1. Cromwell CurrentThe Cromwell Current (also called Pacific Equatorial Undercurrent or just Equatorial Undercurrent) is an eastward-flowing subsurface current that extends the length of the equator in the Pacific Ocean. The Cromwell Current was discovered in 1952 by Townsend Cromwell, a researcher with the Honolulu Laboratory. It is 250 miles (400 km) wide and flows to the east.
Read “Cromwell Current” on English Wikipedia
Read “赤道潜流” on Japanese Wikipedia
Read “Cromwell Current” on DBpedia
Read “Cromwell Current” on English Wikipedia
Read “赤道潜流” on Japanese Wikipedia
Read “Cromwell Current” on DBpedia
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