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Climate of the Past An interactive open-access journal of the European Geosciences Union
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https://doi.org/10.5194/cp-2020-141
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-2020-141
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

  17 Nov 2020

17 Nov 2020

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This preprint is currently under review for the journal CP.

Holocene climatic changes in the Westerly-Indian Monsoon realm and its anthropogenic impact

Nicole Burdanowitz1, Tim Rixen1,2, Birgit Gaye1, and Kay-Christian Emeis1,3 Nicole Burdanowitz et al.
  • 1Institute for Geology, Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany
  • 2Leibniz-Zentrum für Marine Tropenforschung (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
  • 3Institute of Coastal Research, Helmholtz Center Geesthacht, Max-Planck-Straße 1, 21502 Geesthacht, Germany

Abstract. The Indian Summer Monsoon (ISM) with its rainfall is the lifeline for people living on the Indian subcontinent today and possibly was the driver of the rise and fall of early agricultural societies in the past. Intensity and position of the ISM have shifted in response to orbitally forced thermal land-ocean contrasts. At the northwestern monsoon margins, interactions between the subtropical westerly jet (STWJ) and the ISM constitute a tipping element in the Earth's climate system, because their non-linear interaction may be a first-order influence on rainfall. We reconstructed marine sea surface temperature (SST), supply of terrestrial material and vegetation changes from a very well-dated sediment core from the northern Arabian Sea to reconstruct the STWJ-ISM interaction. The Holocene record (from 11,000 years) shows a distinct, but gradual, southward displacement of the ISM in the Early to Mid-Holocene, increasingly punctuated by phases of intensified STWJ events that are coeval with interruptions of North Atlantic overturning circulation (Bond events). Effects of the non-linear interactions culminate between 4.6–3 ka BP, marking a climatic transition period during which the ISM shifted southwards and the influence of SWTJ became prominent. The lithogenic input shows an up to 4-fold increase after this time period signaling the strengthened influence of agricultural activities of the Indus civilization with enhanced erosion of soils amplifying the impact of Bond events and adding to the marine sedimentation rates adjacent to the continent.

Nicole Burdanowitz et al.

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Nicole Burdanowitz et al.

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Grain sizes and geochemistry of Holocene sediments in the Arabian Sea. Burdanowitz, Nicole, Gaye, Birgit, Hilbig, Lea, Lahajnar, Niko, Lückge, Andreas, Rixen, Tim, and Emeis, Kay-Christian https://doi.org/10.1594/PANGAEA.900973

Nicole Burdanowitz et al.

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Short summary
To understand the interaction of the Westerlies and Indian Summer Monsoon (ISM) during the Holocene, we used paleoenvironmental reconstructions by using a sediment core from the NE Arabian Sea. We found a climatic transition period between 4.6–3 ka BP during which the ISM shifted southwards and the influence of Westerlies became prominent. Our data indicate a stronger influence of agriculture activities and enhanced soil erosion adding to the impact of Bond events after this transition period.
To understand the interaction of the Westerlies and Indian Summer Monsoon (ISM) during the...
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