Instead, changes in the South Pole's ozone hole from year - to - year are likely the result of natural
variations in wind patterns, researchers said here Wednesday (Dec. 11) in a press conference at the annual meeting of the American Geophysical Union.
There are
variations in wind pattern, ocean currents and arctic melting.
Not exact matches
The
pattern of
wind change is complex, but
variations in winds can help to explain some of the regional
patterns in sea - ice formation [8].
Then there are seasonal
variations in the
pattern: we see much stronger
wind from late winter to early summer than
in the rest of the year.
Phenomena such as El Niño and La Niña — which warm and cool the tropical Pacific Ocean and cause corresponding
variations in global
wind and weather
patterns — contribute to short - term
variations in global temperatures.
«The authors write that «the El Niño - Southern Oscillation (ENSO) is a naturally occurring fluctuation,» whereby «on a timescale of two to seven years, the eastern equatorial Pacific climate varies between anomalously cold (La Niña) and warm (El Niño) conditions,» and that «these swings
in temperature are accompanied by changes
in the structure of the subsurface ocean, variability
in the strength of the equatorial easterly trade
winds, shifts
in the position of atmospheric convection, and global teleconnection
patterns associated with these changes that lead to
variations in rainfall and weather
patterns in many parts of the world,» which end up affecting «ecosystems, agriculture, freshwater supplies, hurricanes and other severe weather events worldwide.»»
Climate variability associated with the North Atlantic Oscillation (NAO) determines many physical coastal processes
in Europe (Hurrell et al., 2003, 2004), including
variations in the seasonality of coastal climates, winter
wind speeds and
patterns of storminess and coastal flooding
in north - west Europe (Lozano et al., 2004; Stone and Orford, 2004; Yan et al., 2004).
It's a mode of natural
variation in the tropical eastern Pacific ocean which is indicated by sea surface temperature
in that region, as well as
patterns of atmospheric pressure, surface
winds over the ocean, even precipitation over a much larger region.
It implied transient
variations of
wind patterns within broad limits, and mostly concerned how weather might change
in a particular region.
These changes will likely include major shifts
in wind patterns, annual precipitation and seasonal temperatures
variations.
This eastward moving pulse of anomalous
variations in rainfall,
wind, sea surface temperatures, and clouds
in the tropics typically recurs every 30 — 60 days, creating a
pattern that profoundly influences global weather and climate systems, including monsoons, tropical cyclone activity, and El Niño — Southern Oscillation events.
As noted above,
patterns of large - scale variability
in the extratropical atmospheric
wind field exhibit
variations on timescales from weeks to decades (Hartmann and Lo, 1998; Feldstein, 2000).
Defining Climate Climate = long term weather
patterns... — Averages and
variations in temp., precip.,
wind, etc..
These jet
variations underlie the variability associated with
patterns such as the North Atlantic Oscillation (NAO) and have considerable societal impact through
variations in the prevailing westerly
winds.