J. David Neelin, Baird Langenbrunner, Joyce E. Meyerson, Alex Hall, and Neil Berg
J. Climate, 26, 6238-6256, doi:10.1175/JCLI-D-12-00514.1.
Paper (PDF 4.3 MB).
© Copyright 2013 by the American Meteorological Society.
Abstract:
Projections of possible precipitation change in California under global warming have been subject to considerable
uncertainty because California lies between the region anticipated to undergo increases in precipitation at mid-to-high
latitudes and regions of anticipated decrease in the subtropics. Evaluation of the large-scale model experiments for
Coupled Model Intercomparison Project 5 (CMIP5) suggests a greater degree of agreement on the sign of the winter
(December-February) precipitation change than in the previous such intercomparison, indicating a greater portion of
California falling within the increased precipitation zone. While the resolution of global models should not be relied
on for accurate depiction of topographic rainfall distribution within California, the precipitation changes depend
substantially on large-scale shifts in the storm tracks arriving at the coast. Significant precipitation increases in
the region arriving at the California coast are associated with an eastward extension of the region of strong Pacific
jetstream, which appears to be a robust feature of the large-scale simulated changes. This suggests that effects of this
jet extension in steering storm tracks toward the California coast constitute an important factor that should be assessed
for effects on incoming storm properties for high resolution regional model assessments.
Citation. Neelin, J. D., B. Langenbrunner, J. E. Meyerson, A. Hall, and N. Berg: California winter precipitation change under global warming in the Coupled Model Intercomparison Project 5 ensemble. J. Climate, 26, 6238-6256, doi:10.1175/JCLI-D-12-00514.1.