The North Atlantic warms in a few months in response to an El Niño,
through changes in atmospheric circulation (slower trade winds in the tropical North Atlantic, for example).
Not exact matches
The regions where droughts have occurred seem to be determined largely by
changes in SSTs, especially
in the tropics,
through associated
changes in the
atmospheric circulation and precipitation.
That process releases warm water from below the surface of the PWP, shifts it to the central and eastern equatorial Pacific, releases heat there
through evaporation, which causes
changes in atmospheric circulation,
in turn causing SST outside of the tropical Pacific to vary.
The cryosphere derives its importance to the climate system from a variety of effects, including its high reflectivity (albedo) for solar radiation, its low thermal conductivity, its large thermal inertia, its potential for affecting ocean
circulation (
through exchange of freshwater and heat) and
atmospheric circulation (
through topographic
changes), its large potential for affecting sea level (
through growth and melt of land ice), and its potential for affecting greenhouse gases (
through changes in permafrost)(Chapter 4).
Long - term
changes in atmospheric circulation have resulted
in an increased amount of perennial sea ice being exported
through Fram Strait rather than being recirculated (e.g., Beaufort Gyre); this was what set up the 2007 record September minimum.
Abrupt climate
change due to variations
in the
atmospheric circulation and its attendant patterns of climate variability can arise
through two principal mechanisms: (1)
through abrupt
changes in the time - dependent behavior of the
circulation; or (2)
through slowly evolving
changes in the
circulation that project onto large horizontal gradients
in surface weather.
Thus an understanding of the mechanisms distributing water vapor
through the atmosphere and of water vapor's effects on
atmospheric radiation and
circulation is vital to estimating long - term
changes in climate.