Altimeter Measurements of Wind and Wave Modulation by the Kuroshio in the Yellow and East China Seas

Abstract

The Kuroshio is the major ocean current conveying heat and water mass in the Pacific Ocean. The impact of the Kuroshio on regional wind and wave distributions has been studied with spaceborne-altimeter measurements in the Yellow and East China Seas. In this region the Kuroshio trajectory is relatively stationary and the monsoon patterns dominate, making it an ideal natural laboratory for large scale air-sea-current interaction research. Major findings from this study include: (a) the Kuroshio exerts significant influence on the wind and wave distributions over a swath about 800-kim wide along its path. (b) Seasonal average wind speeds reach a maximum near the Kuroshio axis. The magnitude of enhancement ranges between 20 and 50 percent. (c) The distribution of the surface wave heights displays similar spatial patterns to the wind-speed distribution. The Kuroshio effects on wave heights are further complicated by the hydrodynamic modulation of wave-current interaction and the influence of thermal stratification on wind-wave generation. (d) Kuroshio effects are most prominent in the first and last quarters of the year, and least prominent in the third quarter.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 2005
Accession Number
ADA449216

Entities

People

  • Paul Hwang

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Space

DTIC Thesaurus Topics

  • Boundaries
  • Climatology
  • Differential Equations
  • East China Sea
  • Equations
  • Gulf Stream
  • Measurement
  • Military Research
  • Ocean Currents
  • Ocean Waves
  • Oceanography
  • Oceans
  • Pacific Ocean
  • Partial Differential Equations
  • Surface Waves
  • Trajectories
  • Yellow Sea

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Atmospheric Science/Meteorology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers