Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791
Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asi...
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ftdatacite:10.1594/pangaea.860017 2023-05-15T17:58:03+02:00 Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 Ramisch, Arne Lockot, Gregori Haberzettl, Torsten Hartmann, Kai Kuhn, Gerhard Lehmkuhl, Frank Schimpf, Stefan Schulte, Philipp Stauch, Georg Wang, Rong Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Diekmann, Bernhard 2016 application/zip https://dx.doi.org/10.1594/pangaea.860017 https://doi.pangaea.de/10.1594/PANGAEA.860017 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1038/srep25791 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Collection article Supplementary Collection of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.860017 https://doi.org/10.1038/srep25791 2021-11-05T12:55:41Z Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asia. Paleoclimatic evidence, however, suggests increased moisture availability in the Early Holocene north of the Himalayan range which is attributed to an intensification of the Indian Summer Monsoon. Nevertheless, mechanisms leading to a surpassing of the Himalayan range and the northern maximum extent of summer monsoonal influence remain unknown. Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer Monsoon which is persistent throughout the Holocene. Precipitation intensities at its northern extent seem to be driven by differentiated solar heating of the Northern Hemisphere indicating dependency on energy-gradients rather than absolute radiation intensities. The identified spatial constraints of monsoonal precipitation will facilitate the prediction of future monsoonal precipitation patterns in Central Asia under varying climatic conditions. Article in Journal/Newspaper permafrost DataCite Metadata Store (German National Library of Science and Technology) Indian |
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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 |
English |
topic |
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
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Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Ramisch, Arne Lockot, Gregori Haberzettl, Torsten Hartmann, Kai Kuhn, Gerhard Lehmkuhl, Frank Schimpf, Stefan Schulte, Philipp Stauch, Georg Wang, Rong Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Diekmann, Bernhard Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
topic_facet |
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
description |
Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asia. Paleoclimatic evidence, however, suggests increased moisture availability in the Early Holocene north of the Himalayan range which is attributed to an intensification of the Indian Summer Monsoon. Nevertheless, mechanisms leading to a surpassing of the Himalayan range and the northern maximum extent of summer monsoonal influence remain unknown. Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer Monsoon which is persistent throughout the Holocene. Precipitation intensities at its northern extent seem to be driven by differentiated solar heating of the Northern Hemisphere indicating dependency on energy-gradients rather than absolute radiation intensities. The identified spatial constraints of monsoonal precipitation will facilitate the prediction of future monsoonal precipitation patterns in Central Asia under varying climatic conditions. |
format |
Article in Journal/Newspaper |
author |
Ramisch, Arne Lockot, Gregori Haberzettl, Torsten Hartmann, Kai Kuhn, Gerhard Lehmkuhl, Frank Schimpf, Stefan Schulte, Philipp Stauch, Georg Wang, Rong Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Diekmann, Bernhard |
author_facet |
Ramisch, Arne Lockot, Gregori Haberzettl, Torsten Hartmann, Kai Kuhn, Gerhard Lehmkuhl, Frank Schimpf, Stefan Schulte, Philipp Stauch, Georg Wang, Rong Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Diekmann, Bernhard |
author_sort |
Ramisch, Arne |
title |
Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
title_short |
Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
title_full |
Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
title_fullStr |
Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
title_full_unstemmed |
Bulk mineralogy and membership degrees of sediments from the Heihai lake area, supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791 |
title_sort |
bulk mineralogy and membership degrees of sediments from the heihai lake area, supplement to: ramisch, arne; lockot, gregori; haberzettl, torsten; hartmann, kai; kuhn, gerhard; lehmkuhl, frank; schimpf, stefan; schulte, philipp; stauch, georg; wang, rong; wünnemann, bernd; yan, dada; zhang, yongzhan; diekmann, bernhard (2016): a persistent northern boundary of indian summer monsoon precipitation over central asia during the holocene. scientific reports, 6, 25791 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.860017 https://doi.pangaea.de/10.1594/PANGAEA.860017 |
geographic |
Indian |
geographic_facet |
Indian |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
https://dx.doi.org/10.1038/srep25791 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.860017 https://doi.org/10.1038/srep25791 |
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1766166588102279168 |