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This is a guest post from Richard P Allan, who is a professor in the Department of Meteorology at the University of Reading/UK. He is a lead investigator of the DEEP-C project and tweets at @rpallanuk . This guest post reflects one interpretation of this expansive topic, which like all cutting-edge science, will be revised and updated as new observations and analysis arise.
It is well known that the surface has warmed over the past few decades, primarily in response to rising concentrations of greenhouse gases. ENSO variability and other natural factors, have additionally contributed toward year-to-year fluctuations about this warming trend (dark red line in Figure 1). …
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No, we’re not just talking about ice cream in this post (mmm…. yum), but about the different types, or flavors, of the El Niño-Southern Oscillation (ENSO). These different flavors of ENSO are usually based on the location where tropical Pacific sea surface temperature (SST) anomalies are the largest. There is debate on whether differences in the cold state of ENSO, La Niña, can be classified (1), so we’ll leave that alone for now and focus on the warm state, El Niño.
El Niño can take on a wide range of flavors, but here we show two examples of El Niño winters that are at opposite extremes:
(1) Eastern Pacific El Niño (a.k.a. Cold Tongue, Conventional, or Canonical El Niño):
(2) …
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Do we sound like a broken record? The CPC/IRI El Niño-Southern Oscillation forecast released today is essentially unchanged from last month, with around 60-65% chance of El Niño, starting in October-November. Sea surface temperatures in the Niño3.4 region are +0.3°C over the last week, a downwelling Kelvin wave continues to transport warm water toward the eastern equatorial Pacific, and global climate models continue to call for the development of a weak El Niño.
Just how good are these models, though? In our last post, Tony discussed ENSO forecasts over the last few years, including prediction for El Niño in the fall of 2012 that never materialized. Here, I’ll take a look at one forecast…
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People often want to know how accurate today’s ENSO (El Niño-Southern Oscillation) predictions are. To provide a flavor for how they have been performing lately, we look at results since 2012. For an assessment of ENSO predictions over 2002-2012, check out Barnston et al. (2012).
One of my responsibilities as the lead ENSO forecaster at IRI is to judge how well the forecasts have matched reality. One way I do this is I go back through the archived forecasts and make graphics that compare the forecasts with actual sea surface temperature observations. I look for places where they agree and where they don’t, and try to understand what went wrong where they don’t. But eyeballing …
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This is a guest post from Prof. Adam Sobel, Dept. of Applied Physics and Applied Mathematics & Dept. of Earth and Environmental Sciences, Columbia University. He has also started his own blog, adamsobel.org, and his book about Hurricane Sandy, Storm Surge, will be published by HarperCollins on October 14.
In mid-July 2014, Michelle hypothesized that the reason El Niño was having trouble getting started was that although eastern Pacific sea surface temperatures (SST) were above average, they weren’t being felt by the atmosphere (1). While the central and eastern Pacific were warm, so were the western Pacific and Indian Ocean—so the SST gradient was small (2)—and the gradient is one fac…
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