The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP

A high resolution continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany). This Maar is suitable to archive easterly wind directions due to its location west of the Devonia...

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Published in:Climate of the Past
Main Authors: K. Seelos, S. Dietrich
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
Online Access:https://doi.org/10.5194/cp-6-145-2010
https://doaj.org/article/c175dc8230d94647b1f0c1473c42bf21
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spelling ftdoajarticles:oai:doaj.org/article:c175dc8230d94647b1f0c1473c42bf21 2023-05-15T16:30:05+02:00 The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP K. Seelos S. Dietrich 2010-03-01T00:00:00Z https://doi.org/10.5194/cp-6-145-2010 https://doaj.org/article/c175dc8230d94647b1f0c1473c42bf21 EN eng Copernicus Publications http://www.clim-past.net/6/145/2010/cp-6-145-2010.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-6-145-2010 1814-9324 1814-9332 https://doaj.org/article/c175dc8230d94647b1f0c1473c42bf21 Climate of the Past, Vol 6, Iss 2, Pp 145-154 (2010) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2010 ftdoajarticles https://doi.org/10.5194/cp-6-145-2010 2022-12-31T09:13:40Z A high resolution continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany). This Maar is suitable to archive easterly wind directions due to its location west of the Devonian carbonate basins of the Eifel-North-South-Zone. Thus, eolian sediments with high clastic carbonate content can be interpreted as an east wind signal. The detection of such east wind sediments is applied by a new module of the RADIUS grain size analyze technique. The investigated time period from 40.3–12.9 ka BP can be subclassified in three units: The first unit covers the periods of the ending GIS-9, H4, and GIS-8. With the exception of H4 (40–38 ka BP) the content of organics in our record is relatively high. With the end of GIS-8 (38–36.5 ka) the content of organics decrease and the content of dust increases rapidly. The second time slice (36–24 ka BP) has an increased content of dust accumulation and a high amount of east winds layers (up to 19% of the dust storms per century came from the east). In comparison, the subsequent period (24–12.9 ka BP) is characterized by lower east wind sediments again. Increased frequencies of east wind occur during the time intervals corresponding with the Heinrich events H1 and H2. The unusual H3 show no higher east wind frequency but so do its former and subsequent Greenland stadials. The late LGM (21–18 ka BP) is characterized by a slightly elevated east wind frequency again. Article in Journal/Newspaper Greenland Directory of Open Access Journals: DOAJ Articles Greenland Climate of the Past 6 2 145 154
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
spellingShingle Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
K. Seelos
S. Dietrich
The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
topic_facet Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
description A high resolution continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany). This Maar is suitable to archive easterly wind directions due to its location west of the Devonian carbonate basins of the Eifel-North-South-Zone. Thus, eolian sediments with high clastic carbonate content can be interpreted as an east wind signal. The detection of such east wind sediments is applied by a new module of the RADIUS grain size analyze technique. The investigated time period from 40.3–12.9 ka BP can be subclassified in three units: The first unit covers the periods of the ending GIS-9, H4, and GIS-8. With the exception of H4 (40–38 ka BP) the content of organics in our record is relatively high. With the end of GIS-8 (38–36.5 ka) the content of organics decrease and the content of dust increases rapidly. The second time slice (36–24 ka BP) has an increased content of dust accumulation and a high amount of east winds layers (up to 19% of the dust storms per century came from the east). In comparison, the subsequent period (24–12.9 ka BP) is characterized by lower east wind sediments again. Increased frequencies of east wind occur during the time intervals corresponding with the Heinrich events H1 and H2. The unusual H3 show no higher east wind frequency but so do its former and subsequent Greenland stadials. The late LGM (21–18 ka BP) is characterized by a slightly elevated east wind frequency again.
format Article in Journal/Newspaper
author K. Seelos
S. Dietrich
author_facet K. Seelos
S. Dietrich
author_sort K. Seelos
title The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
title_short The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
title_full The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
title_fullStr The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
title_full_unstemmed The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP
title_sort reconstruction of easterly wind directions for the eifel region (central europe) during the period 40.3–12.9 ka bp
publisher Copernicus Publications
publishDate 2010
url https://doi.org/10.5194/cp-6-145-2010
https://doaj.org/article/c175dc8230d94647b1f0c1473c42bf21
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Climate of the Past, Vol 6, Iss 2, Pp 145-154 (2010)
op_relation http://www.clim-past.net/6/145/2010/cp-6-145-2010.pdf
https://doaj.org/toc/1814-9324
https://doaj.org/toc/1814-9332
doi:10.5194/cp-6-145-2010
1814-9324
1814-9332
https://doaj.org/article/c175dc8230d94647b1f0c1473c42bf21
op_doi https://doi.org/10.5194/cp-6-145-2010
container_title Climate of the Past
container_volume 6
container_issue 2
container_start_page 145
op_container_end_page 154
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