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塔克拉玛干沙漠南缘近地层风温湿廓线与能量交换特征

付光祥 何清 王勇辉 马明杰 阴璐璐 张乾

干旱区地理2024,Vol.47Issue(1):68-80,13.
干旱区地理2024,Vol.47Issue(1):68-80,13.DOI:10.12118/j.issn.1000-6060.2023.445

塔克拉玛干沙漠南缘近地层风温湿廓线与能量交换特征

Characteristics of wind,temperature,humidity profiles and energy exchange in the surface layer in the southern edge of Taklimakan Desert

付光祥 1何清 2王勇辉 3马明杰 1阴璐璐 1张乾4

作者信息

  • 1. 新疆师范大学地理科学与旅游学院/新疆干旱区湖泊环境与资源重点实验室,新疆 乌鲁木齐 830054||中国气象局乌鲁木齐沙漠气象研究所/新疆塔克拉玛干沙漠气象国家野外科学观测研究站/中国气象局塔克拉玛干沙漠气象野外科学试验基地/新疆沙漠气象与沙尘暴重点实验室,新疆 乌鲁木齐 830002
  • 2. 中国气象局乌鲁木齐沙漠气象研究所/新疆塔克拉玛干沙漠气象国家野外科学观测研究站/中国气象局塔克拉玛干沙漠气象野外科学试验基地/新疆沙漠气象与沙尘暴重点实验室,新疆 乌鲁木齐 830002
  • 3. 新疆师范大学地理科学与旅游学院/新疆干旱区湖泊环境与资源重点实验室,新疆 乌鲁木齐 830054
  • 4. 民丰县气象局,新疆 民丰 848599
  • 折叠

摘要

Abstract

The southern edge of the Taklimakan Desert of China belongs to the desert-oasis ecological transition zone,and the temporal and spatial changes in land surface properties are significant.The underlying surface prop-erties and hydrothermal characteristics are unique.Therefore,it is of great significance to investigate the charac-teristics of micrometeorological elements in this region for future climate change.Based on meteorological ele-ment data measured through the land-atmosphere interaction observatory on the northern side of the Tibetan Pla-teau in 2022,the wind,temperature,and humidity profile structure,radiation flux,and energy exchange character-istics of the ecological transition zone on the southern edge of the Taklimakan Desert were analyzed.The results show the following:(1)The wind speed,temperature,and specific humidity of the southern margin of the Takli-makan Desert change significantly with increasing altitude,and the temperature and specific humidity profiles of the inversion and humidity inversions occur in the temperature and specific humidity profiles,the heights of the inversion layer and the inversion humidity layer reach 30 m,the maximum average wind speed occurs in spring at 6.23 m·s-1,and the maximum average temperature and specific humidity are 28.93℃and 6.36 g·kg-1 in sum-mer,respectively.(2)The surface radiation balance of the four seasons is mainly positive,and there are differenc-es in the peak size and occurrence time of each radiation component,among which downward shortwave radia-tion is affected by sand and dust weather,which is manifested in spring>autumn>summer>winter.The surface al-bedo was negatively correlated with the solar altitude angle and soil moisture,with an annual average of 0.326,with the highest in December(0.366)and the lowest in August(0.297).(3)Sensible heat,soil heat flux,and net radiation changed significantly in the four seasons;the latent heat changed steadily,fluctuating up and down with 0 W·m-2 as the center,and the energy consumption was dominated by sensible heat.The energy closure rates of the four seasons were 76%,82%,53%,and 48%,respectively,which were manifested in summer>spring>au-tumn>winter.(4)The effective energy varies significantly in the four seasons,with positive values during the day and heat sources on the ground,indicating that the ground transports heat to the atmosphere,whereas,at night,it is the opposite,exhibiting spring>summer>autumn>winter.These findings can provide a scientific basis for the parameterization of land surface processes in the southern edge of the Taklimakan Desert in the future and im-prove the understanding of land surface processes in this area.

关键词

生态过渡区/风温湿廓线/辐射平衡/能量交换

Key words

ecological transition zone/wind temperature and humidity profile/radiation balance/energy ex-change

引用本文复制引用

付光祥,何清,王勇辉,马明杰,阴璐璐,张乾..塔克拉玛干沙漠南缘近地层风温湿廓线与能量交换特征[J].干旱区地理,2024,47(1):68-80,13.

基金项目

第三次新疆综合科学考察项目(2021xjkk030501) (2021xjkk030501)

国家自然科学基金项目(42030612)资助 (42030612)

干旱区地理

OA北大核心CSTPCD

1000-6060

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