Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q1190478> ?p ?o }
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- Q1190478 subject Q21400605.
- Q1190478 subject Q7007096.
- Q1190478 abstract "The 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. It is hidden 300 feet (100 m) under the surface of the Pacific Ocean at the Equator and is relatively shallow compared to other ocean currents being only 100 feet from top to base. It has 1000 times the volume of Mississippi River and its length is 3500 miles (6000 km).".
- Q1190478 wikiPageWikiLink Q1250263.
- Q1190478 wikiPageWikiLink Q129558.
- Q1190478 wikiPageWikiLink Q1337681.
- Q1190478 wikiPageWikiLink Q1497.
- Q1190478 wikiPageWikiLink Q206668.
- Q1190478 wikiPageWikiLink Q21400605.
- Q1190478 wikiPageWikiLink Q23538.
- Q1190478 wikiPageWikiLink Q2467321.
- Q1190478 wikiPageWikiLink Q38095.
- Q1190478 wikiPageWikiLink Q43518.
- Q1190478 wikiPageWikiLink Q7007096.
- Q1190478 wikiPageWikiLink Q7830169.
- Q1190478 wikiPageWikiLink Q7939.
- Q1190478 wikiPageWikiLink Q930179.
- Q1190478 wikiPageWikiLink Q97.
- Q1190478 wikiPageWikiLink Q98.
- Q1190478 wikiPageWikiLink Q981348.
- Q1190478 comment "The 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.".
- Q1190478 label "Cromwell Current".