Improvement of extreme climate predictions from dynamical climate downscaling Yang Gao 1 , Joshua S. Fu 1 , John B. Drake 1 , Yang Liu 2 , Jean-Francois Lamarque 3 , Kan Huang 1 , Xinyi Dong 1 and David Wong 4 1 Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, TN 2 Rollins School of Public Health, Emory University, Atlanta, Georgia 3 Atmospheric Chemistry and Climate and Global Dynamics Divisions, National Center for Atmospheric Research, Boulder, CO 4 Atmospheric Modeling and Analysis Division, NERL, USEPA, Research Triangle Park, NC 11 th Annual CMAS Conference 15-17 th October, 2012
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Improvement of extreme climate predictions from dynamical climate downscaling Yang Gao 1, Joshua S. Fu 1, John B. Drake 1, Yang Liu 2, Jean-Francois Lamarque.
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Improvement of extreme climate predictions from dynamical climate downscaling
Yang Gao1, Joshua S. Fu1, John B. Drake1, Yang Liu2, Jean-Francois Lamarque3, Kan Huang1, Xinyi Dong1 and David Wong4
1Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, TN2Rollins School of Public Health, Emory University, Atlanta, Georgia3Atmospheric Chemistry and Climate and Global Dynamics Divisions, National Center for Atmospheric Research, Boulder, CO4Atmospheric Modeling and Analysis Division, NERL, USEPA, Research Triangle Park, NC
11th Annual CMAS Conference
15-17th October, 2012
Linkage from Global model to Regional Model
Community Earth System Model
CESM 1.0
Regional Climate/Chem Model
WRF 3.2.1/CMAQ 5.0
D1/D2/D3: 36-12-4 km
Community Land Model
(CLM)
Community Atmosphere Model (CAM)
Community Sea Ice Model
(CSIM)
Ocean component(POP)
http://dss.ucar.edu (dataset number ds510.6)
The points represent NCDC US COOP network station observation points in three regions: Northeast (red color), Midwest (blue color) and Southeast (green color).
City-Level Increase in Heat Wave Intensity, Duration and Frequency 11
A rainy day is defined as a day when the daily precipitation totals at least 1 mm. In the current analysis, extreme precipitation is defined as the 95th percentile of all the rainy days
• Total extreme precipitation (mm/year): Annual total of extreme daily precipitation amounts
• Annual extreme events (days/year): Number of extreme daily precipitation events
• Daily extreme precipitation (mm/day): Annual mean rate of extreme daily precipitation, which is calculated as the total amount of annual extreme precipitation divided by total annual extreme precipitation days.
Extreme precipitation12
Evaluation of precipitation13
Extreme precipitation
Total extreme precipitation
Annual extreme events
Daily extreme precipitation
Present RCP8.5 RCP8.5-Present
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Maximum Daily 8-hr Ozone (MDA8) 15
• Dynamical climate downscaling technique has been applied to CESM, and the downscaled results show significant improvement over global outputs, primarily due to the incorporation of local detailed topography and land use information
• In future climate, more intense and frequency heat waves and extreme precipitation were projected
• In RCP 4.5, ozone concentrations show significant decrease by the end of 2050s; In RCP 8.5, ozone concentration could increase from combined climate and emission effects
Summary
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This research was supported in part by the National Science Foundation through TeraGrid resources provided by National Institute for Computational Sciences (NICS) under grant number [TG-ATM110009].
This research also used resources of the Oak Ridge Leadership Computing Facility at the Oak Ridge National Laboratory, which is supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC05-00OR22725.
This work was partially sponsored by the Centers for Disease Control and Prevention (CDC) under a research project cooperative agreement (5 U01 EH000405).