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1961~2009年我国地面太阳辐射变化特征及云对其影响的研究
引用本文:杨溯,石广玉,王标,杨红龙,段云霞. 1961~2009年我国地面太阳辐射变化特征及云对其影响的研究[J]. 大气科学, 2013, 37(5): 963-970. DOI: 10.3878/j.issn.1006-9895.2013.11122
作者姓名:杨溯  石广玉  王标  杨红龙  段云霞
作者单位:1.国家气象信息中心, 北京100081
基金项目:国家重点基础研究发展计划项目(973计划)2010CB950502;中国科学院战略性先导科技专项XDA05100504
摘    要:基于我国100个地面站点的地面太阳总辐射、日平均云量资料分析1961~2009年我国地面太阳辐射(Surface Solar Radiation,SSR)变化特征及云在不同时期对SSR的影响。结果显示:1961~2009年我国SSR经历了先下降后上升的变化过程,其中1961~1990年SSR显著下降("变暗"),下降速率为-4.3%/10 a(7.87 W m–2(10 a)–1),各地SSR变化趋势比较一致;1990年后SSR开始上升("变亮"),上升速率为2.8%/10 a(2.4 W m–2(10 a)–1),各地SSR变化趋势不如前一阶段一致,但没有显著的地域分布特征。晴空条件的设置对1961~1990年各站点SSR变化特征影响不大,仍为大范围下降("变暗"),但对1990~2009年的结果影响显著。相比全天空条件的结果,晴空条件下1990~2009年我国SSR变化有明显的南北特征,南方地区以"变亮"为主,而北方地区大多继续"变暗",但"变暗"速度减缓。1961~1990年我国总云量总体呈小幅下降趋势,下降速率很慢,这一时期总云量与全天空SSR没有很好的对应关系;1990~2009年我国总云量总体呈小幅上升趋势,有显著的南北分布差异,北方地区以上升趋势为主,南方地区以下降趋势为主,期间云量与全天空情况下SSR有很好的对应关系。这些结果表明,在"变暗"阶段,云对SSR的作用不显著,而在"变亮"阶段,云的作用变得较为突出。

关 键 词:地面太阳辐射     全球变暗   全球变亮
收稿时间:2012-03-05
修稿时间:2013-02-19

Trends in Surface Solar Radiation (SSR) and the Effect of Clouds on SSR during 1961-2009 in China
YANG Su,SHI Guangyu,WANG Biao,YANG Honglong and DUAN Yunxia. Trends in Surface Solar Radiation (SSR) and the Effect of Clouds on SSR during 1961-2009 in China[J]. Chinese Journal of Atmospheric Sciences, 2013, 37(5): 963-970. DOI: 10.3878/j.issn.1006-9895.2013.11122
Authors:YANG Su  SHI Guangyu  WANG Biao  YANG Honglong  DUAN Yunxia
Affiliation:1.National Meteorological Information Centre, Beijing 1000812.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 1000293.Shenzhen National Climate Observatory, Shenzhen Meteorological Bureau, Shenzhen 5180404.Shenyang Meteorological Service, Shenyang 110016
Abstract:This study investigates variations in surface solar radiation (SSR) and the effects of cloud on SSR during 1961-2009 based on global radiation and cloud fraction data from 100 radiation observation sites over China. The results indicate a general decrease of -4.3%/10a (7. 87 W m-2 (10 a)-1) in SSR over land surfaces since measurements began (in about 1961) until 1990, with a turnover corresponding to a 2.8%/10a (2.4 W m-2 (10a)-1) increase from 1990 onward. Moreover, this turnover was more significant in southern China. It seems that cloud was not one of the primary factors inducing global dimming during 1961-1990, based on the similar variation characteristics witnessed under all-sky and clear-sky conditions and the weak correlation between total cloud fraction and SSR. However, there were distinct differences between all-sky and clear-sky SSR results after 1990 and it shows a significant negative correlation between all-sky and clear-sky SSR values. Thus, it may be concluded that cloud had a significant effect on SSR variation, such that it may have inhibited global brightening in some way during 1990-2009.
Keywords:Surface solar radiation  Cloud  Global dimming  Global brightening
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