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.
Not exact matches
Only 10 % of the long -
term LOD variation can be explained by the observable
changes in atmospheric circulation.
A shift
in atmospheric circulation in response to
changes in solar activity is broadly consistent with
atmospheric circulation patterns
in long -
term climate model simulations, and
in reanalysis data that assimilate observations from recent solar minima into a climate model.
Clouds
change — associated with
changes in ocean and
atmospheric circulation —
in the short
term and radically
change the energy budget.
LONDON, 17 March, 2017 — Scientists have calculated that at least 30 % and perhaps one half of the decline
in Arctic summer sea ice could be attributed to natural causes —
changes of ocean and
atmospheric circulation that happen according to some long -
term cycle.
In both the tropics and extratropics, it is difficult to discern significant long - term trends in the patterns of climate variability from natural variability, never mind abrupt (threshold) changes in the atmospheric circulatio
In both the tropics and extratropics, it is difficult to discern significant long -
term trends
in the patterns of climate variability from natural variability, never mind abrupt (threshold) changes in the atmospheric circulatio
in the patterns of climate variability from natural variability, never mind abrupt (threshold)
changes in the atmospheric circulatio
in the
atmospheric circulation.
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.
While on first thought this might seem undesirable because we are looking for a global number, it might make sense to separate them due to the large difference
in land / ocean ratio and the fact that
atmospheric circulation patterns isolate them WRT shorter
term changes.
In summary, it seems to me that in his evidence, Hansen has only addressed changes in the distribution of continents in terms of albedo effects, rather than oceanic and atmospheric circulatio
In summary, it seems to me that
in his evidence, Hansen has only addressed changes in the distribution of continents in terms of albedo effects, rather than oceanic and atmospheric circulatio
in his evidence, Hansen has only addressed
changes in the distribution of continents in terms of albedo effects, rather than oceanic and atmospheric circulatio
in the distribution of continents
in terms of albedo effects, rather than oceanic and atmospheric circulatio
in terms of albedo effects, rather than oceanic and
atmospheric circulation.