Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years
Statistical analysis of reanalysis and observed data reveals that high dust surface mass concentration in northern Greenland is associated with a Pacific Decadal Oscillation like pattern in its negative phase in the North Pacific as well as with La Niña conditions in the tropical Pacific region. The...
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American Geophysical Union (AGU)
2022
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ftawi:oai:epic.awi.de:58655 2024-05-19T07:40:56+00:00 Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years Rimbu, N Ionita, M Lohmann, G 2022-12-28 application/pdf https://epic.awi.de/id/eprint/58655/ https://epic.awi.de/id/eprint/58655/1/Rimbu2022.pdf https://doi.org/10.1029/2022gl101500 https://hdl.handle.net/10013/epic.bd67b4de-a980-44c6-be15-27a42f6afd54 unknown American Geophysical Union (AGU) https://epic.awi.de/id/eprint/58655/1/Rimbu2022.pdf Rimbu, N. orcid:0000-0003-2832-9396 , Ionita, M. orcid:0000-0001-8240-4380 and Lohmann, G. orcid:0000-0003-2089-733X (2022) Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years , Geophysical Research Letters, 49 (24) . doi:10.1029/2022gl101500 <https://doi.org/10.1029/2022gl101500> , hdl:10013/epic.bd67b4de-a980-44c6-be15-27a42f6afd54 EPIC3Geophysical Research Letters, American Geophysical Union (AGU), 49(24), ISSN: 0094-8276 Article isiRev 2022 ftawi https://doi.org/10.1029/2022gl101500 2024-04-23T23:38:07Z Statistical analysis of reanalysis and observed data reveals that high dust surface mass concentration in northern Greenland is associated with a Pacific Decadal Oscillation like pattern in its negative phase in the North Pacific as well as with La Niña conditions in the tropical Pacific region. The sea surface temperature anomalies in the Pacific realm resemble the Interdecadal Pacific Oscillation (IPO). The associated atmospheric circulation pattern, in the form of a wave-train from the North Pacific to the Eurasian continent, favors enhanced dust uptake and transport toward the northern Greenland. Similar patterns are associated with a low-resolution stacked record of five Ca2+ ice cores, that is, ngt03C93.2 (B16), ngt14C93.2 (B18), ngt27C94.2 (B21), GISP2−B, and NEEM-2011-S1, from northern Greenland, a proxy for regional dust concentration, during the last 400 years. We argue that northern Greenland ice core dust records could be used as proxies for the IPO and related teleconnections. Article in Journal/Newspaper Greenland Greenland ice core ice core Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Geophysical Research Letters 49 24 |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
Statistical analysis of reanalysis and observed data reveals that high dust surface mass concentration in northern Greenland is associated with a Pacific Decadal Oscillation like pattern in its negative phase in the North Pacific as well as with La Niña conditions in the tropical Pacific region. The sea surface temperature anomalies in the Pacific realm resemble the Interdecadal Pacific Oscillation (IPO). The associated atmospheric circulation pattern, in the form of a wave-train from the North Pacific to the Eurasian continent, favors enhanced dust uptake and transport toward the northern Greenland. Similar patterns are associated with a low-resolution stacked record of five Ca2+ ice cores, that is, ngt03C93.2 (B16), ngt14C93.2 (B18), ngt27C94.2 (B21), GISP2−B, and NEEM-2011-S1, from northern Greenland, a proxy for regional dust concentration, during the last 400 years. We argue that northern Greenland ice core dust records could be used as proxies for the IPO and related teleconnections. |
format |
Article in Journal/Newspaper |
author |
Rimbu, N Ionita, M Lohmann, G |
spellingShingle |
Rimbu, N Ionita, M Lohmann, G Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
author_facet |
Rimbu, N Ionita, M Lohmann, G |
author_sort |
Rimbu, N |
title |
Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
title_short |
Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
title_full |
Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
title_fullStr |
Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
title_full_unstemmed |
Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years |
title_sort |
interdecadal pacific oscillation in northern greenland dust concentration variability during the last 400 years |
publisher |
American Geophysical Union (AGU) |
publishDate |
2022 |
url |
https://epic.awi.de/id/eprint/58655/ https://epic.awi.de/id/eprint/58655/1/Rimbu2022.pdf https://doi.org/10.1029/2022gl101500 https://hdl.handle.net/10013/epic.bd67b4de-a980-44c6-be15-27a42f6afd54 |
genre |
Greenland Greenland ice core ice core |
genre_facet |
Greenland Greenland ice core ice core |
op_source |
EPIC3Geophysical Research Letters, American Geophysical Union (AGU), 49(24), ISSN: 0094-8276 |
op_relation |
https://epic.awi.de/id/eprint/58655/1/Rimbu2022.pdf Rimbu, N. orcid:0000-0003-2832-9396 , Ionita, M. orcid:0000-0001-8240-4380 and Lohmann, G. orcid:0000-0003-2089-733X (2022) Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years , Geophysical Research Letters, 49 (24) . doi:10.1029/2022gl101500 <https://doi.org/10.1029/2022gl101500> , hdl:10013/epic.bd67b4de-a980-44c6-be15-27a42f6afd54 |
op_doi |
https://doi.org/10.1029/2022gl101500 |
container_title |
Geophysical Research Letters |
container_volume |
49 |
container_issue |
24 |
_version_ |
1799480496700260352 |