A Technique for Predicting South China Sea Tropical Cyclones.

Abstract

The low-level cyclonic shear zone in the South China Sea is investigated as a possible precursor of tropical storm activity within the South China Sea. For tropical storm genesis in this area, it is shown that the strength of the cyclonic shear zone reaches a critical intensity approximately 24 to 48 hours before cyclogenesis takes place. Also, if the cyclonic shear zone is not present and there is either a large-scale ridge or easterly flow across the South China Sea, then tropical storm genesis does not take place for at least a week. With respect to tropical storms approaching the South China Sea from the Philippine Sea, the presence of a cyclonic shear zone is a good indication that the tropical storm will move into the area. On the other hand, when a large-scale low-level ridge is present over the area, these storm recurve northward and will not enter the South China Sea. (Author)

Document Details

Document Type
Technical Report
Publication Date
May 01, 1969
Accession Number
AD0780209

Entities

People

  • J. D. Jarrell
  • L. R. Brody

Tags

DTIC Thesaurus Topics

  • Cyclogenesis
  • Cyclones
  • Intensity
  • Landforms
  • Philippine Sea
  • Precursors
  • Ridges
  • South China Sea
  • Tropical Cyclones

Fields of Study

  • Environmental science

Readers

  • Asian Economic Studies
  • Atmospheric Science/Meteorology