HR: 16:00h
AN: A44A-03 [Abstracts]
TI: Storm track predictability on seasonal to decadal scales
AU: * Compo, G P
EM: compo@colorado.edu
AF: NOAA-CIRES Climate Diagnostics Center, 325 Broadway R/CDC1, Boulder, CO 80305 United States
AU: Sardeshmukh, P D
EM: prashant.d.sardeshmukh@noaa.gov
AF: NOAA-CIRES Climate Diagnostics Center, 325 Broadway R/CDC1, Boulder, CO 80305 United States
AB:
This talk is concerned with estimating the predictable variation of extratropical daily weather statistics ("storm tracks")
associated with global sea surface temperature (SST) changes on interannual to interdecadal scales, and its magnitude
relative to the unpredictable noise. The SST-forced stormtrack signal in each northern winter in 1950-2004 is estimated as
the mean stormtrack anomaly in an ensemble of
atmospheric general circulation model (AGCM) integrations for that winter with prescribed observed SSTs. Since the
stormtrack signals cannot be derived directly from the archived monthly AGCM output, they are diagnosed from the SST-forced
winter-mean 200 mb height signals using an empirical linear stormtrack model (STM). For two particular
winters, the El Nino of JFM 1987 and the La Nina of JFM 1989, the stormtrack signals and noise are estimated directly, and
more accurately, from additional large ensembles of AGCM integrations. The linear STM is remarkably successful at capturing
the AGCM's stormtrack signal in these two winters, and is thus also suitable for estimating the signal in other winters.
Our principal conclusion is that a predictable SST-forced
stormtrack signal exists in many winters, but its strength and pattern can change substantially from winter to winter. The
pattern correlation of the SST-forced and observed stormtrack anomalies is high enough in the Pacific-North American sector
to be of practical use. In the Euro-Atlantic region, we find much lower correlations, which we argue arise from substantial
AGCM error in representing the regional response to tropical SST forcing, rather than intrinsically low stormtrack
predictability.
DE: 1610 Atmosphere (0315, 0325)
SC: Atmospheric Sciences [A]
MN: 2005 Joint Assembly