Seasonal variation of rain-belts over China
Tóm tắt
Decadal rainfall data of 228 stations in 1951–1970 and upper-wind records in 1960–1969 published by the Central Meteorological Bureau and relevant provincial organizations are employed in the analysis. It is found that the characteristic features of seasonal variation of the main rain-belts over eastern China to the east of 105°F are quite different from those to the west, over the Qinghai-Xizhang (Tibetan) Plateau. The eastern rain-belts are closely related to the low level flow convergence lines and significantly influenced by the south Asian high and the western Pacific subtropical high.
Tài liệu tham khảo
陶 诗言等, 气象学报, 29(1958), 2: 119-133.
高 由禧, 郭 其蕴, 气象学报, 29(1958), 264-273.
段月薇, 许孟英, 地理集刑, 第11 号, 科学出版社, 1979, 40–49.
张家诚, 中央气象研究所论文汇集, 1965.
王 德瀚, 气象学报, 39(1981), 2:252-256.
徐国昌, 长期天气预报文集,气象出版社, 1981.
兰州高原大气所, 青藏高原, 象论文选编, 1974.
徐国昌、李梅芳, 青藏高原的雨季 北方天气文集 (5), 北京大学出版社, 1984, 54–63.
刘匡南等, 气象学报, 27(1956), 3期.
叶 笃正 等, 气象学报, bd29(1958), 4: 249-263.
李 麦村、 徐 国昌, 地理科学, 3(1983), 1:1-10.