El Nino Watch
Sea surface temperature anomaly of the western Pacific warm pool east of the Philippines (JMA).
Indices
JMA's NINO.WEST index is the monthly SST anomaly over Eq-15N, 130E-150E. The same collector also stores JMA's NINO.3 (5N-5S, 150W-90W), JMA's main El Nino index. Series nino_west_jma_anom, nino3_jma_anom (degC).
Limits. Monthly, preliminary for the latest month.
During El Nino the warm pool usually cools relative to normal while NINO.3 warms. A cool warm pool means less rising air and fewer rain clouds near the Philippines and South-East Asia.
Less convection over the western Pacific is one of the ways El Nino reduces rainfall over Thailand and shifts where typhoons form.