Small Ice Caps in Climate Models
Introduction The presence of ice or snow at the surface of the Earth changes the reflectivity of the system to sunlight. When the planet is made colder by changing some control parameter such as the solar constant, ice caps grow; moreover, the increased reflectivity (albedo) of the ice-covered surfa...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.40.7978 2023-05-15T16:38:13+02:00 Small Ice Caps in Climate Models Gerald R. North Kwang-yul Kim Wan-ho Lee The Pennsylvania State University CiteSeerX Archives application/postscript http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.40.7978 http://chammp.met.fsu.edu/paper/ice_caps.ps en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.40.7978 http://chammp.met.fsu.edu/paper/ice_caps.ps Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://chammp.met.fsu.edu/paper/ice_caps.ps text ftciteseerx 2016-09-25T00:18:16Z Introduction The presence of ice or snow at the surface of the Earth changes the reflectivity of the system to sunlight. When the planet is made colder by changing some control parameter such as the solar constant, ice caps grow; moreover, the increased reflectivity (albedo) of the ice-covered surface causes an enhancement of the cooling. The effect of the ice-cap growth is to amplify the effects of an externally induced climate change. The ice-albedo mechanism is a positive feedback in the climate system. The climate system has many feedbacks, positive and negative. They play various roles in forced climate change. This lecture will concentrate on the effects of that one isolated feedback, since in this simplified form the problem becomes tractable and quasi-analytical solutions can be found. The ice-albedo feedback mechanism is a nonlinear phenomenon which leads to multiple solutions to the governing equations for fixed, prescribed values of the control parameters and bound Text Ice cap Unknown |
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ftciteseerx |
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English |
description |
Introduction The presence of ice or snow at the surface of the Earth changes the reflectivity of the system to sunlight. When the planet is made colder by changing some control parameter such as the solar constant, ice caps grow; moreover, the increased reflectivity (albedo) of the ice-covered surface causes an enhancement of the cooling. The effect of the ice-cap growth is to amplify the effects of an externally induced climate change. The ice-albedo mechanism is a positive feedback in the climate system. The climate system has many feedbacks, positive and negative. They play various roles in forced climate change. This lecture will concentrate on the effects of that one isolated feedback, since in this simplified form the problem becomes tractable and quasi-analytical solutions can be found. The ice-albedo feedback mechanism is a nonlinear phenomenon which leads to multiple solutions to the governing equations for fixed, prescribed values of the control parameters and bound |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Gerald R. North Kwang-yul Kim Wan-ho Lee |
spellingShingle |
Gerald R. North Kwang-yul Kim Wan-ho Lee Small Ice Caps in Climate Models |
author_facet |
Gerald R. North Kwang-yul Kim Wan-ho Lee |
author_sort |
Gerald R. North |
title |
Small Ice Caps in Climate Models |
title_short |
Small Ice Caps in Climate Models |
title_full |
Small Ice Caps in Climate Models |
title_fullStr |
Small Ice Caps in Climate Models |
title_full_unstemmed |
Small Ice Caps in Climate Models |
title_sort |
small ice caps in climate models |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.40.7978 http://chammp.met.fsu.edu/paper/ice_caps.ps |
genre |
Ice cap |
genre_facet |
Ice cap |
op_source |
http://chammp.met.fsu.edu/paper/ice_caps.ps |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.40.7978 http://chammp.met.fsu.edu/paper/ice_caps.ps |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766028497407442944 |