Long-term record of H2O2 in polar ice cores
At Dye 3 and Camp Century, Greenland, and at Byrd Station, West-Antarctica, ice cores were drilled to bedrock. They offer an archive of solid precipitation over the last 50.000 to 100,OOO years. H2O2 has been found to be one of the dominant trace components in the ice. We present a survey of the H2O...
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1986
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ftdatacite:10.48350/158747 2023-05-15T13:47:04+02:00 Long-term record of H2O2 in polar ice cores Neftel, A. Jacob, P. Klockow, D. 1986 https://dx.doi.org/10.48350/158747 https://boris.unibe.ch/158747/ unknown Munksgaard restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec 530 Physics Text article-journal journal article ScholarlyArticle 1986 ftdatacite https://doi.org/10.48350/158747 2021-11-05T12:55:41Z At Dye 3 and Camp Century, Greenland, and at Byrd Station, West-Antarctica, ice cores were drilled to bedrock. They offer an archive of solid precipitation over the last 50.000 to 100,OOO years. H2O2 has been found to be one of the dominant trace components in the ice. We present a survey of the H2O2 levels in the three deep cores. In the Greenland ice cores the H2O2 level decreases with increasing depth and is extremely low during the last glaciation. In the Byrd core an H2O2 concentration spike is observed in the time period 6000 to 12,000 years before present. Possible explanations for the decreasing trend with age and depth and the drop during the Ice Age are discussed. Text Antarc* Antarctica Dye 3 Dye-3 Greenland Greenland ice cores West Antarctica DataCite Metadata Store (German National Library of Science and Technology) West Antarctica Greenland Byrd Byrd Station ENVELOPE(-119.533,-119.533,-80.017,-80.017) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
530 Physics |
spellingShingle |
530 Physics Neftel, A. Jacob, P. Klockow, D. Long-term record of H2O2 in polar ice cores |
topic_facet |
530 Physics |
description |
At Dye 3 and Camp Century, Greenland, and at Byrd Station, West-Antarctica, ice cores were drilled to bedrock. They offer an archive of solid precipitation over the last 50.000 to 100,OOO years. H2O2 has been found to be one of the dominant trace components in the ice. We present a survey of the H2O2 levels in the three deep cores. In the Greenland ice cores the H2O2 level decreases with increasing depth and is extremely low during the last glaciation. In the Byrd core an H2O2 concentration spike is observed in the time period 6000 to 12,000 years before present. Possible explanations for the decreasing trend with age and depth and the drop during the Ice Age are discussed. |
format |
Text |
author |
Neftel, A. Jacob, P. Klockow, D. |
author_facet |
Neftel, A. Jacob, P. Klockow, D. |
author_sort |
Neftel, A. |
title |
Long-term record of H2O2 in polar ice cores |
title_short |
Long-term record of H2O2 in polar ice cores |
title_full |
Long-term record of H2O2 in polar ice cores |
title_fullStr |
Long-term record of H2O2 in polar ice cores |
title_full_unstemmed |
Long-term record of H2O2 in polar ice cores |
title_sort |
long-term record of h2o2 in polar ice cores |
publisher |
Munksgaard |
publishDate |
1986 |
url |
https://dx.doi.org/10.48350/158747 https://boris.unibe.ch/158747/ |
long_lat |
ENVELOPE(-119.533,-119.533,-80.017,-80.017) |
geographic |
West Antarctica Greenland Byrd Byrd Station |
geographic_facet |
West Antarctica Greenland Byrd Byrd Station |
genre |
Antarc* Antarctica Dye 3 Dye-3 Greenland Greenland ice cores West Antarctica |
genre_facet |
Antarc* Antarctica Dye 3 Dye-3 Greenland Greenland ice cores West Antarctica |
op_rights |
restricted access publisher holds copyright http://purl.org/coar/access_right/c_16ec |
op_doi |
https://doi.org/10.48350/158747 |
_version_ |
1766246265955287040 |