THE CHARACTERISTICS OF LOW-LATITUDE FLOW PATTERNS OVER SOUTHEAST ASIA AND WESTERN PACIFIC FROM OCTOBER TO DECEMBER,

Abstract

Based on a study of the 1958 - 1959 data, the large-scale flow patterns over the Western Pacific at low latitudes in early winter may be classified into two types according to the vertical extent of the anticyclonic flow of the subtropical high, viz., the 'shallow subtropical high' type and the 'deep subtropical high' type. The former is characterized by a low zonal index at high latitudes and moderate development of easterly waves in the lower troposphere near the equator with the subtropical jet in phase with its mean position. The latter is characterized by a high zonal index at high latitudes and the presence of equatorial westerlies in the lower troposphere with the subtropical jet completely out of phase with its mean position. Typhoons may also form in the equatorial belt of convergence in the latter pattern. The sequential occurrence of these two types seems to follow a quasi-periodic oscillation with a period of about one month. (Author)

Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1966
Accession Number
AD0648052

Entities

People

  • Chen Shou-jun
  • Hsieh Yi-ping
  • Kuo Xiao-lun

Organizations

  • Emmanuel College

Tags

DTIC Thesaurus Topics

  • Asia
  • Convergence
  • Geographic Regions
  • Grids
  • Grids (Coordinates)
  • High Latitudes
  • Latitude
  • Oscillation
  • Republic
  • Southeast Asia
  • Troposphere

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology