Aerosols of the Trade Wind RegionSource: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 006::page 611Author:Hogan, Austin W.
DOI: 10.1175/1520-0450(1976)015<0611:AOTTWR>2.0.CO;2Publisher: American Meteorological Society
Abstract: A series of aerosol and meteorological observations have been obtained for the trade wind region, from a meteorological tower on the north shore of Oahu. These observations have been supported by aircraft experiments, and observations at the Mauna Loa Observatory. The mean surface concentration found in trade winds is 242 cm?3, the median 262 cm?3, but extreme variation over the range 30 to more than 400 cm?3 occurs. This extreme variation is similar in amplitude to the spatial variation in the vicinity of cumulus clouds, and in agreement with the periodicities in aerosol concentration described by Blanchard. A similar aerosol concentration, of much smaller particles, is found above the trade inversion. This aerosol exhibits less short-term variation than that at the surface, and is the same at the Mauna Loa Observatory as at several miles seaward. This above-inversion aerosol may be representative of the world background tropospheric aerosol.
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| contributor author | Hogan, Austin W. | |
| date accessioned | 2017-06-09T17:38:38Z | |
| date available | 2017-06-09T17:38:38Z | |
| date copyright | 1976/06/01 | |
| date issued | 1976 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-9093.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232543 | |
| description abstract | A series of aerosol and meteorological observations have been obtained for the trade wind region, from a meteorological tower on the north shore of Oahu. These observations have been supported by aircraft experiments, and observations at the Mauna Loa Observatory. The mean surface concentration found in trade winds is 242 cm?3, the median 262 cm?3, but extreme variation over the range 30 to more than 400 cm?3 occurs. This extreme variation is similar in amplitude to the spatial variation in the vicinity of cumulus clouds, and in agreement with the periodicities in aerosol concentration described by Blanchard. A similar aerosol concentration, of much smaller particles, is found above the trade inversion. This aerosol exhibits less short-term variation than that at the surface, and is the same at the Mauna Loa Observatory as at several miles seaward. This above-inversion aerosol may be representative of the world background tropospheric aerosol. | |
| publisher | American Meteorological Society | |
| title | Aerosols of the Trade Wind Region | |
| type | Journal Paper | |
| journal volume | 15 | |
| journal issue | 6 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1976)015<0611:AOTTWR>2.0.CO;2 | |
| journal fristpage | 611 | |
| journal lastpage | 619 | |
| tree | Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 006 | |
| contenttype | Fulltext |