A MODEL CLIMATOLOGY OF THE OCEANIC THERMAL STRUCTURE AS APPLIED TO SINGLE STATION ANALYSIS

A model of the seasonal thermocline is presented. The model, based on parameters deduced from climatic data from ocean stations located in the Subarctic domain (north of the Gulf Stream-North Atlantic Current system), describes the onset, growth, and decay of the seasonal thermocline. However, owing...

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Bibliographic Details
Main Author: Corton, Edward L.
Other Authors: NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Format: Text
Language:English
Published: 1966
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0489565
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0489565
Description
Summary:A model of the seasonal thermocline is presented. The model, based on parameters deduced from climatic data from ocean stations located in the Subarctic domain (north of the Gulf Stream-North Atlantic Current system), describes the onset, growth, and decay of the seasonal thermocline. However, owing to lack of data below 400 feet, the model does not delineate the convective layer in mid-winter. Temporal changes in temperature gradients above, within, and below the thermocline are discussed.