Official NOAA El Nino Update: Current El Nino is NOT Strongest on Record, Current Strong El Nino Should Last Until Spring

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Ocean temperature false color representation.
Ocean temperature false color representation.

No, the current El Nino is not the strongest on record, yet.ย  Media outlets reporting that are incorrect.ย  NOAA won’t be able to tell if this is the strongest on record until February 2016 when the November, December, and January sea surface averages have been recorded and compared to other El Nino years.ย  On average, the current El Nino wasn’t as strong as the 1997 El Nino the past 3 months.

“The Niรฑo3.4 ERSSTv4 for Septemberโ€“November is 2.04ยฐC, second to 1997โ€™s 2.18ยฐC.” – NOAA, today

Monthly sea surface temperature in the Niรฑo 3.4 region of the tropical Pacific compared to the long-term average for all moderate-to-strong El Niรฑo years since 1950, showing how 2015 (black line) compares to other strong events. Climate.gov graph based on ERSSTv4 temperature data.
Monthly sea surface temperature in the Niรฑo 3.4 region of the tropical Pacific compared to the long-term average for all moderate-to-strong El Niรฑo years since 1950, showing how 2015 (black line) compares to other strong events. Climate.gov graph based on ERSSTv4 temperature data.

NOAA’s El Nino update today is basically just telling us that the current strong El Nino will last through the winter and that the ocean should return to normal temperatures beginning in late spring, early summer.

For more information, please read NOAA’s article below.

EL NIร‘O/SOUTHERN OSCILLATION (ENSO) DIAGNOSTIC
DISCUSSION
issued by
CLIMATE PREDICTION CENTER/NCEP/NWS
and the International Research Institute for Climate and Society
10 December 2015
ENSO Alert System Status: El Niรฑo Advisory

Synopsis: El Niรฑo is expected to remain strong through the Northern Hemisphere winter 2015-16, with a transition to ENSO-neutral anticipated during late spring or early summer 2016.

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A strong El Niรฑo continued during November as indicated by well above-average sea surface
temperatures (SSTs) across the central and eastern equatorial Pacific Ocean (Fig. 1). The Niรฑo-4, Niรฑo-
3.4 and Niรฑo-3 indices rose to their highest levels so far during this event, while the Niรฑo-1+2 index
remained approximately steady (Fig. 2). The subsurface temperatures in the central and eastern Pacific,
while still well above average, decreased slightly (Fig. 3) due to the eastward push of the upwelling phase
of an equatorial oceanic Kelvin wave (Fig. 4). Low-level westerly wind anomalies and upper-level
easterly wind anomalies continued over the most of the tropical Pacific. The traditional and equatorial
Southern Oscillation Index (SOI) values remained negative. These conditions are associated with
enhanced convection over the central tropical Pacific and suppressed convection over Indonesia (Fig. 5).
Collectively, these atmospheric and oceanic anomalies reflect a strong El Niรฑo episode that has matured.

Screen Shot 2015-12-10 at 10.28.01 AM Screen Shot 2015-12-10 at 10.28.10 AM

Most models indicate that a strong El Niรฑo will continue through the Northern Hemisphere winter
2015-16, followed by weakening and a transition to ENSO-neutral during the late spring or early summer
(Fig. 6). The forecaster consensus remains nearly unchanged from last month, with the expectation that
this El Niรฑo will rank among the three strongest episodes as measured by the 3-month SST departures in
the Niรฑo 3.4 region dating back to 1950. El Niรฑo is expected to remain strong through Northern
Hemisphere winter 2015-16, with a transition to ENSO-neutral anticipated during the late spring or early
summer 2016 (click CPC/IRI consensus forecast for the chance of each outcome for each 3-month
period).

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El Niรฑo has already produced significant global impacts and is expected to affect temperature and
precipitation patterns across the United States during the upcoming months (the 3-month seasonal outlook will be updated on Thursday December 17th). Seasonal outlooks indicate an increased likelihood of
above-median precipitation across the southern tier of the United States, and below-median precipitation
over the northern tier of the United States. Above-average temperatures are favored in the West and
northern half of the country with below-average favored in the southern Plains and along the Gulf Coast.

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