globalchange  > 气候减缓与适应
DOI: 10.1029/2018JC013813
Scopus记录号: 2-s2.0-85052632857
论文题名:
Hydrography of the Central and Western Gulf of Mexico
作者: Portela E.; Tenreiro M.; Pallàs-Sanz E.; Meunier T.; Ruiz-Angulo A.; Sosa-Gutiérrez R.; Cusí S.
刊名: Journal of Geophysical Research: Oceans
ISSN: 21699275
出版年: 2018
卷: 123, 期:8
起始页码: 5134
结束页码: 5149
语种: 英语
英文关键词: 18C Sargasso Sea Water ; extensive database ; hydrography of the Gulf of Mexico ; new data inside Loop Current Eddies ; thermohaline properties and dissolved oxygen of water masses ; water masses inside and outside Loop Current Eddies
英文摘要: This study describes in detail the water masses of the Gulf of Mexico (GoM) west of 88°W based on their thermohaline properties and dissolved oxygen concentration. The existent historical information is complemented with new data from 14 cruises, Argo floats, and over one year of continuous glider monitoring. The results describe the general hydrography of the central and western GoM with focus on the difference between the water properties inside and outside Loop Current Eddies (LCEs). Caribbean Surface Water, Subtropical Underwater, and 18 °C Sargasso Sea Water (18SSW) are exclusive of the LCEs, and they are found along the LCEs preferred path between 23°N and 27°N. Outside the LCEs, the prominent characteristics of these water masses erode, and the Gulf Common Water is ubiquitous in the subsurface. It is shown that the water masses in the GoM need to be described in the frame of the dominant mesoscale features that take place there and that the dissolved oxygen is a key variable to identify some water masses of Caribbean origin as the Tropical Atlantic Central Water and the 18SSW. The previous potential temperature and salinity limits of the water masses within the GoM were revised and redefined in terms of absolute salinity and conservative temperature in the frame of the Thermodynamic Equation of Seawater, 2010 (TEOS-10). While temperature values after conversion have little variation compared to the previous ones, the absolute salinity is in average 0.2 units greater than the former practical salinity. ©2018. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/113306
Appears in Collections:气候减缓与适应

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作者单位: Departamento de Oceanografía Física, Centro de Investigación Científica y Educación Superior de Ensenada, Ensenada, Mexico; Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de Mexico, Mexico City, Mexico

Recommended Citation:
Portela E.,Tenreiro M.,Pallàs-Sanz E.,et al. Hydrography of the Central and Western Gulf of Mexico[J]. Journal of Geophysical Research: Oceans,2018-01-01,123(8)
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