Figure 10: Geophysical Fluid Dynamics Laboratory Atmosphere Model version 3 DJF idealized uniform warming responses.
From: El Niño-like teleconnection increases California precipitation in response to warming

GFDL (left) uniform SST warming; (centre) uniform warming with fixed tropical Pacific SSTs; and (right) tropical Pacific SST warming responses for (a–c) precipitation (mm day−1); (d–f) U300 (m s−1); (g–i) V300 (m s−1); and (j–l) pp (hPa2). Symbols represent significance at the 90% (diamond), 95% (X) or 99% (+) confidence level, based on a t-test for the difference of means. Climatological U300, V300 and pp values are also included as thin black contour lines.