MONSOONS
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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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MONSOONS

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Monsoons

MONSOONS


Monsoons

200 hPa


Monsoons

850 hPa


Monsoons

ps(hPa)


Monsoons

rainfall (mm day-1)


Monsoons

U(ms-1),

T(oC)

χ(kg s-1)


Monsoons

OLR (W per sq. m)


Monsoons

850hPa

Steady, linear shallow water model


Monsoons

200hPa

850hPa


Monsoons

850 hPa


Monsoons

500hPa

400hPa

850hPa


Monsoons

V(p,t) at Dakar

Easterly waves

Thorncroft et al., QJRMS, 1994

t (days)


Monsoons

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)


Monsoons

V(p,t) at Dakar

Easterly waves

Thorncroft et al., QJRMS, 1994

t (days)


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