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Dr Pankiewicz's presentation - NERC

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The role of Arabian Sea SST bias<br />

Strong monsoons depend on Arabian<br />

Sea moisture in observations<br />

• Large systematic cold SST<br />

errors in Arabian Sea reduce<br />

monsoon rainfall (up to 30%)<br />

and delay onset by weakening<br />

local evaporation.<br />

• Cold Arabian Sea SST errors<br />

develop in winter due (in part)<br />

to excessive winter monsoon<br />

northerlies.<br />

• This tends to reduce Indian<br />

rainfall, particularly in June.<br />

• Inter-model spread of early<br />

monsoon rainfall for future<br />

scenarios is more constrained<br />

in CMIP5 models with large<br />

cold Arabian Sea SST biases.<br />

© Crown copyright Met Office<br />

Idealised re<strong>presentation</strong> of SST bias<br />

Coupled model SST biases and the effect of (1) & (2) on<br />

HadGEM3-A (rainfall and vertically-integrated moisture flux)<br />

Richard Levine

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