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Ultraviolet radiation spatio-temporal characteristics derived from the ground-based measurements taken in China

机译:紫外线辐射的时空特征来源于中国的地面测量

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摘要

Ultraviolet (UV) radiation and broadband solar radiation (R_s) measured from January 2005 to June 2006 at 31 stations in Chinese Ecosystem Research Network (CERN) were used to investigate the spatio-temporal characteristics of UV radiation and UV fraction (the ratio of UV radiation to R_s) in China. Results indicated that the seasonal variations of UV radiation and R_s were consistent with the solar activities, which reached their lower values during winter period, and increased throughout the spring, peaking in June or July, in most sites. The Meiyu weather system and Southwest Monsoon produced different variation characteristics of UV radiation and R_s in subtropical and tropical regions. The UV fraction values showed a similar seasonal trend as that of UV radiation, which was mainly determined by the seasonal change of the aerosol optical depth (AOD) and water vapor content in atmosphere. The seasonal variations of UV fraction were much smoother in southern China due to high water vapor content over the whole year.rnThe UV radiation showed an increasing trend from east to west in China. In the western area, a simple increasing trend was observed from north to south, with the largest annual mean daily UV value 0.91 MJ m~(-2) appearing in the Qinghai-Tibet Plateau area. In east China there was a low center that appeared in the subtropical region due to high aerosol burden, with the lowest value 0.41 MJ m~(-2) observed in Yanting site. Two high centers were located in the tropics with higher solar altitudes and the north desert region with low atmospheric attenuation. The largest values of UV fraction appeared in the tropical and subtropical regions due to higher relative humidity (RH) in these areas. However, the smallest value did not appear in the north desert region where the RH was the lowest, they were found at the Luancheng site which featured relatively low humidity and abundant fine aerosols. The variations in the UV fraction were not such distinctive as those of the UV radiation in China due to the more complex influences of aerosol and water vapor.
机译:2005年1月至2006年6月在中国生态系统研究网(CERN)的31个站点测得的紫外线(UV)和宽带太阳辐射(R_s)用于研究紫外线辐射和紫外线分数(时空比率)的时空特征。辐射到中国)。结果表明,紫外线辐射和R_s的季节变化与太阳活动一致,在冬季期间达到了较低的值,并在整个春季增加,在大多数地点在6月或7月达到峰值。梅雨天气系统和西南季风在亚热带和热带地区产生不同的紫外线辐射和R_s变化特征。 UV分数值显示出与UV辐射相似的季节趋势,这主要由气溶胶光学深度(AOD)和大气中水汽含量的季节变化决定。由于全年水汽含量较高,中国南方地区紫外线分率的季节变化更为平稳。rn中国的紫外线辐射呈从东向西增加的趋势。在西部地区,从北向南观察到简单的增加趋势,最大的年平均日紫外线值出现在青藏高原地区,为0.91 MJ m〜(-2)。在华东地区,由于气溶胶负荷较高,在亚热带地区出现了一个低中心,在盐亭地区观测到的最低值为0.41 MJ m〜(-2)。两个高中心位于热带,太阳高度较高,而北部沙漠地区的大气衰减较小。由于这些地区较高的相对湿度(RH),UV分数的最大值出现在热带和亚热带地区。但是,在相对湿度最低,气溶胶含量较低的栾城县发现的相对湿度最低的北部沙漠地区没有出现最小值。由于气溶胶和水蒸气的影响更为复杂,因此紫外线分率的变化不像中国的紫外线辐射那样明显。

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