Recent variations in surface mass balance of the Antarctic Peninsula ice sheet

Over the period 1972-98 the height of the snow surface at eight Antarctic sites in Palmer Land and on Alexander Island has been measured with respect to fixed points on local nunataks. From these data an empirical relation between height changes over a given period and three key variables has been d...

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Published in:Journal of Glaciology
Main Authors: Morris, Elizabeth M., Mulvaney, Robert
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2004
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/12306/
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spelling ftnerc:oai:nora.nerc.ac.uk:12306 2023-05-15T13:15:19+02:00 Recent variations in surface mass balance of the Antarctic Peninsula ice sheet Morris, Elizabeth M. Mulvaney, Robert 2004 http://nora.nerc.ac.uk/id/eprint/12306/ unknown International Glaciological Society Morris, Elizabeth M.; Mulvaney, Robert orcid:0000-0002-5372-8148 . 2004 Recent variations in surface mass balance of the Antarctic Peninsula ice sheet. Journal of Glaciology, 50 (169). 257-267. https://doi.org/10.3189/172756504781830051 <https://doi.org/10.3189/172756504781830051> Meteorology and Climatology Glaciology Publication - Article PeerReviewed 2004 ftnerc https://doi.org/10.3189/172756504781830051 2023-02-04T19:27:55Z Over the period 1972-98 the height of the snow surface at eight Antarctic sites in Palmer Land and on Alexander Island has been measured with respect to fixed points on local nunataks. From these data an empirical relation between height changes over a given period and three key variables has been derived. These variables are (i) the local mean annual surface air temperature, (ii) a regional estimate of energy available for melt over the period (derived from the nearby Rothera air-temperature record) and (iii) a regional estimate of accumulation over the period (derived from the nearby Gomez Nunatak ice-core accumulation record). Using this relation, the contribution of the Antarctic Peninsula to sea-level rise for warming from climatic conditions (averaged over the last 30 years) is estimated to be -0.006 +/- 0.002 mm a(-1) K-1. If recent warm conditions persist, however, and meltwater can run off to the sea, the contribution to sea-level rise from ablation is calculated to be 0.07 +/- 0.02 mm a(-1) K-1. Article in Journal/Newspaper Alexander Island Antarc* Antarctic Antarctic Peninsula ice core Ice Sheet Journal of Glaciology Palmer Land Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Rothera ENVELOPE(-68.130,-68.130,-67.568,-67.568) Alexander Island ENVELOPE(-69.895,-69.895,-71.287,-71.287) Gomez ENVELOPE(-58.795,-58.795,-62.196,-62.196) Palmer Land ENVELOPE(-65.000,-65.000,-71.500,-71.500) Gomez Nunatak ENVELOPE(-68.632,-68.632,-73.934,-73.934) Journal of Glaciology 50 169 257 267
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Meteorology and Climatology
Glaciology
spellingShingle Meteorology and Climatology
Glaciology
Morris, Elizabeth M.
Mulvaney, Robert
Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
topic_facet Meteorology and Climatology
Glaciology
description Over the period 1972-98 the height of the snow surface at eight Antarctic sites in Palmer Land and on Alexander Island has been measured with respect to fixed points on local nunataks. From these data an empirical relation between height changes over a given period and three key variables has been derived. These variables are (i) the local mean annual surface air temperature, (ii) a regional estimate of energy available for melt over the period (derived from the nearby Rothera air-temperature record) and (iii) a regional estimate of accumulation over the period (derived from the nearby Gomez Nunatak ice-core accumulation record). Using this relation, the contribution of the Antarctic Peninsula to sea-level rise for warming from climatic conditions (averaged over the last 30 years) is estimated to be -0.006 +/- 0.002 mm a(-1) K-1. If recent warm conditions persist, however, and meltwater can run off to the sea, the contribution to sea-level rise from ablation is calculated to be 0.07 +/- 0.02 mm a(-1) K-1.
format Article in Journal/Newspaper
author Morris, Elizabeth M.
Mulvaney, Robert
author_facet Morris, Elizabeth M.
Mulvaney, Robert
author_sort Morris, Elizabeth M.
title Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
title_short Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
title_full Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
title_fullStr Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
title_full_unstemmed Recent variations in surface mass balance of the Antarctic Peninsula ice sheet
title_sort recent variations in surface mass balance of the antarctic peninsula ice sheet
publisher International Glaciological Society
publishDate 2004
url http://nora.nerc.ac.uk/id/eprint/12306/
long_lat ENVELOPE(-68.130,-68.130,-67.568,-67.568)
ENVELOPE(-69.895,-69.895,-71.287,-71.287)
ENVELOPE(-58.795,-58.795,-62.196,-62.196)
ENVELOPE(-65.000,-65.000,-71.500,-71.500)
ENVELOPE(-68.632,-68.632,-73.934,-73.934)
geographic Antarctic
The Antarctic
Antarctic Peninsula
Rothera
Alexander Island
Gomez
Palmer Land
Gomez Nunatak
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Rothera
Alexander Island
Gomez
Palmer Land
Gomez Nunatak
genre Alexander Island
Antarc*
Antarctic
Antarctic Peninsula
ice core
Ice Sheet
Journal of Glaciology
Palmer Land
genre_facet Alexander Island
Antarc*
Antarctic
Antarctic Peninsula
ice core
Ice Sheet
Journal of Glaciology
Palmer Land
op_relation Morris, Elizabeth M.; Mulvaney, Robert orcid:0000-0002-5372-8148 . 2004 Recent variations in surface mass balance of the Antarctic Peninsula ice sheet. Journal of Glaciology, 50 (169). 257-267. https://doi.org/10.3189/172756504781830051 <https://doi.org/10.3189/172756504781830051>
op_doi https://doi.org/10.3189/172756504781830051
container_title Journal of Glaciology
container_volume 50
container_issue 169
container_start_page 257
op_container_end_page 267
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