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warm and wintertime cold extreme occurrences increased over land during the so-called hiatus period, and that these increases occurred for distinct reasons. The increase in cold extremes is associated with an atmospheric circulation pattern resembling the warm Arctic-cold continents pattern, whereas the...
The near-coastal South East Atlantic Ocean off Africa is a unique and highly dynamic environment, comprising the cool Benguela Current, warm Angola Current... NJ Hardman-Mountford,AJ Richardson,JJ Agenbag,... - 《Progress in Oceanography》 被引量: 237发表: 2003年 Influence of ENSO and the ...
it means the New Year is coming. "Laba porridge" is popular in many parts of our country. It is said that "Laba porridge can freeze your chin". In such cold weather, a bowl of steaming "Laba porridge can...
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, ...
Here we use global palaeoclimate reconstructions for the past 2,000 years, and find no evidence for preindustrial globally coherent cold and warm epochs. In particular, we find that the coldest epoch of the last millennium—the putative Little Ice Age—is most likely to have experienced the ...
Warm and cold water routes of an O.G.C.M. thermo- haline conveyor belt. Geophys. Res. Lett. 28, 311-314.Speich, S., Blanke, B., and Madec, G.: Warm and cold water routes of an O.G.C.M. thermohaline conveyor belt, Geophys. Res. Lett., 28,...
Hydrographic data and satellite images show the structure of the East Korea Warm Current (EKWC) and its seasonal variation. Satellite images taken in April with concurrent hydrographic data provide evidence of the branching of the Tsushima Current. However there is no evidence of branching in Februa...
In contrast, in the warm season, the North Pacific Subtropical High, which is centered in the eastern North Pacific, covers the North Pacific widely, forming relatively calm conditions. In the western North Pacific subtropical gyre, the Kuroshio flows poleward as the western boundary current, and...
This was consistent with the higher phytoplankton and microzooplankton biomass and higher primary production in the warm-core eddy. The source water for the warm-core eddy was Leeuwin Current water with about a 10% admixture of shelf water. The plankton biomass and productivity of these water ...