The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance
Measurements of broadband spectral absorption of solar radiation by the Arctic atmosphere during haze events are reported. A preliminary analysis of the data indicates that large changes occur in the radiative transfer processes in the Arctic during haze events. For example, the planetary albedo is...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19840051515 2023-05-15T13:10:46+02:00 The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance Valero, F. P. J. Ackerman, T. P. Gore, W. J. Y. Unclassified, Unlimited, Publicly available May 1, 1984 http://ntrs.nasa.gov/search.jsp?R=19840051515 unknown http://ntrs.nasa.gov/search.jsp?R=19840051515 Accession ID: 84A34302 Copyright Other Sources 47 Geophysical Research Letters; 11; 465-468 1984 ftnasantrs 2012-02-15T15:53:14Z Measurements of broadband spectral absorption of solar radiation by the Arctic atmosphere during haze events are reported. A preliminary analysis of the data indicates that large changes occur in the radiative transfer processes in the Arctic during haze events. For example, the planetary albedo is estimated to increase by 2.5 percent over the ocean and to decrease by 9 percent over the ice cap. Changes of such magnitude in the radiative parameters have the potential for significant climatic effects. The need for further experimental and modeling efforts is emphasized. Other/Unknown Material albedo Arctic Ice cap NASA Technical Reports Server (NTRS) Arctic |
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NASA Technical Reports Server (NTRS) |
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unknown |
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47 |
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47 Valero, F. P. J. Ackerman, T. P. Gore, W. J. Y. The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
topic_facet |
47 |
description |
Measurements of broadband spectral absorption of solar radiation by the Arctic atmosphere during haze events are reported. A preliminary analysis of the data indicates that large changes occur in the radiative transfer processes in the Arctic during haze events. For example, the planetary albedo is estimated to increase by 2.5 percent over the ocean and to decrease by 9 percent over the ice cap. Changes of such magnitude in the radiative parameters have the potential for significant climatic effects. The need for further experimental and modeling efforts is emphasized. |
format |
Other/Unknown Material |
author |
Valero, F. P. J. Ackerman, T. P. Gore, W. J. Y. |
author_facet |
Valero, F. P. J. Ackerman, T. P. Gore, W. J. Y. |
author_sort |
Valero, F. P. J. |
title |
The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
title_short |
The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
title_full |
The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
title_fullStr |
The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
title_full_unstemmed |
The absorption of solar radiation by the Arctic atmosphere during the haze season and its effects on the radiation balance |
title_sort |
absorption of solar radiation by the arctic atmosphere during the haze season and its effects on the radiation balance |
publishDate |
1984 |
url |
http://ntrs.nasa.gov/search.jsp?R=19840051515 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic Ice cap |
genre_facet |
albedo Arctic Ice cap |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19840051515 Accession ID: 84A34302 |
op_rights |
Copyright |
_version_ |
1766242024313323520 |