the usclivar working group on drought: a multi-model assessment of the impact of sst anomalies on...
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The USCLIVAR Working Group on Drought: A Multi-Model Assessment of the
Impact of SST Anomalies on Regional Drought
The US CLIVAR Drought Working Group http://www.usclivar.org/Organization/drought-wg.html
U.S. Membership• Tom Delworth NOAA GFDL • Rong Fu Georgia Institute of Technology • Dave Gutzler (co-chair) University of New Mexico• Wayne Higgins NOAA/CPC• Marty Hoerling NOAA/CDC • Randy Koster NASA/GSFC• Arun Kumar NOAA/CPC• Dennis Lettenmaier University of Washington• Kingtse Mo NOAA CPC• Sumant Nigam University of Maryland • Roger Pulwarty NOAA- NIDIS Director • David Rind NASA - GISS • Siegfried Schubert (co-chair) NASA GSFC • Richard Seager Columbia University/LDEO • Mingfang Ting Columbia University/LDEO • Ning Zeng University of Maryland
International Membership: Ex Officio• Bradfield Lyon International Research Institute for Climate • Victor O. Magana Mexico • Tim Palmer ECMWF • Ronald Stewart Canada • Jozef Syktus Australia
Other interested participants• Lisa Goddard <[email protected]> • Alex Hall <[email protected]> • Jerry Meehl <[email protected]>• Jin Huang <[email protected]>• John Marshall <[email protected]> • Adam Sobel <[email protected]>• Max Suarez <[email protected]>• Phil Pegion <[email protected]>• Tim Palmer <[email protected]>• Entin, Jared K. <[email protected]>• Donald Anderson <[email protected]> • Rong Fu <[email protected]>• Doug Lecomte <[email protected]>• Hailan Wang <[email protected]>• Junye Chen <[email protected]>• Eric Wood <[email protected]>• Aiguo Dai <[email protected]>• Alfredo Ruiz-Barradas <[email protected]>• Jae Kyung E Schemm <[email protected]>• Clara Deser [email protected]• Kirsten Findell <[email protected]>• Mark Helfand [email protected]• Scott J. Weaver <[email protected]>• Kit K. Szeto <[email protected]>• Chunzai Wang <[email protected]>• Adam Phillips <[email protected]>• Matias Mendez <[email protected]>• Hugo Berbery <[email protected]>
Terms of Reference
• propose a working definition of drought and related model predictands of drought
• coordinate evaluations of existing relevant model simulations
• suggest new model experiments designed to address some of the outstanding uncertainties concerning the roles of the ocean and land in long term drought
• coordinate and encourage the analysis of observational data sets to reveal antecedent linkages of multi-year drought
• organize a community workshop in 2008 to present and discuss results
Model Experiments
• Force global models with idealized SST anomalies– Address physical mechanisms, model dependence
• Participating groups/models: NASA (NSIPP1), Lamont(CCM3), NCEP(GFS), GFDL (AM2.1), NCAR (CAM3.5), and COLA/Univ. of Miami/ (CCSM3.0)
• Web site with access to monthly data ftp://gmaoftp.gsfc.nasa.gov/pub/data/clivar_drought_wg/README/www/index.html
Focus Here on Two Leading Patterns of Annual SST Variability
Pacific Pattern
Atlantic Pattern
C
Main Experiments
Warm Atlantic
Neutral Atlantic
Cold Atlantic
Warm Pacific
PwAw PwAn PwAc
Neutral Pacific
PnAw PnAn
Control
PnAc
Cold Pacific
PcAw PcAn PcAc
- REOF patterns superimposed on mean seasonal cycle with +/- 2 std amplitude- e.g., PwAc is the combined pattern of warm Pacific and cold Atlantic- all runs 50 years (35 for GFS)
Global Spatial Correlations of Annual Mean Responses
Precipitation
z 200mb
Agreement among models for response to Pacific is high
Agreement among models for response to Atlantic is lower
Agreement is higher for z200 than it is for precipitation
Warm Pacific
Annual Mean Precip (mm/day) and z200 (5 meter CI) Response
Warm Atlantic
Annual Mean Precip (mm/day) and z200 (5 meter CI) Response
Annual Precipitation (mm/day)
Pacific Cold+Atlantic Warm Pacific Warm+Atlantic Cold
US Drought! US Pluvials!
Some Basic Results: Over US
• Mean Responses– Models tend to agree that
• Cold Pacific+Warm Atlantic => drought/warm• Warm Pacific+Cold Atlantic => pluvial conditions/cold
– There are substantial differences in details of anomaly patterns– There is a large seasonality in responses
• Potential Predictability (Pacific signal to noise)
– Largest in spring
– Models appear to agree more on precipitation than surface temperature responses!
Special issue highlighting results is now being put together for J.
Climate
End
The model results are from AMIP-style runs from each model (runs forced by observed SSTs for the period 1980-1998). Contour interval for the height field is 20m (negative values are dashed and the zero line is the first solid contour). Precipitation is in mm/day.
Annual Mean Precipitation and 200mb Eddy Height Climatologies
Annual Mean Tsfc Response (°C)
Pacific Warm Pacific Cold
Annual Mean Tsfc Response (°C)
Atlantic Warm Atlantic Cold
Great Plains(Annual Mean Response)
Tsfc
Precip
warm Pacific
cold Pacific
Cold Pacific
Annual Mean Precip (mm/day) and z200 (5 meter CI) Response
Cold Atlantic
Annual Mean Precip (mm/day) and z200 (5 meter CI) Response
Annual Precipitation (mm/day)
Pacific Cold Atlantic Warm
Tendency for US Drought!
Annual Precipitation (mm/day)
Pacific Warm
Atlantic Cold
Tendency for US Pluvials!
Annual Precipitation (mm/day)
Pacific Cold+Atlantic Warm Pacific Warm+Atlantic Cold
US Drought! US Pluvials!
Seasonal Evolution of Response
DJF - Cold
Weak and shifted anti-cyclonic anomalies
Contours: 200mb height anomalies
Vectors: 850mb wind anomalies
Colors: precipitation anomalies
MAM - Cold
General consistency in height anomalies but CFS again shifted south
JJA - Cold
Cyclonic anomalies in IAS
SON - Cold
Cyclonic anomalies in IAS
DJF MAM
JJA SON
Great Plains(Seasonality of Response)
warm Pacificcold Pacific
Tsfc
Precip
Predictability Measures
Signal to Noise Ratio
R = ( x-y )/sxy
( ): 50 yr mean
x: seasonal mean from experiment
y: seasonal mean from control (climatological SST)
s2xy = (s2
X+s2Y)/2
s2X variance of seasonal mean from experiment
s2Y : variance of seasonal mean from control
Signal to Noise Ratio ( R)
GP SESW
NW
Focus U.S. Response to Pacific Forcing
Precipitation Response to Warm and Cold Pacific (signal/noise)
R
R
Tsfc Response to Warm/Cold Pacific (signal/noise)
R
R