陈隆勋,段庭扬,李维亮. 1985. 1979年夏季青藏高原上空大气热源的变化及大气能量收支特性[J]. 气象学报, 43(1):1-12, doi:10.11676/qxxb1985.001
1979年夏季青藏高原上空大气热源的变化及大气能量收支特性
THE VARIATION OF THE ATMOSPHERIC HEAT SOURCE AND THE BUDGET OF ATMOSPHERIC ENERGY ON THE QINGHAI-XIZANG PLATEAU DURING SUMMER 1979
投稿时间:1983-01-07  修订日期:1983-06-05
DOI:10.11676/qxxb1985.001
中文关键词:  
英文关键词:
基金项目:
作者单位
陈隆勋 中国科学院大气物理研究所 
段庭扬 成都气象学院 
李维亮 国家气象局气象科学研究院 
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中文摘要:
      本文把青藏高原分成东西两个区,各区取5个站组成一个5边形,研究该两区1979年夏季的垂直运动、大气总加热、凝结加热、各种大气能量转换和输送、不均匀非绝热加热的特性,特别是其垂直分布和谱密度和交叉谱特性.其结果见第5节中结论.
英文摘要:
      In this paper, the vertical velocity ω, the large-scale apparent heat source Q1 the moisture sink Q2, the atmospheric energy transformation are computed daily for the subareas over the Oinghai-Xizang plateau during summer 1979. The western subarea is bounded by Lhasa, Nagqa, Shuanghu,Gerze and Zhongba stations(fig. 1) The last three stations were established for the purpose of the Oinghai-Xizang Plateau Meteorology Experiment of summer 1979.The eastern subarea is bounded by Lasa, Nagqa, Yushu, Ganzi and Deqing stations. Moreover, a spectral analysis was made for the above mentioned elements. Fig.5 shows computed results of the cycle of energy tramsformation averaged for the whole summer.
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