Can Current AGCMs Reproduce Historical Changes in the Atmospheric Diabatic Heating over the Tibetan Plateau?
DUAN An-Min1,3, XIAO Zhi-Xiang1,2, HU Jun1,2
Figure 3 Average for the 71 stations, and results from the five reanalysis datasets and nine AGCMs interpolated onto the locations of 71 stations for spring linear trends in: a and b SH flux W m -2 per decade, c and d V m s -1 per decade, and e and f T s - T a #cod#x000b0;C per decade for 1980-2005. The solid lines denote the zero values and the bars indicate the uncertainty at the 95% confidence level based on the standard error.