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