LIU KWANG-NAN, Wu HUNG-SHUN. 1956: A PRELIMINARY STUDY ON THE DETERMINATION OF NATURAL SYNOPTIC SUMMER SEASON OVER ASIATIC NATURAL SYNOPTIC REGION AND THE PREVAILING WEATHER PROCESS IN THIS SEASON. Acta Meteorologica Sinica, (3): 219-242. DOI: 10.11676/qxxb1956.017
Citation: LIU KWANG-NAN, Wu HUNG-SHUN. 1956: A PRELIMINARY STUDY ON THE DETERMINATION OF NATURAL SYNOPTIC SUMMER SEASON OVER ASIATIC NATURAL SYNOPTIC REGION AND THE PREVAILING WEATHER PROCESS IN THIS SEASON. Acta Meteorologica Sinica, (3): 219-242. DOI: 10.11676/qxxb1956.017

A PRELIMINARY STUDY ON THE DETERMINATION OF NATURAL SYNOPTIC SUMMER SEASON OVER ASIATIC NATURAL SYNOPTIC REGION AND THE PREVAILING WEATHER PROCESS IN THIS SEASON

  • The synoptic process on 500mb over Asiatic natural synoptic region have been analized for 5 summers.The results are given below:1.The variation of the position and strength of the maximum westerly wind belt at 500mb surface along four meridians 65°E,105°E,120°E,140°E gives a good index in determing the natural synoptic seasons over Eastern Asiatic synoptic natural region.The disappearence of the low latitude westerly wind maximum along 65°E is the first indication of the beginning of Bai-Ü period.When the westerlies wind maximum belt to the south of 40°N completely disappears along 140°E summer begins.This is accompanied with the filling of the Asiatic main trough over Japan and the Northward shift of the Pacific subtropical high pressure belt from low latitudes to 30°-40°N.The mean date on which summer begins is nearly on 13th,July.It is also the end of Bai-Ü over middle Yangtze river.Thence the synoptic process in Bai-Ü period is the prevailing process before summer season.The precipitation in this period is closely related to the strength of the maximum wind belt i.e.socalled frontal zone.
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