首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Disturbance of light-absorbing aerosols on the albedo in a winter snowpack of Central Tibet
Authors:Jing Ming  Pengling Wang  Shuyu Zhao and Pengfei Chen
Institution:1. National Climate Center, China Meteorological Administration, Beijing 100081, China ;State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
2. National Climate Center, China Meteorological Administration, Beijing 100081, China
3. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
4. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
Abstract:A field observation on the albedo of the snowpack in Central Tibet was conducted in the Nam Co region in the winter of 2011. Snow properties, including grain size and density, were measured in the field, and surface-layer snow samples (down to 5 cm) were collected. The average concentrations of black carbon and dust were 72 ppbm (close to that in the glaciers of Mt. Nyainqentanglha) and 120 ppmm, respectively. Inverse trends were found to exist between the albedo of the snowpack and light-absorbing aerosols (LAAs) as well as grain size growth. Modeling showed that black carbon, dust, and grain growth in the winter snowpack can reduce the broadband albedo by 11%, 28%, and 61%, respectively.
Keywords:albedo  black carbon  dust  snow  Tibetan Plateau
本文献已被 CNKI 维普 万方数据 ScienceDirect 等数据库收录!
点击此处可从《环境科学学报(英文版)》浏览原始摘要信息
点击此处可从《环境科学学报(英文版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号