HR: 09:30h
AN: GC21A-07 [Abstracts]
TI: Detecting Tropical Precipitation Change in Global Warming
AU: * Munnich, M
EM: munnich@atmos.ucla.edu
AF: UCLA Dept. of Atmospheric and Oceanic Sciences, 405 Hilgard Ave, Los Angeles, CA 90095-1565
United States
AU: Neelin, D
EM: neelin@atmos.ucla.edu
AF: UCLA Dept. of Atmospheric and Oceanic Sciences, 405 Hilgard Ave, Los Angeles, CA 90095-1565
United States
AU: Su, H
EM: hui.su@jpl.nasa.gov
AF: Jet Propulsion Laboratory, 4800 Oak Grove Dr., Pasadena, ca 91109-8099
United States
AU: Meyerson, J
EM: hobo@atmos.ucla.edu
AF: UCLA Dept. of Atmospheric and Oceanic Sciences, 405 Hilgard Ave, Los Angeles, CA 90095-1565
United States
AU: Holloway, C
EM: chollow@atmos.ucla.edu
AF: UCLA Dept. of Atmospheric and Oceanic Sciences, 405 Hilgard Ave, Los Angeles, CA 90095-1565
United States
AB:
Climate model global warming simulations predict large-scale regional changes
in tropical rainfall.
Poor agreement on the spatial distribution of these
still occurs in the latest generation models analyzed here.
Such sensitivity appears consistent with
current hypothesized physical mechanisms
as does the occurence of strong local drying trends.
Persistence of the spatial pattern within each model,
with amplitude increasing with warming, suggests that observational
detection of early large-scale tropical regional precipitation changes
may be a predictor of larger future changes.
Trends exist in current time series; we identify
particular candidate regions that have model counterparts.
Using the models as a proxy, we estimate the timing of skillful detection.
For data availability since 1950,
regions with early locally significant trends
correlate skillfully with local late-century signal
beginning this decade (median 2010) with range 2005-2035
(median 60% of models) for dry regions; 1979
start (satellite era) yields 0-2 decade delay.
We find the early signal misses many regions, so skillful prediction of the
whole late-century pattern begins
in the 2030s.
DE: 1610 Atmosphere (0315, 0325)
DE: 1626 Global climate models (3337, 4928)
DE: 1637 Regional climate change
DE: 1655 Water cycles (1836)
SC: Global Climate Change [GC]
MN: Fall Meeting 2005