Pollen analyses of sediment core GeoB9508-5
Millennial-scale dry events in the Northern Hemisphere monsoon regions during the last Glacial period are commonly attributed to southward shifts of the Intertropical Convergence Zone (ITCZ) associated with an intensification of the northeasterly (NE) trade wind system during intervals of reduced At...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.801827 2023-05-15T17:36:39+02:00 Pollen analyses of sediment core GeoB9508-5 Bouimetarhan, Ilham Prange, Matthias Schefuß, Enno Dupont, Lydie M Lippold, Jörg Mulitza, Stefan Zonneveld, Karin A F LATITUDE: 15.498333 * LONGITUDE: -17.948000 * DATE/TIME START: 2005-06-15T13:51:00 * DATE/TIME END: 2005-06-15T13:51:00 2012-11-14 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.801827 https://doi.org/10.1594/PANGAEA.801827 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.801827 https://doi.org/10.1594/PANGAEA.801827 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Bouimetarhan, Ilham; Prange, Matthias; Schefuß, Enno; Dupont, Lydie M; Lippold, Jörg; Mulitza, Stefan; Zonneveld, Karin A F (2012): Sahel megadrought during Heinrich Stadial 1: evidence for a three-phase evolution of the low- and mid-level West African wind system. Quaternary Science Reviews, 58, 66-76, https://doi.org/10.1016/j.quascirev.2012.10.015 293 Center for Marine Environmental Sciences GeoB9508-5 Gravity corer (Kiel type) M65/1 MARUM Meteor (1986) SL Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.801827 https://doi.org/10.1016/j.quascirev.2012.10.015 2023-01-20T07:32:47Z Millennial-scale dry events in the Northern Hemisphere monsoon regions during the last Glacial period are commonly attributed to southward shifts of the Intertropical Convergence Zone (ITCZ) associated with an intensification of the northeasterly (NE) trade wind system during intervals of reduced Atlantic meridional overturning circulation (AMOC). Through the use of high-resolution last deglaciation pollen records from the continental slope off Senegal, our data show that one of the longest and most extreme droughts in the western Sahel history, which occurred during the North Atlantic Heinrich Stadial 1 (HS1), displayed a succession of three major phases. These phases progressed from an interval of maximum pollen representation of Saharan elements between ~19 and 17.4 kyr BP indicating the onset of aridity and intensified NE trade winds, followed by a millennial interlude of reduced input of Saharan pollen and increased input of Sahelian pollen, to a final phase between ~16.2 and 15 kyr BP that was characterized by a second maximum of Saharan pollen abundances. This change in the pollen assemblage indicates a mid-HS1 interlude of NE trade wind relaxation, occurring between two distinct trade wind maxima, along with an intensified mid-tropospheric African Easterly Jet (AEJ) indicating a substantial change in West African atmospheric processes. The pollen data thus suggest that although the NE trades have weakened, the Sahel drought remained severe during this time interval. Therefore, a simple strengthening of trade winds and a southward shift of the West African monsoon trough alone cannot fully explain millennial-scale Sahel droughts during periods of AMOC weakening. Instead, we suggest that an intensification of the AEJ is needed to explain the persistence of the drought during HS1. Simulations with the Community Climate System Model indicate that an intensified AEJ during periods of reduced AMOC affected the North African climate by enhancing moisture divergence over the West African realm, thereby extending ... Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-17.948000,-17.948000,15.498333,15.498333) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
293 Center for Marine Environmental Sciences GeoB9508-5 Gravity corer (Kiel type) M65/1 MARUM Meteor (1986) SL |
spellingShingle |
