Thousands of years ago, in the middle of an ocean, miles from the nearest island, an undersea volcano broke out.The hot liquid rock piled higher and higher and spread wider and wider.In this way, an island rose up in the sea. As time went on, hot sun
Sea ice is shrinking during Antarctic winter: here’s what it means for Earth’s oceans and atmosphere The extent of Antarctic sea ice dropped precipitously in 2023. Analysis shows that this decline has increased the transfer of ocean heat to the atmosphere — in turn affecting ocean circulation...
For tidal currents, the M2 component of the model largely dominates the surface current spectrum as expected23. Tidal currents can reach more than 3 m s−1 near the coast and 2 m s−1 in the middle of the Channel (Fig. 2a). Fig. 2: Tidal currents modify the surface stress, ...
Behavior of rare earth elements in seawater at the ocean margin: A study along the slopes of Sagami and Nankai Troughs near Japan Zhang J,Nozaki Y.Behavior of rare earth elements in seawater at the ocean margin:A study along the slopes of the Sagami and Nankai troughs near Japan. ...
thank you 正在翻译,请等待... [translate] a‘Like if you are floating in the middle of the Atlantic Ocean,’ said hadfield。 `喜欢,如果您在大西洋中间浮动’,说hadfield。 [translate] 英语翻译 日语翻译 韩语翻译 德语翻译 法语翻译 俄语翻译 阿拉伯语翻译 西班牙语翻译 葡萄牙语翻译 意大利语翻译 荷兰...
The Pingxiang–Shexian–Suzhou junction zone connects the Jinsha River–Red River junction zone to the north of Henei, which is the subduction zone of the South China Ocean in the middle Neogene. It formed the boundary between the Yangtse plate and the newly-defined China-Southeast Asia plate...
In addition to the Walker and Hadley circulations, ENSO can also remotely affect remote places via other atmospheric teleconnections. An example of the atmospheric teleconnections to other middle-high latitudes is the Pacific-North American (PNA) pattern (Wallace and Gutzler 1981). This PNA teleconne...
3a) corresponding to the late Holocene (5–0 ka), the early and middle Holocene (11–5 ka) and the last glacial period and deglaciation (35–11 ka) (see age models in Extended Data Fig. 3). During the last glacial period and deglaciation, the western Arctic δ15NN.p. values...
The strong ascending motion by the warmer SST over the Indian ocean moves to the troposphere of the tropical Atlantic ocean, with sinking motion in the lower level and ascending motion in the middle and higher level (Supplementary Fig. 5a). Meanwhile, the increased cloudiness over the western ...
- 《Journal of Geophysical Research Solid Earth》 被引量: 152发表: 1994年 Late Paleozoic brachiopod faunas of the South Kitakami Belt, northeast Japan, and their paleobiogeographic and tectonic implications Late Paleozoic (Middle Devonian, Early Carboniferous and Middle Permian) brachiopod faunas of ...