Mid-Holocene Ocean Feedback on Global Monsoon Area and Precipitation
TIAN Zhi-Ping1, JIANG Da-Bang1,2
Figure 2 Changes in summer monsoon precipitation units: mm d -1 for the a AGCM and b AOGCM, and c due to ocean feedback. d Changes in summer vertically integrated water vapor flux arrows; units: kg m -1 s -1 and its divergence shading; units: mm d -1 due to ocean feedback. The vertical integration of the water vapor flux was performed from the surface to 300 hPa, and the impacts of topography have been removed using the surface pressure. The units of divergence have been converted to mm d -1 assuming the density of liquid water as 1 g cm -3 .