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范子昂,陆恒.中国天山西部森林积雪短波辐射收支特征[J].沙漠与绿洲气象,2020,14(5):136~143
中国天山西部森林积雪短波辐射收支特征
The characteristic of shortwave radiation to snow beneath forest canopies of the Western Tianshan Mountains, China
投稿时间:2018-08-10  修订日期:2018-09-26
DOI:10.12057/j.issn.1002-0799.2020.05.018
中文关键词:  森林积雪  短波辐射  短波辐射透射率
英文关键词:forest snow  shortwave radiation  shortwave transmissivity
基金项目:国家自然科学基金(41741014, 41401089), 中国科学院西部之光-西部博士项目(2015-XBQN-B-24),中央级公益性科研院所基本科研业务费(IDM2016007)
作者单位E-mail
范子昂 新疆金锋华云气象科技有限公司 franz1326@163.com 
陆恒* 四川师范大学地理与资源科学学院  
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中文摘要:
      本文通过对中国科学院天山积雪与雪崩研究站不同开阔度森林下积雪表面短波辐射的观测研究,分析了森林积雪短波辐射收支特征,短波辐射透射率。结果表明:阴坡林下积雪表面短波辐射小于阳坡,且随森林开阔度的减小而减小;林下雪面短波辐射和净短波辐射随太阳高度角增加而逐渐增加,不同开阔度林下雪面短波辐射和净短波辐射的差异也随太阳高度角的增加而不断增大;阳坡、阴坡林冠上方和80%开阔度林下积雪短波辐射在晴天日变化呈单峰型,林下积雪短波辐射峰值出现时间由林冠上方直接辐射和散射辐射的相对关系决定;多云天气,短波辐射的日变化特征取决于云量的变化;林冠开阔度越大,其短波辐射率越大,日平均短波辐射透射率随太阳高度角的增加而增加,且开阔度越大,其增加速率越快,短波辐射透射率日变化呈“U”型,早晚大于12:00~17:00。
英文摘要:
      Downward and upward shortwave radiation beneath different canopy openness forest were measured in Tianshan Research Station for Snow-cover and Avalanche of Chinese Academy of Sciences. The variation of shortwave radiation beneath forest canopy, shortwave transmissivity and the influence of intercept snow above forest crown on shortwave were analyzed. The results showed the downward shortwave radiation beneath forest canopy were less than that on the sunny slope, it decreased with canopy openness decreased. The downward and net shortwave radiation beneath forest canopy increased with solar elevation angle increased, the difference of downward and net shortwave radiation beneath forest canopy between different canopy openness forest also increased with solar elevation angle. In clear day, the daily variation of downward shortwave radiation in sunny slope, above forest canopy and beneath 80% canopy openness forest presented single peak type, the relative proportion of direct shortwave radiation and diffuse shortwave radiation decided the appeared time of downward shortwave radiation peak value. In cloudy day, the variation of downward shortwave radiation was mainly influenced by cloud cover. The sparser the forest was, the bigger the shortwave transmissivity was ,the daily average of shortwave radiation was increased with solar elevation angle increased. The sparser the forest was, the more the shortwave transmissivity increase. The daily variation of shortwave transmissivity presented “U” type, the value of shortwave transmissivity in the morning and evening were bigger than that in 12:00~17:00 period.
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