Figure 5 | Scientific Reports

Figure 5

From: Double blanket effect caused by two layers of black carbon aerosols escalates warming in the Brahmaputra River Valley

Figure 5

(a), (b), (c) represent the Walker circulation (zonal and vertical winds are averaged between 25N-27N) during 30 August, 4th Sep and 6th September 2009 respectively while (d), (e) and (f) represent the Hadley circulation (meridional and vertical velocity fields are averaged between 80E-92E). The vertical velocity (x -100 hPa/s) is shown by shading where red (blue) indicates upward (downward) motions. Gray portions indicate the Tibetan Plateau.

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