Lagrangian Measurements of Velocity and Upper Ocean Temperature and Salinity Fields in the Sea of Japan

The long-term goal of this project is to better understand the properties of the upper portion of the water column in the Japan Sea. It is important to understand the seasonal cycle in the upper 1000 m of the Japan Sea: how the Sea stratifies in spring and summer and how it forms a mixed layer in fa...

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Bibliographic Details
Main Author: Riser, Stephen C.
Other Authors: WASHINGTON UNIV SEATTLE SCHOOL OF OCEANOGRAPHY
Format: Text
Language:English
Published: 1998
Subjects:
Physical and Dynamic Oceanography
*SALINITY
*OCEANOGRAPHY
*LAGRANGIAN FUNCTIONS
*JAPAN SEA
SEASONAL VARIATIONS
WINTER
OCEANS
HYDROGRAPHY
SUBTROPICAL REGIONS
WATER
TEMPERATURE
MEASUREMENT
VELOCITY
MIXING
Subarctic
Online Access:http://www.dtic.mil/docs/citations/ADA538294
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA538294
Description
Summary:The long-term goal of this project is to better understand the properties of the upper portion of the water column in the Japan Sea. It is important to understand the seasonal cycle in the upper 1000 m of the Japan Sea: how the Sea stratifies in spring and summer and how it forms a mixed layer in fall and winter, sometimes with deep convection occurring. I want to be able to study the circulation and hydrography of the upper 1000 m of the Japan Sea over at least a few complete seasonal cycles in order to understand the process of mixed-layer formation and destruction there. In some ways the Japan Sea behaves as a subtropical ocean, and in other ways it is more like a subarctic one; as a result, it is a useful laboratory for studying many oceanographic processes that occur throughout the world ocean. I plan to use PALACE floats in this study, and the work discussed here will fit into a larger program in the Japan Sea with about 20 PIs. See also ADM002252.

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