The Diurnal Hysteresis of Snow Albedo
Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two...
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Language: | English |
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Cambridge University Press (CUP)
1985
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Online Access: | http://dx.doi.org/10.1017/s0022143000006456 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456 |
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crcambridgeupr:10.1017/s0022143000006456 2024-09-09T19:09:58+00:00 The Diurnal Hysteresis of Snow Albedo Mcguffie, K. Henderson-Sellers, A. 1985 http://dx.doi.org/10.1017/s0022143000006456 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456 en eng Cambridge University Press (CUP) Journal of Glaciology volume 31, issue 108, page 188-189 ISSN 0022-1430 1727-5652 journal-article 1985 crcambridgeupr https://doi.org/10.1017/s0022143000006456 2024-08-21T04:04:46Z Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two in the region of the marginal cryosphere. Surface irregularities probably are the dominant influence only on permanent cryospheric areas such as the Greenland and Antarctic plateaux. Article in Journal/Newspaper Antarc* Antarctic Greenland Journal of Glaciology Cambridge University Press Antarctic Greenland Sastrugi ENVELOPE(163.683,163.683,-74.617,-74.617) Journal of Glaciology 31 108 188 189 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two in the region of the marginal cryosphere. Surface irregularities probably are the dominant influence only on permanent cryospheric areas such as the Greenland and Antarctic plateaux. |
format |
Article in Journal/Newspaper |
author |
Mcguffie, K. Henderson-Sellers, A. |
spellingShingle |
Mcguffie, K. Henderson-Sellers, A. The Diurnal Hysteresis of Snow Albedo |
author_facet |
Mcguffie, K. Henderson-Sellers, A. |
author_sort |
Mcguffie, K. |
title |
The Diurnal Hysteresis of Snow Albedo |
title_short |
The Diurnal Hysteresis of Snow Albedo |
title_full |
The Diurnal Hysteresis of Snow Albedo |
title_fullStr |
The Diurnal Hysteresis of Snow Albedo |
title_full_unstemmed |
The Diurnal Hysteresis of Snow Albedo |
title_sort |
diurnal hysteresis of snow albedo |
publisher |
Cambridge University Press (CUP) |
publishDate |
1985 |
url |
http://dx.doi.org/10.1017/s0022143000006456 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456 |
long_lat |
ENVELOPE(163.683,163.683,-74.617,-74.617) |
geographic |
Antarctic Greenland Sastrugi |
geographic_facet |
Antarctic Greenland Sastrugi |
genre |
Antarc* Antarctic Greenland Journal of Glaciology |
genre_facet |
Antarc* Antarctic Greenland Journal of Glaciology |
op_source |
Journal of Glaciology volume 31, issue 108, page 188-189 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000006456 |
container_title |
Journal of Glaciology |
container_volume |
31 |
container_issue |
108 |
container_start_page |
188 |
op_container_end_page |
189 |
_version_ |
1809824282127106048 |