The Second Decadal Leading Mode of East Asian Summer Monsoon Rainfall
BAO Qing1 
, YU Pei1, 2
, YU Pei
The Second Decadal Leading Mode of East Asian Summer Monsoon Rainfall |
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BAO Qing
, YU Pei |
| Figure 2 Atmospheric circulation anomalies regressed with the principal component PC of 2DLM-EASR: a winds at 850 hPa vectors; units: m s -1 ; b geopotential height at 500 hPa units: 10 gpm; and c zonal winds at 200 hPa units: m s -1 . The green colored regions in a and the dotted regions in b and c exceed the 95% confidence level. The black shaded areas in a and the bold black lines in b and c denote TP areas with elevations over 2500 m. |
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