Sentences with phrase «mean atmospheric response»

The role of ocean — atmosphere coupling in the zonal - mean atmospheric response to Arctic sea ice loss.

Not exact matches

The climate sensitivity classically defined is the response of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures, clouds, water vapour, winds, snow, sea ice etc.), but before any of the «slow» feedbacks have kicked in (ice sheets, vegetation, carbon cycle etc.).
The climate sensitivity classically defined is the response of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures, clouds, water vapour, winds, snow, sea ice etc.), but before any of the «slow» feedbacks have kicked in (ice sheets, vegetation, carbon cycle etc.).
[Response: Depends a bit on whether you mean basic atmospheric physics, or of - climate - change.
[Response: In this context it means the downward branch of the atmospheric Hadley circulation which exists in the sub-tropics to balance the upward mass flux that occurs near the equator.
This means that if the mean atmospheric pressure varies from year to year (or seasonally) there is a detectable response.
DK12 used ocean heat content (OHC) data for the upper 700 meters of oceans to draw three main conclusions: 1) that the rate of OHC increase has slowed in recent years (the very short timeframe of 2002 to 2008), 2) that this is evidence for periods of «climate shifts», and 3) that the recent OHC data indicate that the net climate feedback is negative, which would mean that climate sensitivity (the total amount of global warming in response to a doubling of atmospheric CO2 levels, including feedbacks) is low.
This means it will take centuries to millennia for deep ocean temperatures to warm in response to today's surface conditions, and at least as long for ocean warming to reverse after atmospheric greenhouse gas concentrations decrease (virtually certain).
Both values are projected global mean surface temperature changes in response to doubled atmospheric carbon dioxide concentrations but on different timescales.»
However, considerable evidence (8 ⇓ ⇓ — 11, 31 ⇓ — 33) simultaneously suggests that the response of northeastern Pacific atmospheric circulation to anthropogenic warming is likely to be complex and spatiotemporally inhomogeneous, and that changes in the atmospheric mean state may not be reflective of changes in the risk of extreme events (including atmospheric configurations conducive to precipitation extremes).
An overall increase in global - mean atmospheric temperatures is predicted to occur in response to human - induced increases in atmospheric concentrations of heat - trapping «greenhouse gases.»
Scientific term ##### Public meaning ##### Better choice enhance ######### improve ########## intensify, increase aerosol ########## spray can ######### tiny atmospheric particle positive trend ####### good trend ####### upward trend positive feedback ##### good response, praise ##### vicious cycle, self - reinforcing cycle
Modeledzonal mean atmospheric temperature change (ºC per century, 1890 - 1999) in response to five distinct forcings (a-e), and to all five forcings combined (f).
a b c d e f g h i j k l m n o p q r s t u v w x y z