Evidence of Subarctic Water Mass Intrusions at Ocean Weather Station November.

A divergent heat budget equation which included the effects of surface heat flux, horizontal and vertical advection, and horizontal divergence on the near-surface heat content was used to examine the role of thermal advection in the upper 250m of the water column at Ocean Weather Station NOVEMBER. T...

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Bibliographic Details
Main Authors: Pfeiffer,John Francis, Bourke,Robert H
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CALIF
Format: Text
Language:English
Published: 1976
Subjects:
Physical and Dynamic Oceanography
*NORTH PACIFIC OCEAN
*MARINE GEOPHYSICS
HEAT TRANSFER
COMPUTATIONS
LAYERS
MIXTURES
OCEANOGRAPHIC DATA
SEASONAL VARIATIONS
VERTICAL ORIENTATION
HORIZONTAL ORIENTATION
EQUATIONS
SALINITY
AIR WATER INTERACTIONS
WEATHER STATIONS
HEAT FLUX
SEA WATER
ADVECTION
HEAT BALANCE
GRADIENTS
ARCTIC OCEAN
Ocean Weather Station NOVEMBER
Arctic
Arctic Ocean
Pacific
Subarctic
Online Access:http://www.dtic.mil/docs/citations/ADA032057
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA032057
Description
Summary:A divergent heat budget equation which included the effects of surface heat flux, horizontal and vertical advection, and horizontal divergence on the near-surface heat content was used to examine the role of thermal advection in the upper 250m of the water column at Ocean Weather Station NOVEMBER. This station is located on the southern boundary of the transition zone separating the Subarctic water mass from the Subtropic water mass. Values for horizontal thermal advection changes were computed over the period 1962-1970. This term was correlated with salinity fluctuations over the period 1968-1970. Pulse-like periods of cool advection were associated with periods of reduced salinities suggesting these were intrusions of Subarctic water. Over the nine-year period of analysis, these intrusions had a periodicity of 7 to 8 months with a duration of 3 to 4.5 months. It is suggested these wave-like intrusions along the Subtropic front are the result of the passage of non-dispersive baroclinic Rossby waves. (Author) Master's thesis.

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