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Three principal factors control the features of South America’s climate. The first and most important of them are the subtropical high-pressure air masses over the South Atlantic and South Pacific oceans and their seasonal shifts in position, which determine both large-scale patterns of wind circulation and the location of the rain-bearing ...
Jul 30, 2021 · Results. Scaling of precipitation change with temperature. Surface warming in East Asia is projected to be stronger at higher latitudes, more over land than over the ocean, and larger in the...
- Wengui Liang, Minghua Zhang
- 2021
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Does cold air cause severe winters in East Asia or North America?
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How are rains borne in Central Asia?
Apr 25, 2018 · 4220 Accesses. 25 Citations. 1 Altmetric. Metrics. El Niño-Southern Oscillation (ENSO) is a key feature for seasonal weather and climate prediction in the extra-tropics since related sea...
- Tianjiao Ma, Wen Chen, Debashis Nath, Hans-F. Graf, Lin Wang, Jingliang Huangfu
- 2018
Sep 9, 2023 · Winters tend to be milder in the Southern Hemisphere than in the North, and many of the factors that cranked up the heat across North America, Europe, and Asia in recent months are doing the...
(The summer rains are borne by monsoon winds, determined by the land mass of Central Asia: in the winter, the cold, dry heavy air over Central Asia flows outward toward the sea; in the summer months, when the warm air over the Central Asian land mass rises and cools, moist air from the ocean flows back bringing rainfall over the land.) **
Aug 31, 2015 · We find that severe winters across East Asia are associated with anomalous warmth in the Barents–Kara Sea region, whereas severe winters over North America are related to anomalous warmth...
The northern and southern continental interactions in winter and summer and the differential heating due to the asymmetric character of the two sub-regions give rise to the monsoon development ( Hastenrath 1991 ), which, to a large extent, influences the rainfall characteristics of the region as a whole ( Figure 5.1 ).
