Major Components of Aerosols in North China: Desert Region and the Yellow Sea in the Spring and Summer of 1995 and 1996Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 009::page 1515DOI: 10.1175/1520-0469(2002)059<1515:MCOAIN>2.0.CO;2Publisher: American Meteorological Society
Abstract: Aerosol samples were collected from the northwest China desert region (i.e., Minqin), a coastal suburb area (i.e., Qingdao), and an island from the Yellow Sea (i.e., Qianliyan), respectively, in spring and summer of 1995 and 1996. Samples were analyzed for major components (Al, Ca, K, Mg, and Na), carbon (RAC), and sulphur (RAS). The results show that concentration of aerosols change considerably in time and space. The application of a three end-member-mixing model indicates that dust-dominated materials contribute up to 80%?90% of total aerosols when the cold fronts pass through over the Yellow Sea. The crust-dominated aerosols carried by cold front systems may well reduce the percentage concentrations of pollutant and sea salt over the Yellow Sea. The sea salt and regional aerosols become dominant fractions in atmosphere in summer when the dust storms expire in desert regions and the southeast monsoon starts in the subtropical Pacific Ocean.
|
Collections
Show full item record
| contributor author | Zhang, J. | |
| contributor author | Wu, Y. | |
| contributor author | Liu, C. L. | |
| contributor author | Shen, Z. B. | |
| contributor author | Zhang, Y. | |
| date accessioned | 2017-06-09T14:37:39Z | |
| date available | 2017-06-09T14:37:39Z | |
| date copyright | 2002/05/01 | |
| date issued | 2002 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-23100.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4159625 | |
| description abstract | Aerosol samples were collected from the northwest China desert region (i.e., Minqin), a coastal suburb area (i.e., Qingdao), and an island from the Yellow Sea (i.e., Qianliyan), respectively, in spring and summer of 1995 and 1996. Samples were analyzed for major components (Al, Ca, K, Mg, and Na), carbon (RAC), and sulphur (RAS). The results show that concentration of aerosols change considerably in time and space. The application of a three end-member-mixing model indicates that dust-dominated materials contribute up to 80%?90% of total aerosols when the cold fronts pass through over the Yellow Sea. The crust-dominated aerosols carried by cold front systems may well reduce the percentage concentrations of pollutant and sea salt over the Yellow Sea. The sea salt and regional aerosols become dominant fractions in atmosphere in summer when the dust storms expire in desert regions and the southeast monsoon starts in the subtropical Pacific Ocean. | |
| publisher | American Meteorological Society | |
| title | Major Components of Aerosols in North China: Desert Region and the Yellow Sea in the Spring and Summer of 1995 and 1996 | |
| type | Journal Paper | |
| journal volume | 59 | |
| journal issue | 9 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(2002)059<1515:MCOAIN>2.0.CO;2 | |
| journal fristpage | 1515 | |
| journal lastpage | 1532 | |
| tree | Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 009 | |
| contenttype | Fulltext |