Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling
ABSTR ACT. Ice a b la tion is rel a ted to a ir temperature b y the positive d egree-day factor. V a ri a tions of th e positi ve degree-d ay fac tor in \Ves t Greenland a re st ud ied using a n energy-ba la n ce m odel to simulate ablation under differen t condi tions. Degree-d ay factors for simul...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.634.5942 2023-05-15T16:28:27+02:00 Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling Roger J. Braithwaite The Pennsylvania State University CiteSeerX Archives 1995 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.634.5942 http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.634.5942 http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf text 1995 ftciteseerx 2016-01-08T15:38:25Z ABSTR ACT. Ice a b la tion is rel a ted to a ir temperature b y the positive d egree-day factor. V a ri a tions of th e positi ve degree-d ay fac tor in \Ves t Greenland a re st ud ied using a n energy-ba la n ce m odel to simulate ablation under differen t condi tions. Degree-d ay factors for simula ted a nd m easured ice a bla tio n at;.Jordbogle tscher a nd Q amana rss up sermia agree well with valu es a round 8 mm d 1oC I. Degree-d ay factors for snow a re less tha n h a lf those for ice. Energy-bala nce m od ell ing shows th a t degree-day factors va ry with summer mean tempera ture, surface a lbedo and turbulence but there is only evidence of la rge positive d egree-day facto rs a t lower tempera tures and with low a lbedo (0. 3). Th e greates t effec t of albedo varia ti o ns (0.3- 0. 7) is a t lower tempera tures while vari a tio ns in turbulen ce have grea ter e ITeC! a t higher tempera tures. Current m odels may underes tima te rllnoff from the Green la nd ice shee t b y severa l tenths becallse they use a d egree-day facto r for melting ice tha t is too sm a ll fo r the cold er pa rts of the ice shee t, i.e. the upper a bla tion a rea a nd the northerly m a rgin. Text Greenland Ice Sheet Unknown Bala ENVELOPE(132.817,132.817,67.178,67.178) Greenland |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
ABSTR ACT. Ice a b la tion is rel a ted to a ir temperature b y the positive d egree-day factor. V a ri a tions of th e positi ve degree-d ay fac tor in \Ves t Greenland a re st ud ied using a n energy-ba la n ce m odel to simulate ablation under differen t condi tions. Degree-d ay factors for simula ted a nd m easured ice a bla tio n at;.Jordbogle tscher a nd Q amana rss up sermia agree well with valu es a round 8 mm d 1oC I. Degree-d ay factors for snow a re less tha n h a lf those for ice. Energy-bala nce m od ell ing shows th a t degree-day factors va ry with summer mean tempera ture, surface a lbedo and turbulence but there is only evidence of la rge positive d egree-day facto rs a t lower tempera tures and with low a lbedo (0. 3). Th e greates t effec t of albedo varia ti o ns (0.3- 0. 7) is a t lower tempera tures while vari a tio ns in turbulen ce have grea ter e ITeC! a t higher tempera tures. Current m odels may underes tima te rllnoff from the Green la nd ice shee t b y severa l tenths becallse they use a d egree-day facto r for melting ice tha t is too sm a ll fo r the cold er pa rts of the ice shee t, i.e. the upper a bla tion a rea a nd the northerly m a rgin. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Roger J. Braithwaite |
spellingShingle |
Roger J. Braithwaite Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
author_facet |
Roger J. Braithwaite |
author_sort |
Roger J. Braithwaite |
title |
Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
title_short |
Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
title_full |
Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
title_fullStr |
Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
title_full_unstemmed |
Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling |
title_sort |
positive degree-day factors for ablation on the greenland ice sheet studied by energy-balance modelling |
publishDate |
1995 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.634.5942 http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf |
long_lat |
ENVELOPE(132.817,132.817,67.178,67.178) |
geographic |
Bala Greenland |
geographic_facet |
Bala Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.634.5942 http://www.igsoc.org/journal/41/137/igs_journal_vol41_issue137_pg153-160.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766018106294009856 |