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Titlebook: Bottom Gravity Currents and Overflows in Deep Channels of the Atlantic Ocean; Observations, Analys Eugene G. Morozov,Roman Y. Tarakanov,Dmi

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樓主: 人工合成
31#
發(fā)表于 2025-3-26 23:51:30 | 只看該作者
https://doi.org/10.1057/9781137313911of several water masses in the deep and bottom layers of the Atlantic. We analyze the mechanisms of the formation of these waters and their circulation. We compare different definitions of Antarctic Bottom Water (as well as some other water masses) and criteria to identify their boundaries.
32#
發(fā)表于 2025-3-27 01:23:17 | 只看該作者
33#
發(fā)表于 2025-3-27 07:41:28 | 只看該作者
34#
發(fā)表于 2025-3-27 11:53:00 | 只看該作者
35#
發(fā)表于 2025-3-27 16:33:42 | 只看該作者
36#
發(fā)表于 2025-3-27 20:40:10 | 只看該作者
https://doi.org/10.1007/978-3-030-68968-1hannels into the North American Basin. Much consideration is related to the eastward flow in the equatorial fracture zones in the Mid-Atlantic Ridge: the Romanche and Chain fracture zones. A special region for analysis is the inflow of Antarctic Bottom Water into the western part of the Romanche Fra
37#
發(fā)表于 2025-3-27 22:02:13 | 只看該作者
The Creation and Use of Public Spacee flows of Antarctic Bottom Water through the fracture zones in the northern part of the Mid-Atlantic Ridge based on the CTD and LADCP observations in 2006, 2014, 2015, and 2016. We measured the thermohaline properties and velocities and analyzed the flows of bottom water in the Strakhov, Bogdanov,
38#
發(fā)表于 2025-3-28 05:28:05 | 只看該作者
39#
發(fā)表于 2025-3-28 08:49:13 | 只看該作者
Leisure Venues: London by Day and by?Nightadeira Basin to the Iberian Basin is studied on the basis of hydrographic measurements in October 2011 and in September 2013, historical data from the WOD18 database, and recent data on bottom topography. The overflow of the coldest water occurs through two passages with close depths at 16° W (Disco
40#
發(fā)表于 2025-3-28 13:19:41 | 只看該作者
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