Global atmospheric circulation consists of the observed wind systems with their annual and seasonal variations, and is the principal factor in determining the distribution of climatic zones, while variations in the atmospheric and oceanic circulations are responsible for many of the observed longer-term ...
摘要: Global atmospheric circulationGlobal atmospheric circulation consists of the observed wind systems with their annual and seasonal variations and is the principal factor in determining the...DOI: 10.1007/0-387-30749-4_20 被引量: 47 年份: 1987 ...
Atmospheric Circulation, Global ; Ferrel Cell : Rossby Regime .Atmospheric Circulation, Global ; Hadley Cell, Hadley Regime ; Rossby Number ; ROSSBY WAVE ; Zonal Circulation and Index .Atmospheric Circulation, Global ; Coriolis Effect ; Rossby Regime ; Rossby Wave .Atmospheric Circulation, Global ;...
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The first type, with the payload mounted inside the envelope to protect the electronics from rainfall (Figure 5) were, for example, flown for several weeks in the 1980s over the Indian Ocean for investigating the atmospheric circulation associated to the monsoon. The experiment was repeated in ...
Among atmospheric energies, the mechanical energies (that is, the potential energy and the kinetic energy) are mainly related to the atmospheric movement and circulation, which influence weather and climate. Lorenz provided the first modern picture of the mechanical energies and their conversions for ...
Variations of global zonal-mean atmospheric circulation are studied using the National Center of Environment Prediction/National Center of Atmosphere Research (NCEP/NCAR) reanalysis data set from January 1948 to February 2001 and CCM3.6 (Community Climate Model Version 3.6) simulations for the period 19...
Figure 3: Simple vertical cycle of atmospheric circulation that might exist if the Earth didn't rotate. Heating air along the equator lowers its density so it rises. It then spreads to higher latitude, cooling as it radiates energy to space. ...
of 1.8, 2.1, 2.4 and 2.7 °C are chosen as best estimates of end-of-century global warming corresponding to different policy assumptions, taken from the Climate Action Tracker1, which uses an ensemble of runs of the MAGICC6 model that, in turn, emulates different general circulation models...
Arctic amplification is a consequence of surface albedo, cloud, and temperature feedbacks, as well as poleward oceanic and atmospheric heat transport. However, the relative impact of changes in sea surface temperature (SST) patterns and ocean heat flux s