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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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Presentation Transcript
slide6

U(ms-1),

T(oC)

χ(kg s-1)

slide9

850hPa

Steady, linear shallow water model

slide10

200hPa

850hPa

slide13

500hPa

400hPa

850hPa

slide14

V(p,t) at Dakar

Easterly waves

Thorncroft et al., QJRMS, 1994

t (days)

slide15

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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