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Presented by LCF Climate Science Computational End Station James B. White III (Trey) Scientific Computing National Center for Computational Sciences Oak Ridge National Laboratory Lawrence Buja National Center for Atmospheric Research

LCF Climate Science Computational End Station

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LCF Climate Science Computational End Station. James B. White III (Trey) Scientific Computing National Center for Computational Sciences Oak Ridge National Laboratory Lawrence Buja National Center for Atmospheric Research. Objectives of the Climate Science Computational End Station. - PowerPoint PPT Presentation

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Page 1: LCF Climate Science  Computational End Station

Presented by

LCF Climate Science Computational End Station

James B. White III (Trey)Scientific Computing

National Center for Computational SciencesOak Ridge National Laboratory

Lawrence BujaNational Center for Atmospheric Research

Page 2: LCF Climate Science  Computational End Station

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Objectives of the Climate Science Computational End Station

Predict future climate Based on scenarios of

anthropogenic emissions Resulting from options

in energy policies

Deliver simulations that improve climate models Scientific basis Accuracy Fidelity

Inform national science policy

Thus contribute to DOE science mission

Page 3: LCF Climate Science  Computational End Station

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Approach of the Climate Science Computational End Station

Develop, maintain, and support the Community Climate System Model (CCSM)

Execute high-priority simulations at LCF

Outreach to research community Simulation products Analysis of model results CCSM workshop

Champion and execute research program to deliver CCSM4 in three years In time for next assessment by the Intergovernmental Panel on

Climate Change

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CCSM4 development objectives Document, understand, and correct biases and

systematic errors Improve simulation of important quantities, like regional

precipitation patterns Higher resolution in dynamics Higher fidelity in physical parameterizations

Characterize dominant nonlinear dynamical mechanisms Climate variability and abrupt transitions Ice and ocean processes with long timescales but small

characteristic length scales

Quantify nature and timing of biogeochemical feedbacks Atmosphere, ocean, and land Impacting global carbon cycle

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Unique value of the Climate Computational End Station

Coordination of development and simulations

Priority setting in climate-change research simulations

Sharing of software expertise

Development of scalable solutions

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Roles within the Climate Science Computational End Station

National Center for Atmospheric Research Higher-resolution atmosphere models Improved physical processes that remove biases Climate-change studies

Los Alamos National Laboratory Increased resolution of ocean and sea-ice models High-resolution coupled experiments Ocean biogeochemistry models

Lawrence Livermore National Laboratory Comparison and validation of new models Scaled, distributed analysis infrastructure Development and testing of high-resolution atmosphere models

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Roles within the Climate Science Computational End Station Pacific Northwest National Laboratory

Downscaling to investigate regional water resources Embedded cloud-resolving models Physically based replacements for cloud parameterizations

NASA Goddard Space Flight Center New observations and measurements to evaluate models Advanced data-assimilation technologies Improvements for policy formulation and impact planning

Oak Ridge National Laboratory Software integration Coupled carbon-cycle simulation Biogeochemistry feedbacks

Additional experiments by university partners

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CCSM development (Peter Gent) Three 100-year control runs of new CCSM 3.5

Tuned snow albedos for best simulation of Arctic sea ice

Much-improved El Nino / Southern Oscillation

Critical-path development of CCSM4 for the IPCC AR5

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Dynamic-ecosystem feedback simulation (Hoffman) Tests of ocean advection schemes on ecosystem tracers

Spin up of terrestrial carbon in CLM-CASA and CLM-CN for Carbon Land Model Intercomparison Project

Courtesy of Jamison Daniel, ORNL

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Regional downscaling

Goal: Improve simulation and surface hydrology in regions of complex orography

Simulations of orographic effects on western United States Regional simulation with Weather Research and

Forecasting (WRF) model Subgrid parameterization with global Community

Atmosphere Model (CAM)

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Regional downscaling

Surface temperature Precipitation Snowpack

Su

bgri

d C

AM

WR

F

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Resolution studies Fully coupled simulations at T170 resolution

(versus T85 for last IPCC)

Improved simulation of tropical cyclones and transients

Better input for regional models

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High-resolution ocean

Several simulated years of spinup at 0.1° resolution

Resolve inconsistency in surface forcing

Tested new modules Lagrangian particles High-frequency time-series

output Passive-tracer transport Courtesy of Jamison Daniel, ORNL

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Emissions-reduction scenarios

450 ppmIPCC commitmentB1A1BA2

450 ppm CO2 case

First of a series of Climate Change Science Program scenarios examining alternative future energy and emissions reduction pathways

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Contact

James B. White III (Trey)Scientific ComputingNational Center for Computational Sciences(865) [email protected]

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