作者: Michael S. McCartney , Lynne D. Talley
DOI: 10.1175/1520-0485(1982)012<1169:TSMWOT>2.0.CO;2
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摘要: Abstract The warm waters of the subtropical and subpolar basins North Atlantic have tight regional temperature-salinity relationships, are conventionally called “Central Waters.” A volumetric census characteristics by Wright Worthington (1970) shows that characterized certain segments T-S relationships large volumes compared to those other segments: “Mode Such Mode Waters appear as layers with increased vertical separation between isopycnals-pycnostads. present study reports on existence pycnostads in central eastern Atlantic. These Subpolar formed deep winter convection Atlantic, participate upper water circulation northern seasonal outcropping occurs within adjacent Current, Irminger East West Greenland Currents, and...