- Oct 22, 2014
- 22,983
Good Morning.
While James is working on the write up of the 10 August 2023 NOAA Hurricane Forecast Update, I thought a refresher would be helpful to those interested is one of the driving forces of world weather phenomena.
Located in the Southern Pacific, there is a current of warmish water that flows 'East to West' or 'West to East' identified as the El Niño Southern Oscillation (aka “ENSO”). It seems recently, everything from weather to climate change are blamed on the natural reoccurring motions of ENSO.
John and Jim on Weather.
While James is working on the write up of the 10 August 2023 NOAA Hurricane Forecast Update, I thought a refresher would be helpful to those interested is one of the driving forces of world weather phenomena.
Located in the Southern Pacific, there is a current of warmish water that flows 'East to West' or 'West to East' identified as the El Niño Southern Oscillation (aka “ENSO”). It seems recently, everything from weather to climate change are blamed on the natural reoccurring motions of ENSO.
El Niño is a coupled phenomenon, meaning the changes we see in the ocean surface temperature must be matched by changes in the atmospheric patterns above the tropical Pacific. The average atmospheric circulation over the tropical Pacific, the Walker circulation, is like a conveyor belt: rising air over the very warm far western Pacific, west-to-east winds high up in the atmosphere, descending air and dry conditions over the east-central Pacific, and returning east-to-west winds near the surface—the trade winds.
Generalized Walker Circulation (December-February) during ENSO-neutral conditions. Convection associated with rising branches of the Walker Circulation is found over the Maritime continent, northern South America, and eastern Africa. NOAA Climate.gov drawing by Fiona Martin.
During El Niño, the warmer east-central tropical Pacific Ocean surface leads to lower surface air pressure and more rising air, clouds, and rain over that region, weakening the overall circulation. The trade winds slow, and drier conditions and higher-than-average air pressure are observed over the western Pacific and Indonesia. The ocean-atmosphere coupling is both how El Niño perpetuates itself, as the atmospheric changes feed back into the oceanic changes, and how El Niño affects global weather and climate.
Generalized Walker Circulation (December-February) anomaly during El Niño events, overlaid on map of average sea surface temperature anomalies. Anomalous ocean warming in the central and eastern Pacific (orange) help to shift a rising branch of the Walker Circulation to east of 180°, while sinking branches shift to over the Maritime continent and northern South America. NOAA Climate.gov drawing by Fiona Martin.
Be aware of this data as you review the Hurricane update and the reported causes of these weather events.John and Jim on Weather.