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首页|期刊导航|干旱区地理|塔克拉玛干沙漠南缘戈壁下垫面辐射平衡与地表反照率特征

塔克拉玛干沙漠南缘戈壁下垫面辐射平衡与地表反照率特征

邢立文 赵景峰 何清 李娟 苏华丽 何亚玲

干旱区地理2024,Vol.47Issue(5):762-772,11.
干旱区地理2024,Vol.47Issue(5):762-772,11.DOI:10.12118/j.issn.1000-6060.2023.535

塔克拉玛干沙漠南缘戈壁下垫面辐射平衡与地表反照率特征

Radiation balance and surface albedo characteristics of the gobi underlying surface in the southern margin of the Taklimakan Desert

邢立文 1赵景峰 1何清 2李娟 1苏华丽 1何亚玲1

作者信息

  • 1. 四川师范大学地理与资源科学学院,四川 成都 610068||四川师范大学西南土地资源评价与监测教育部重点实验室,四川 成都 610068
  • 2. 中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐 830002
  • 折叠

摘要

Abstract

The gobi,a prominent terrain feature in desert regions,exhibits surface characteristics markedly dis-tinct from those of typical desert terrains.Therefore,it is imperative to investigate the radiation balance properties of the gobi's surface in desert environments to enhance the accuracy of parameters used in land-atmosphere ener-gy exchange models,particularly in the Taklimakan Desert.Utilizing continuous observational data from the Qira gobi station,situated on the southern periphery of the Taklimakan Desert as part of the China-Japan Sand and Dust Storm Cooperation Project(ADEC),this study examines the diurnal variations in the components of surface radiation balance at the Qira gobi station throughout the year,across different seasons,and under various weather conditions.The findings indicate that:(1)The peak values for radiation components at the Qira gobi station are typically observed in July,with the exception of upward shortwave radiation,which peaks in January.(2)The di-urnal variation maxima for downward and upward shortwave radiation are recorded in spring,whereas the peak values for downward longwave radiation,upward longwave radiation,and net radiation are noted in summer.(3)During sunny days,the radiation components exhibit a consistent trend across seasons,whereas under cloudy,overcast,and rainy conditions,their variations are erratic.Specifically,during precipitation events,both down-ward and upward longwave radiations significantly surpass the levels of other components.(4)The annual aver-age surface albedo is calculated at 0.32.Notably,the albedo increases substantially during winter owing to snow cover,with the seasonal sequence from highest to lowest being winter,spring,autumn,and summer.The diurnal albedo variation,influenced by the solar zenith angle,forms a smooth"U"shape on clear days,whereas it fluctu-ates irregularly under different weather conditions.

关键词

辐射平衡/净辐射/地表反照率/戈壁下垫面

Key words

radiation balance/net radiation/surface albedo/gobi subsurface cushion

引用本文复制引用

邢立文,赵景峰,何清,李娟,苏华丽,何亚玲..塔克拉玛干沙漠南缘戈壁下垫面辐射平衡与地表反照率特征[J].干旱区地理,2024,47(5):762-772,11.

基金项目

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

干旱区地理

OA北大核心CSTPCD

1000-6060

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