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DOIhttps://doi.org/10.1594/PANGAEA.865177
Oxygen Utilization and Downward Carbon Flux in an Oxygen-Depleted Eddy in the Eastern Tropical North Atlantic
Fiedler; Björn; Grundle; Damian; Schütte; Florian; Karstensen; Johannes; Löscher; Carolin R; Hauss; Helena; Wagner; Hannes; Loginova; Alexandra; Kiko; Rainer; Silva; P; Tanhua; Toste; Körtzinger; Arne
发布日期2016-09-30
数据集类型dataset
英文简介The occurrence of mesoscale eddies that develop suboxic environments at shallow depth (about 40-100 m) has recently been reported for the eastern tropical North Atlantic (ETNA). Their hydrographic structure suggests that the water mass inside the eddy is well isolated from ambient waters supporting the development of severe near-surface oxygen deficits. So far, hydrographic and biogeochemical characterization of these eddies was limited to a few autonomous surveys, with the use of moorings, under water gliders and profiling floats. In this study we present
空间范围Median Latitude: 18.892513 * Median Longitude: -24.328921 * South-bound Latitude: 18.587500 * West-bound Longitude: -24.401733 * North-bound Latitude: 19.262933 * East-bound Longitude: -24.199350
时间范围2014-03-06T05:09:00 - 2014-03-07T07:27:52
语种英语
国家国际
学科大类气候变化
学科子类气候变化
文献类型数据集
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/215388
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Fiedler,Björn,Grundle,et al. Oxygen Utilization and Downward Carbon Flux in an Oxygen-Depleted Eddy in the Eastern Tropical North Atlantic.2016-09-30.https://doi.org/10.1594/PANGAEA.865177.
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