Reason, CJC (1998) Warm and cold events in the southeast Atlantic/southwest Indian Ocean region and potential impacts on circulation and rainfall over southern Africa. Meteorol Atmos Phys 69: pp. 49-65Reason, C. J. C. , Warm and cold events in the southeast Atlantic / southwest Indian ...
Atlantic Meridional Overturning Circulation (AMOC) is fed by waters entering the South Atlantic from the Indian Ocean mainly via the Agulhas Current (AC) system and by waters entering from the Pacific through Drake Passage (DP), commonly referred to as the warm and cold water routes, ...
Ocean Circulation in Warm and Cold Climates 来自 Springer 喜欢 0 阅读量: 28 作者:K Bryan,S Manabe 摘要: The response of a coupled atmosphere-ocean model is determined over a wide range of atmospheric CO2 levels. The solutions indicate the type of ocean circulations expected over a very wide...
depending on complex combinations of wind and buoyancy forcing31,32,33. Those currents may in turn be subject to instabilities that facilitate exchanges with the basin interior33,34,35. Yet the process of warm PSW subduction in the Arctic
WASHINGTON, July 4 (Xinhua) -- A new study published on Wednesday in the journal Nature showed that the fastest rates of species formation have occurred at the highest latitudes and in the coldest ocean waters, instead of the balmy coral reefs. ...
Extreme warm episodes in the southeast Atlantic Ocean, known as Benguela Nios, have devastating environmental impacts and have been shown to be remotely forced. To place these extreme events into perspective, the investigation is here extended to minor warm events as well as to cold episodes. To...
The SST color map was generated together with the base map in the program Ocean Data View22. The distribution of coral reefs, shown in white, is based on the dataset available from UN Environment Programme World Conservation Monitoring C entre23. Currents are simplified from24 and ...
It has been challenging to detect trends of tropical cyclone (TC) properties due to temporal heterogeneities and short duration of the direct observations. TCs impact the ocean surface temperature by creating cold wakes as a “fingerprint”. Here we infer changes of the lifetime maximum intensity ...
aAnother kind of current found far below the surface of the water is called a deep ocean current. These currents form when very cold water meets warm water, and this movement causes currents. 潮流被发现远的另一在水的表面之下称深海潮流。 这些潮流形成,当非常冷水遇见温暖的水和这运动起因潮流。
The western North Pacific (35–45°N and 140–160°E) falls between the sub-arctic and sub-tropical domains of the North Pacific (Roden, 1991). The three main currents in this area, the Oyashio, Kuroshio and Tsugaru Warm Current, and their associated fronts have a strong influence on pel...