The Labrador Current is a cold ocean current in the North Atlantic Ocean which flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Nova Scotia. It is a continuation of the West Greenland Current and the Baffin...
13. PSW originates as Pacific ocean water entering through Bering Strait, and is considerably warmed while transiting across the shallow Chukchi shelf during summer months14. An appreciable amount of the summer warmed water subducts, allowing heat to...
Regional Ocean Modelling SystemROMS is used to investigate a cold-core eddy in the East Australian Current (EAC).The eddy formed on the edge of continental shelf in waters of negative vorticity.A sensitivity analysis on wind shows that wind has little effect on eddy formation.The prevailing ...
Seafloor hydrothermal control over ocean dynamics in Enceladus Article 12 March 2025 A warm jet in a cold ocean Article Open access 23 April 2021 Ocean stratification impedes particulate transport to the plumes of Enceladus Article Open access 06 February 2025 Data...
in a cold sweat 用作形容词&ad 冷汗一身的(地),胆战心惊的(地) I was in a cold sweat while they counted the ballots. 在他们清点选票时,我是浑身冷汗。 He stood there in a cold sweat, waiting for something to happen. 他胆战心惊地站在那里,等待着怕出什么事。 get a hump on 急速行进,...
Ocean currents from the Atlantic brought high concentrations of MPs into the Arctic. However, there existed large uncertainties of estimation on the storage and release of MPs in Arctic cryosphere owing to the hypothesis of average MPs concentrations. Meanwhile, representatives of MPs data across the...
Current, which is a cold subarctic current that flows south and circulates counterclockwise along the western North Pacific Ocean. In the eastern North Pacific off southern British Columbia, it splits into the southward flowing cold water California Current and the northward flowing Alaska Current.”...
Areas of old and cold oceanic plate lack conventional volcanism and have been assumed to be devoid of submarine hydrothermal activity. However, petit-spot volcanoes are common in areas of flexure of such oceanic plates. Here, we report hydrothermal ferro
Interactions among the Pacific, Atlantic and Indian Oceans through ocean–atmosphere coupling can initiate and/or modulate climate variability. The Pa
S2). If the Paris Agreement is fulfilled and the current global warming trend is reversed, such ocean cooling could occur in the decades to centuries that follow. Our experiments suggest, however, that this substantial ocean cooling alone would not cause Petermann’s ice shelf to recover (Figs...