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contributor authorRoosen, Robert G.
contributor authorAngione, Ronald J.
date accessioned2017-06-09T14:40:11Z
date available2017-06-09T14:40:11Z
date copyright1984/09/01
date issued1984
identifier issn0003-0007
identifier otherams-24091.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160725
description abstractA combination of published and archival observations from the Smithsonian Institution's Astrophysical Observatory (APO) is presented and analyzed. This paper concentrates on the data from the two primary sites?Mount Montezuma, Chile, and Table Mountain, California, from 1923 to 1957. Baseline values and their variations are presented for solar aureole brightness, precipitable water vapor, pyrheliometry, corrected pyrheliometry, and spectrobolometry. In addition to clouds and water vapor, possible causes for the observed variations in atmospheric transmission are volcanic eruptions, nuclear weapons testing, and aerosols from plants. Physical theories may not be sufficient to explain climate change, and considerations of biological processes may be required.
publisherAmerican Meteorological Society
titleAtmospheric Transmission and Climate: Results from Smithsonian Measurements
typeJournal Paper
journal volume65
journal issue9
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/1520-0477(1984)065<0950:ATACRF>2.0.CO;2
journal fristpage950
journal lastpage957
treeBulletin of the American Meteorological Society:;1984:;volume( 065 ):;issue: 009
contenttypeFulltext


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