293 Center for Marine Environmental Sciences GeoB9508-5 Gravity corer (Kiel type) M65/1 MARUM Meteor (1986) SL Bouimetarhan, Ilham Prange, Matthias Schefuß, Enno Dupont, Lydie M Lippold, Jörg Mulitza, Stefan Zonneveld, Karin A F Pollen analyses of sediment core GeoB9508-5 |
topic_facet |
293 Center for Marine Environmental Sciences GeoB9508-5 Gravity corer (Kiel type) M65/1 MARUM Meteor (1986) SL |
description |
Millennial-scale dry events in the Northern Hemisphere monsoon regions during the last Glacial period are commonly attributed to southward shifts of the Intertropical Convergence Zone (ITCZ) associated with an intensification of the northeasterly (NE) trade wind system during intervals of reduced Atlantic meridional overturning circulation (AMOC). Through the use of high-resolution last deglaciation pollen records from the continental slope off Senegal, our data show that one of the longest and most extreme droughts in the western Sahel history, which occurred during the North Atlantic Heinrich Stadial 1 (HS1), displayed a succession of three major phases. These phases progressed from an interval of maximum pollen representation of Saharan elements between ~19 and 17.4 kyr BP indicating the onset of aridity and intensified NE trade winds, followed by a millennial interlude of reduced input of Saharan pollen and increased input of Sahelian pollen, to a final phase between ~16.2 and 15 kyr BP that was characterized by a second maximum of Saharan pollen abundances. This change in the pollen assemblage indicates a mid-HS1 interlude of NE trade wind relaxation, occurring between two distinct trade wind maxima, along with an intensified mid-tropospheric African Easterly Jet (AEJ) indicating a substantial change in West African atmospheric processes. The pollen data thus suggest that although the NE trades have weakened, the Sahel drought remained severe during this time interval. Therefore, a simple strengthening of trade winds and a southward shift of the West African monsoon trough alone cannot fully explain millennial-scale Sahel droughts during periods of AMOC weakening. Instead, we suggest that an intensification of the AEJ is needed to explain the persistence of the drought during HS1. Simulations with the Community Climate System Model indicate that an intensified AEJ during periods of reduced AMOC affected the North African climate by enhancing moisture divergence over the West African realm, thereby extending ... |
format |
Dataset |
author |
Bouimetarhan, Ilham Prange, Matthias Schefuß, Enno Dupont, Lydie M Lippold, Jörg Mulitza, Stefan Zonneveld, Karin A F |
author_facet |
Bouimetarhan, Ilham Prange, Matthias Schefuß, Enno Dupont, Lydie M Lippold, Jörg Mulitza, Stefan Zonneveld, Karin A F |
author_sort |
Bouimetarhan, Ilham |
title |
Pollen analyses of sediment core GeoB9508-5 |
title_short |
Pollen analyses of sediment core GeoB9508-5 |
title_full |
Pollen analyses of sediment core GeoB9508-5 |
title_fullStr |
Pollen analyses of sediment core GeoB9508-5 |
title_full_unstemmed |
Pollen analyses of sediment core GeoB9508-5 |
title_sort |
pollen analyses of sediment core geob9508-5 |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.801827 https://doi.org/10.1594/PANGAEA.801827 |
op_coverage |
LATITUDE: 15.498333 * LONGITUDE: -17.948000 * DATE/TIME START: 2005-06-15T13:51:00 * DATE/TIME END: 2005-06-15T13:51:00 |
long_lat |
ENVELOPE(-17.948000,-17.948000,15.498333,15.498333) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Bouimetarhan, Ilham; Prange, Matthias; Schefuß, Enno; Dupont, Lydie M; Lippold, Jörg; Mulitza, Stefan; Zonneveld, Karin A F (2012): Sahel megadrought during Heinrich Stadial 1: evidence for a three-phase evolution of the low- and mid-level West African wind system. Quaternary Science Reviews, 58, 66-76, https://doi.org/10.1016/j.quascirev.2012.10.015 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.801827 https://doi.org/10.1594/PANGAEA.801827 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.801827 https://doi.org/10.1016/j.quascirev.2012.10.015 |
_version_ |
1766136217063129088 |