The Cromwell current on the east side of the Galapagos Islands

Autor:	J. R. V. Zaneveld, Hasong Pak
Rok vydání:	1973
Předmět:	Atmospheric Science Ecology Paleontology Soil Science Forestry Aquatic Science Oceanography Current (stream) Geophysics Space and Planetary Science Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Upwelling Geology Earth-Surface Processes Water Science and Technology
Zdroj:	Journal of Geophysical Research. 78:7845-7859
ISSN:	0148-0227
DOI:	10.1029/jc078i033p07845
Popis:	What happens to the Cromwell Current as it passes the Galapagos Islands has been a topic of great interest ever since the discovery of the Cromwell Current itself. Montgomery [1962], in a review of the Cromwell Current, concluded that the Cromwell Current is usually weak or absent on the east side of the Galapagos Islands. Wyrtki [1966] said that the Cromwell Current disintegrates west of the Galapagos Islands and it splits into north and south branches, with a part of the water extending to the upwelling region off Peru. Knauss [1966], in his report on the Swan Song Expedition, the specific purpose of which  
Databáze:	OpenAIRE
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