December 21
![Image](http://www.osdpd.noaa.gov/data/sst/anomaly/2009/anomp.12.21.2009.gif)
Febuary 4
![Image](http://www.osdpd.noaa.gov/data/sst/anomaly/2010/anomp.2.4.2010.gif)
http://www.osdpd.noaa.gov/ml/ocean/sst/anomaly.html
Moderator: S2k Moderators
BigA wrote:xironman wrote:Thirty day average of SOI has dropped 14 points in 10 daysCode: Select all
26-Jan-2010 1010.00 1006.05 -3.10 -3.69 -7.42
27-Jan-2010 1008.15 1005.55 -9.46 -4.51 -7.30
28-Jan-2010 1006.18 1005.25 -17.33 -5.59 -7.41
29-Jan-2010 1006.51 1004.25 -11.06 -6.03 -7.40
30-Jan-2010 1005.41 1004.75 -18.60 -7.11 -7.43
31-Jan-2010 1001.99 1006.40 -42.49 -8.90 -7.71
1-Feb-2010 999.10 1006.45 -58.07 -11.14 -8.23
2-Feb-2010 999.15 1005.55 -53.51 -13.07 -8.76
3-Feb-2010 1001.71 1006.15 -44.09 -15.01 -9.27
4-Feb-2010 1000.54 1008.35 -60.28 -17.41 -10.08
I think a lot of this drop can be attributed to the fact that a strong tropical cyclone (Oli) has moved within a couple hundred miles of Tahiti.
Synopsis: El Niño is expected to continue at least into the Northern Hemisphere spring 2010.
A significant El Niño persisted throughout the equatorial Pacific Ocean during January 2010 (Fig. 1). Although sea surface temperature (SST) departures in the Niño-3.4 region decreased to +1.2oC in late January, SSTs continued to be sufficiently warm to support deep tropical convection (Fig. 2 and Fig. 3). Over the last several months, a series of oceanic Kelvin waves contributed to the build-up of heat content anomalies in the central and eastern Pacific (Fig. 4). The latest Kelvin wave was associated with temperature departures exceeding +2oC down to 150m depth across the eastern half of the equatorial Pacific (Fig. 5). Equatorial convection over the central Pacific remained enhanced during the month, while convection over Indonesia exhibited considerable week-to-week variability. While the low-level winds have been variable, low-level westerly and upper-level easterly wind anomalies generally prevailed during January. Collectively, these oceanic and atmospheric anomalies reflect a strong and mature El Niño episode.
Nearly all models predict decreasing SST anomalies in the Niño-3.4 region through 2010, and model spread increases at longer lead times (Fig. 6). Nearly half of the models indicate the 3-month Niño-3.4 SST anomaly will drop below +0.5oC around April-May-June 2010, indicating a transition to ENSO-neutral conditions during Northern Hemisphere spring. However, predicting the timing of this transition is highly uncertain.
El Niño impacts are expected to last into the Northern Hemisphere spring, even as equatorial SST departures decrease, partly due to the typical warming that occurs between now and April/May (Fig. 3). Expected impacts during February-April 2010 include drier-than-average conditions over Indonesia and enhanced convection over the central equatorial Pacific Ocean, which will likely expand eastward and influence portions of the eastern tropical Pacific, as well as coastal sections of Peru and Ecuador. For the contiguous United States, potential El Niño impacts include above-average precipitation for the southern tier of the country, with below-average precipitation in the Pacific Northwest and Ohio Valley. Below-average snowfall and above-average temperatures are most likely across the northern tier of states (excluding New England), while below-average temperatures are favored for the south-central and southeastern states.
Blown_away wrote:So is the prediction there will be an El Nino Modoki for the 2010 Atlantic hurricane season? Interesting.
http://www.time.com/time/health/article ... 33,00.html
Blown_away wrote:I guess for it to be an El Nino Modoki the warming has to occur more in the Central Pacific rather than the Eastern Pacific? Does the current El Nino meet that criteria?
http://www.eurekalert.org/pub_releases/ ... 062909.php
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