Secular Trends of Accumulation Rates at Three Greenland Stations
Abstract The annual layer thickness profiles along three 400 m ice cores are transferred into accumulation-rate records. A linear decrease of 3±2% per millenium is found in mid-Greenland. Intermediate-term (periods longer than 120 years) deviations from the linear trend lines are less than 5% in mid...
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Language: | English |
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Cambridge University Press (CUP)
1978
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Online Access: | http://dx.doi.org/10.1017/s0022143000021195 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021195 |
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crcambridgeupr:10.1017/s0022143000021195 2024-03-03T08:43:56+00:00 Secular Trends of Accumulation Rates at Three Greenland Stations Reeh, N. Clausen, H.B. Dansgaard, W. Gundestrup, N. Hammer, C.U. Johnsen, S.J. 1978 http://dx.doi.org/10.1017/s0022143000021195 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021195 en eng Cambridge University Press (CUP) Journal of Glaciology volume 20, issue 82, page 27-30 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000021195 2024-02-08T08:39:08Z Abstract The annual layer thickness profiles along three 400 m ice cores are transferred into accumulation-rate records. A linear decrease of 3±2% per millenium is found in mid-Greenland. Intermediate-term (periods longer than 120 years) deviations from the linear trend lines are less than 5% in mid-Greenland but reach 11% at Dye 3 around A.D. 1700 and 1400. Short-term (periods between 120 and 30 years) oscillations are generally in phase at Milcent and Crête. Article in Journal/Newspaper Dye 3 Dye-3 Greenland Journal of Glaciology Cambridge University Press Greenland Journal of Glaciology 20 82 27 30 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Reeh, N. Clausen, H.B. Dansgaard, W. Gundestrup, N. Hammer, C.U. Johnsen, S.J. Secular Trends of Accumulation Rates at Three Greenland Stations |
topic_facet |
Earth-Surface Processes |
description |
Abstract The annual layer thickness profiles along three 400 m ice cores are transferred into accumulation-rate records. A linear decrease of 3±2% per millenium is found in mid-Greenland. Intermediate-term (periods longer than 120 years) deviations from the linear trend lines are less than 5% in mid-Greenland but reach 11% at Dye 3 around A.D. 1700 and 1400. Short-term (periods between 120 and 30 years) oscillations are generally in phase at Milcent and Crête. |
format |
Article in Journal/Newspaper |
author |
Reeh, N. Clausen, H.B. Dansgaard, W. Gundestrup, N. Hammer, C.U. Johnsen, S.J. |
author_facet |
Reeh, N. Clausen, H.B. Dansgaard, W. Gundestrup, N. Hammer, C.U. Johnsen, S.J. |
author_sort |
Reeh, N. |
title |
Secular Trends of Accumulation Rates at Three Greenland Stations |
title_short |
Secular Trends of Accumulation Rates at Three Greenland Stations |
title_full |
Secular Trends of Accumulation Rates at Three Greenland Stations |
title_fullStr |
Secular Trends of Accumulation Rates at Three Greenland Stations |
title_full_unstemmed |
Secular Trends of Accumulation Rates at Three Greenland Stations |
title_sort |
secular trends of accumulation rates at three greenland stations |
publisher |
Cambridge University Press (CUP) |
publishDate |
1978 |
url |
http://dx.doi.org/10.1017/s0022143000021195 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021195 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Dye 3 Dye-3 Greenland Journal of Glaciology |
genre_facet |
Dye 3 Dye-3 Greenland Journal of Glaciology |
op_source |
Journal of Glaciology volume 20, issue 82, page 27-30 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021195 |
container_title |
Journal of Glaciology |
container_volume |
20 |
container_issue |
82 |
container_start_page |
27 |
op_container_end_page |
30 |
_version_ |
1792499403212193792 |