"Atmospheric circulation" refers to the movement of air in the Earth's atmosphere. It includes the patterns of wind and the exchange of heat and moisture around the world. This circulation is crucial for weather and climate systems, affecting temperature, precipitation, and wind patterns.
Full definition
To see if heat waves can be triggered by certain large -
scale atmospheric circulation patterns, the scientists looked at data from relatively modern records dating back to 1948.
Importantly, is the movement caused by the temperature movement below or above, as this has considerable impacts
on atmospheric circulation.
This vapor is often moved
by atmospheric circulation vertically and horizontally to cooler locations where it is condensed as rain or is deposited as snow releasing the heat energy stored within it.
This section documents regional changes and slow fluctuations in
atmospheric circulation over past decades, and demonstrates that these are consistent with large - scale changes in other variables, especially temperature and precipitation.
She applied a storm - tracking algorithm to simplified
atmospheric circulation models in which thousands of storms are generated, thus eliminating the dependence on initial conditions.
This in turn
alters atmospheric circulation, which alters cloud cover, but the impact of cloud cover on surface temperature only explains a small percentage of the surface temperature change.
The results indicate that concurrent
atmospheric circulation trends contribute to forcing winter and summer sea ice concentration trends in many parts of the marginal ice zone during both periods.
Small changes in oceanic or
atmospheric circulation due to small changes in radiative equilibrium may translate in flooding here and drying there, warming here and cooling there, etc..
Temperature changes are one of the more obvious and easily measured changes in climate, but atmospheric moisture, precipitation and
atmospheric circulation also change, as the whole system is affected.
It is no coincidence that abrupt shifts in ocean and
atmospheric circulation occur at the same time as changes in the trajectory of global surface temperature.
Given the remarkable persistence and distinct structure of this high - impact feature of
recent atmospheric circulation, I would argue that it's now worthy of a proper name.
The composition of these clouds plays a major part in determining how much sunlight they reflect into space — which helps to
shape atmospheric circulation and weather patterns below.
They looked at precipitation and
atmospheric circulation among other factors before determining that the model was accurately portraying regional climate and informing global climate calculations.
That's because research from 2014 indicates a strong link between a planet's rotation and whether it could develop clouds and
atmospheric circulation necessary to be habitable.
This resulted from the combined effects of high sea surface temperatures in open water areas and the effects of
atmospheric circulation drawing warm air into the region.
One driver of this is anomalies in sea surface temperature which effect large
scale atmospheric circulation and, in turn, influence precipitation.
It offers a valuable opportunity to study a high mass atmosphere on a solid - surface planetary body, and so to advance models
of atmospheric circulation, precipitation and seasonal response.
Whether or not these changes
in atmospheric circulation are themselves linked to global warming wasn't something the study tried to answer.
Because of
atmospheric circulation patterns, whales living in areas far from industrial centres may contain more environmental pollutants than species near such centres.
Hoerling and Kumar (2003) attributed the drought to changes in
atmospheric circulation associated with warming of the western tropical Pacific and Indian oceans, while McCabe et al. (2004) have produced evidence suggesting that the confluence of both Pacific decadal and Atlantic multi-decadal fluctuations is involved.
This is because of the North Atlantic Current and large - scale
atmospheric circulation which transport warm water and air masses from lower latitudes northwards across the Atlantic and along the coast of Norway to Svalbard (Figure 1).
The North Atlantic Oscillation (NAO), the dominant mode of
atmospheric circulation variability over the North Atlantic / European sector, is a leading governor of wintertime climate fluctuations in Europe, the Mediterranean, parts of the Middle East and eastern North America over a wide range of time scales from intra-seasonal to multi-decadal (e.g., Hurrell 1995; Hurrell et al. 2003).
A northern shift of the ITCZ could be the trigger of these abrupt shifts of northern
hemisphere atmospheric circulation resulting in 2 - 4K changes in Greenland moisture source temperature from one year to the next.
Phrases with «atmospheric circulation»