Probably
by changes in jet stream position, due to changes in UV absorption in the stratosphere.
-- The record melt of the Greenland ice sheet was facilitated
by changes in the jet stream... — http://www.redorbit.com/news/science/1112875668/jet-stream-caused-greenland-ice-sheet-melt-2012-061713/ «According to University of Sheffield research, published in the International Journal of Climatology, unusual Jet Stream changes were behind record surface melt of the Greenland Ice Sheet last summer.»
Not exact matches
The study
by the Planetary Sciences Group reports that this gigantic storm is another of the agents of
change in the equatorial
jet stream.
The strength and path of the North Atlantic
jet stream and the Greenland blocking phenomena appear to be influenced
by increasing temperatures
in the Arctic which have averaged at least twice the global warming rate over the past two decades, suggesting that those marked
changes may be a key factor affecting extreme weather conditions over the UK, although an Arctic connection may not occur each year.
Virtually ice - free summers
in the arctic sea could well arrive
by 2030, with troubling implications for accelerated albedo feedback and possibly disruptive
changes in the
jet stream.
Research into three centuries of European tree ring data
by Valerie Trouet of the University of Arizona found evidence of significant
changes in the
jet stream starting
in the 1960s.
«We've got this huge El Niño out there, we have the warm blob
in the northeast Pacific, the cool blob
in the Atlantic, and this ridiculously warm Arctic,» says Jennifer Francis, a climate researcher at Rutgers University who focuses on the Arctic and has argued that Arctic
changes are
changing mid-latitude weather
by causing wobbles
in the
jet stream.
Or it may be caused
by any other mechanism (like the influence of solar
changes on the
jet stream position) which enhance the simple direct insolation
change which is incorporated
in several current climate models...
One was published several months ago
in Geophysical Research Letters
by James Screen and Ian Simmonds, who looked for
changes in jet stream characteristics using a different methodology than that of Francis and Vavrus.
A prominent (
in the media, anyway) research study last year
by Rutgers's Jennifer Francis and University of Wisconsin's Stephen Vavrus suggests that the declining temperature difference between the Arctic and the lower latitudes (adding greenhouse gases into the atmosphere warms colder, drier regions more so than warmer, wetter ones — with the notable exception of Antarctica) has led to
changes in the
jet stream which result
in slower moving, and potentially stronger East Coast winter storm systems.
Francis, who wasn't involved with either study, is one of the main proponents of an idea that
by altering how much heat the ocean lets out, sea ice melt and Arctic warming can also
change atmospheric circulation patterns,
in particular
by making the
jet stream form larger peaks, or highs, and troughs, or lows.
There have been many primarily anthropogenic
changes in the past, but the major
jet stream changes caused
by the retreat of the North American Ice Shield seems to be much more determinative for Holocene
changes in Saharan rainfall.
I have now realised that the global albedo
changes necessary and the
changes in solar energy input to the oceans can be explained
by the latitudinal shifts (beyond normal seasonal variation) of all the air circulation systems and
in particular the net latitudinal positions of the three main cloud bands namely the two generated
by the mid latitude
jet streams plus the Inter Tropical Convergence Zone (ITCZ).
Longer flight times caused
by changes to the
jet stream could keep airliners aloft longer, resulting
in more exhaust emissions of CO2 per flight, researchers suggest.
In a warming world hot and cold waves are both generated by changes in the polar jet strea
In a warming world hot and cold waves are both generated
by changes in the polar jet strea
in the polar
jet stream.