Will the sensitivity of the atmosphere to the primary mechanism at the heart of El Niño — that is, feedback between the higher sea temperatures and slowing trade winds, leading to
atmospheric convection over the central Pacific — continue in the future?
Not exact matches
The researchers have also identified smaller circulations that could significantly affect
atmospheric chemistry such as the North American monsoon and
convections over Africa.
«For various periods
over the last 60 years, we have been able to combine important processes:
atmospheric variability, such as the North Atlantic Oscillation, water and air temperatures, the occurrence of fresh surface water, and the duration of
convection,» explains Dr. Marilena Oltmanns from GEOMAR, lead author of the study.
These
convection changes can in turn drive the formation of an
atmospheric ridge in the North Pacific, resulting in significant drying
over California.
http://www.cpc.ncep.noaa.gov/products/outreach/glossary.shtml Low
atmospheric pressure tends to occur
over warm water (and high
over cold water), partly because of deep
convection over the warm water.
As the central part of the Pacific warms up during El Niño, the
atmospheric convection that normally occurs
over the western warm pool migrates to the central Pacific.