enso_evolution-status-fcsts-web

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Sub-Surface Temperature Departures in the Equatorial Pacific Since early November, positive subsurface temperature anomalies have stretched across most of the equatorial Pacific. Most recent pentad analysis During December, positive subsurface anomalies in the east-central Pacific weakened.
Tropical OLR and Wind Anomalies During the Last 30 Days Positive OLR anomalies (suppressed convection and precipitation, red shading) were apparent near the Date Line (centered south of the equator). Negative OLR anomalies (enhanced convection and precipitation) were evident over Indonesia, the Philippines, and northern Australia. Low-level (850-hPa) winds were near-average across most of the equatorial Pacific, while anomalous easterlies were present over the western Pacific. Anomalous upper-level (200-hPa) easterly winds were evident across the eastcentral equatorial Pacific.
Page 1 and 2: ENSO: Recent Evolution, Current Sta
Page 3 and 4: Summary ENSO-neutral conditions con
Page 5 and 6: Niño Region SST Departures ( o C)
Page 7 and 8: Global SST Departures ( o C) During
Page 9 and 10: Change in Weekly SST Departures ove
Page 11: Central and Eastern Pacific Upper-O
Page 15 and 16: Weekly Heat Content Evolution in th
Page 17 and 18: Upper-level (200-hPa) Velocity Pote
Page 19 and 20: Oceanic Niño Index (ONI) The ONI i
Page 21 and 22: ONI (ºC): Evolution since 1950 The
Page 23 and 24: Historical El Niño and La Niña Ep
Page 25 and 26: IRI/CPC Pacific Niño 3.4 SST Model
Page 27 and 28: Atmospheric anomalies over the Nort
Page 29 and 30: Atmospheric anomalies over the Nort
Page 31 and 32: U.S. Temperature and Precipitation
Page 33: Summary ENSO-neutral conditions con

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