWNSCALING P, Tmin, Tmax GRASS & RHESSYS HYDROLOGIC MODEL FLOW LimnoTech LAKE MODEL Integrated Assessment Model Daily Tmin, Tmax and precipitation LAND USE MODEL LAND USE CHANGE SCENARIOS WATER QUALITY LAND USE
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GENERAL CIRCULATION MODELS
P, Tmin, Tmax P, Tmin, Tmax, solar radiation, relative humidity, pressure, cloud cover u, v REGIONAL CLIMATE CHANGE SCENARIOS DOWNSCALING P, Tmin, Tmax WEATHER GENERATOR GRASS & RHESSYS HYDROLOGIC MODEL FLOW LimnoTech LAKE MODEL Integrated Assessment Model LAND USE MODEL LAND USE CHANGE SCENARIOS North American Regional Reanalysis (NARR) 32 km grid resolution, daily from 1979 – 2014 WATER QUALITY LAND USE
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General Circulation Models
Climate downscaling General Circulation Models Climate ~100 Km CMIP5 Intermediate Downscaling Climate ~12 Km General circulation models, intermediately downscaled climate, and fine-resolution downscaling We take an intermediately downscaled product called CMIP5 Fine Downscaling Climate ~ 1km
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Downscaling to <1km cell size
Cell size:~ 12 km Lake Champlain
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Adding climatic information and spatial detail
Lapse rate relationships: to adjust T and P for variations in elevation Interpolation: to increase spatial resolution of the grid Run on Yellowstone high-performance computing system: Goal 112 ensembles: 28 GCMs 2 interpolation methods 2 climate scenarios RCPs: climate scenarios
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Nov. 21, 1970 access1-0 RCP 8.5
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GENERAL CIRCULATION MODELS
P, Tmin, Tmax P, Tmin, Tmax, solar radiation, relative humidity, pressure, cloud cover u, v REGIONAL CLIMATE CHANGE SCENARIOS DOWNSCALING P, Tmin, Tmax WEATHER GENERATOR GRASS & RHESSYS HYDROLOGIC MODEL FLOW LimnoTech LAKE MODEL Integrated Assessment Model LAND USE MODEL LAND USE CHANGE SCENARIOS WATER QUALITY LAND USE
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Weather generator resampling
Downscaled GCM T and P Daily, NARR T, P, u, v, RH, Pressure, Solar Radiation, Cloud Cover Daily, North American Regional Reanalysis (NARR) The methods resamples data from the historical records provided by NARR reanalysis data Generate daily weather sequences as inputs for the lake model Time-series resampling algorithm capable of generating daily values of weather variables for future time ranges. The sampling of historical values is based on nearest-neighbor concept. The search is conditioned on proximity to both temperature and precipitation For each day of future projections, precipitation and temperature from downscaled data are compared to the NARR historical dataset. The most similar temperature and precipitation values (closest neighbors) are extracted. One of the P&T closest neighbors is randomly selected for the weather temporal sequence. The set of NARR variables for that date is used as input for the lake model.
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daily weather sequence of all climate variables
For each future daily T and P Find a matching pair of T and P in historic NARR Steps: Search the historic data under two conditions: time: near selected date value: close T and P values Collect a set of nearest T and P neighbors Randomly select one neighbor daily weather sequence of all climate variables
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NN Searching methods 1st method: Conditional on smallest Euclidean distances of both T and P. 2nd method: Conditional on smallest temperature differences first and then on smallest precipitation differences. How we solved it... 2 resampling methods: 2nd: we have more control over the search: better control in the selection of temperature and precipitation
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SUMMARY Downscaling: Climate projections of P and T into regional fine-resolution grids Resampling Weather Generator: Large set of climate variables tracking P and T projections
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THANK YOU!
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Gabriela Bucini & AIM Team
Measuring the Climate Change Impact on Water Quality using a Weather Generator Pegasus Workflow Gabriela Bucini & AIM Team May 27, 2015
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Our accomplishment: Estimating the suite of climate variables under GCM projections by downscaling and sampling from historical NARR reanalysis data. Data source: North American Regional Reanalysis (NARR)
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Integrated Assessment Model
High Resolution Forecasting of Global Climate Change Impacts on Fresh Water Lakes: Integrating Climate, Land-Use, Hydrological and Limnology Models.
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Integrated Assessment Model
OVERARCHING QUESTION How will the interaction of climate change and land use alter hydrological processes and nutrient transport from the landscape, internal processing and eutrophic state within the lake and what are the implications for adaptive management strategies? High Resolution Forecasting of Global Climate Change Impacts on Fresh Water Lakes: Integrating Climate, Land-Use, Hydrological and Limnology Models. To simulate impacts of adaptive interventions on water quality
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Interactive Land Use Transition Agent-based Model
Climate Change Modeling Global Climate Change Regional Climate Changes Downscaling Interactive Land Use Transition Agent-based Model NLCD Land use Simulated World File GRASS Forest Elaboration Module RHESSYS Lake model input variables Land Use Model Flow Hydrologic Model Water Quality Lake Model
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Lake Champlain Management
Climate Change Social & Economic behavior Hydrology Land Use Water Quality Architecture of IAM Lake Champlain Management Policy Decisions
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Pegasus Workflow MGMT SYSTEM
NSF Funded since 2001 in collaboration with USC + ISI + HTCondor UW-Madison Built on top of HTCondor DAGMan (Directed Acyclic Graph Manager) is a meta-scheduler for HTCondor Abstract Workflows - Pegasus input workflow description Workflow “high-level language” Python, Java, and Perl Pegasus is a workflow “compiler” (plan/map) Target is DAGMan DAGs and HTCondor submit files Transforms the workflow for performance and reliability Automatically locates physical locations for both workflow components and data Collects runtime provenance
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Pegasus WMS Architecture
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Derive Lapse Rates with an Assumed Functional form and MLE
Calculate the relationship between elevation (z), temperature (T), precipitation (P), and latitude (f) Maximum Likelihood Estimation (MLE) with station observations to find α, β, and χ
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Yellowstone high-performance computing system
Goal 112 ensembles: 28 GCMs 2 interpolation methods 2 climate scenarios RCPs: climate scenarios
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A2EM Progress Background: A2EM (Advanced Aquatic Ecosystem Model)
Wind (speed, dir.) Temp RH Pressure Solar Radiation Cloud Cover Phytoplankton growth and nutrient uptake parameters Initial nutrients, phytoplankton, zooplankton Bathymetry River Inputs, Main lake level Not implemented in this version Initial water levels, temp Initial sediment nutrient concentrations, bulk density, sediment diagenesis parameters
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A2EM Lake model Wind (speed, dir.), Precipitation Temperature, Relative Humidity, Pressure, Solar Radiation, Cloud Cover A2EM (Advanced Aquatic Ecosystem Model)
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Hydrodynamic Model Calibration
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A2EM Model Grid
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