Not exact matches
For example, in Earth
atmospheric circulation (such as Hadley
cells) transport heat between the warmer equatorial regions to the cool polar regions and this
circulation pattern not only determines the temperature distribution, but also sets which regions on Earth are dry or rainy and how clouds form over the planet.
Specifically, they looked at the Hadley
cell, one of the planet's most powerful
atmospheric circulation patterns, driving weather in the tropics and subtropics.
Includes detailed information on the characteristics of the atmosphere, factors affecting wind, global
atmospheric circulation systems, global pressure patterns and Hadley, Ferrel and Polar
cells.
On global vs. local, how about the global model prediction of a deepening and widening of the tropical
atmospheric circulation, which leads to the Hadley
cell expansion and the projection of the dry zones expanding polewards.
Here we are talking about modification of
atmospheric circulation — poleward expansion of the dry, descending portion of the Hadley
Cell circulation by a few degrees, associated shifts in the jet stream.
1) It seems to me that the key mechanism for any impact must be the changes that increased arctic ocean temperatures will impose on the
atmospheric circulation feature known as the Polar
Cell, and via this on the Ferrel cell which sits over the mid latitu
Cell, and via this on the Ferrel
cell which sits over the mid latitu
cell which sits over the mid latitudes.
Its findings suggest that changing storm patterns and the ensuing droughts are due to a southern shift in the Hadley
cell, the large - scale pattern of
atmospheric circulation that transports heat from the tropics to the subtropics.
For example, the Hadley
cell, the large - scale pattern of
atmospheric circulation that transports heat from the tropics to the subtropics, has marched south during recent decades, moving the subtropical dry zone (a band that receives little rainfall) along with it.
Tags:
atmospheric circulation, climate, clouds, hadley
cells Posted in In Case You Missed It 3 Comments and counting
The ITCZ is located at the ascending branch of the Hadley
cell, an
atmospheric circulation associated with rising air near the equator and descending air in subtropical regions (see Fig. 2 for a schematic).
Named after him, the Hadley
cell is the only portion of the
atmospheric circulation we understood in concept for 250 years.
The large scale
atmospheric circulation «
cells» shift polewards in warmer periods (for example, interglacials compared to glacials), but remain largely constant as they are, fundamentally, a property of the Earth's size, rotation rate, heating and
atmospheric depth, all of which change little.
Convection is characterized by a
circulation pattern of rising and sinking air masses, and the
atmospheric vertical volume transport takes place through
cells of updraft and subsidence; however, these may not be coherent or stable in time and space.