Fig. 7: Vertical-meridional structure of the CMJO averaged over 110°E to 130°E. | npj Climate and Atmospheric Science

Fig. 7: Vertical-meridional structure of the CMJO averaged over 110°E to 130°E.

From: Climatological Madden-Julian Oscillation during boreal spring leads to abrupt Australian monsoon retreat and Asian monsoon onsets

Fig. 7

Shown are the specific humidity [contour, solid (dashed) line for positive (negative) value from 1 to 5 (−5 to −1) with an interval of 1, units in 10*g kg−1], divergence (shading, units in 106*s−1), meridional winds and vertical velocity (vector, units in m s−1 and 102*Pa s−1). The purple dashed (solid) lines with plus (minus) signs represent the latitudinal range of the maximum (minimum) OLR CMJO from (a) P24 to (e) P28.

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