Decadal Variation of the Aleutian Low-Icelandic Low Seesaw Simulated by a Climate System Model (CAS-ESM-C)
DONG Xiao1,2, SU Tong-Hua1, WANG Jun3, LIN Ren-Ping2
Figure 1 Climatology of sea-level pressure SLP in the Northern Hemisphere in boreal winter DJF units: hPa: a observation; b simulation by the Chinese Academy of Sciences-Earth System Model-Climate system component CAS-ESM-C. Regions with SLP values less than 1004 hPa are shaded.