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MONSOONS. 200 hPa. 850 hPa. p s (hPa). rainfall (mm day -1 ). U(ms -1 ), T( o C). χ (kg s -1 ). OLR (W per sq. m). 850hPa. Steady, linear shallow water model. 200hPa. 850hPa. 850 hPa. 500hPa. 400hPa. 850hPa. V(p,t) at Dakar. Easterly waves. Thorncroft et al., QJRMS , 1994.

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ps(hPa)



U(ms-1),

T(oC)

χ(kg s-1)



850hPa

Steady, linear shallow water model


200hPa

850hPa



500hPa

400hPa

850hPa


V(p,t) at Dakar

Easterly waves

Thorncroft et al., QJRMS, 1994

t (days)


Easterly wave climatologies

Track density distributions for EWs: (a) ERA15 + operational analyses, (b) NCEP–NCAR, (c) NCEP–DOE, (d) GEOS-1, and (e) AMIP–NCEP. Track density units are number density per month per unit area as defined in the text.

(Hodges et al., JAS,, 2003)


V(p,t) at Dakar

Easterly waves

Thorncroft et al., QJRMS, 1994

t (days)


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