Articles | Volume 13, issue 5
https://doi.org/10.5194/cp-13-491-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-491-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 May 2017
Research article |
| 19 May 2017
Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9–6 ka)
Philipp M. Munz
CORRESPONDING AUTHOR
Senckenberg Centre for Human Evolution and Palaeoenvironment (HEP) at the University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
Department of Geosciences, University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
Stephan Steinke
Department of Geological Oceanography, Xiamen University, Xiping Building, Xiang'an South Road, Xiamen 361102, China
Anna Böll
Institute of Geology, University of Hamburg, Bundesstr. 55, 20146 Hamburg, Germany
Andreas Lückge
Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Stilleweg 2, 30655 Hannover, Germany
Jeroen Groeneveld
MARUM – Center for Marine Environmental Sciences, Germany, Leobener Str., 28359 Bremen, Germany
Michal Kucera
MARUM – Center for Marine Environmental Sciences, Germany, Leobener Str., 28359 Bremen, Germany
Hartmut Schulz
Department of Geosciences, University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
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16 citations as recorded by crossref.
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- Distinct oxygenation modes of the Gulf of Oman over the past 43 000 years – a multi-proxy approach N. Burdanowitz et al. 10.5194/bg-21-1477-2024
- Impact of solar variability on Indian summer monsoon through large scale circulations V. Barde et al. 10.1016/j.jastp.2023.106134
- Coupled Ocean-atmospheric forcing on Indian Summer Monsoon variability during the middle Holocene: Insights from the Core Monsoon Zone speleothem record P. Gupta et al. 10.1016/j.palaeo.2024.112273
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- Monsoons, Upwelling, and the Deoxygenation of the Northwestern Indian Ocean in Response to Middle to Late Miocene Global Climatic Shifts O. Bialik et al. 10.1029/2019PA003762
- Supernova Rates and Burial of Organic Matter H. Svensmark 10.1029/2021GL096376
- A ∼ 50 kyr record of carbonate (pteropods) preservation from the Laccadive Sea, Northern Indian Ocean E. Sreevidya et al. 10.1016/j.margeo.2022.106958
- Potential forcings of summer temperature variability of the southeastern Tibetan Plateau in the past 12 ka E. Zhang et al. 10.1016/j.jseaes.2018.03.023
- Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone G. Auer et al. 10.5194/cp-19-2313-2023
- Changes in the Indian Summer Monsoon during the past 600 years: A high-resolution record from the Anshupa Lake, Upper Mahanadi Delta, Core Monsoon Zone of India C. Dash et al. 10.1016/j.jseaes.2021.105048
- Detection of a mid-Holocene climate event at 7.2 ka BP based on an analysis of globally-distributed multi-proxy records M. Hou et al. 10.1016/j.palaeo.2023.111525
- Investigating the Upper Holocene palaeoenvironment and human subsistence strategy in the Khor Rori coastal area by studying mollusc remains from the Inqitat plateau (Dhofar, Sultanate of Oman) G. Crippa et al. 10.1002/jqs.3610
2 citations as recorded by crossref.
Latest update: 20 Nov 2024
Short summary
We present the results of several independent proxies of summer SST and upwelling SST from the Oman margin indicative of monsoon strength during the early Holocene. In combination with indices of carbonate preservation and bottom water redox conditions, we demonstrate that a persistent solar influence was modulating summer monsoon intensity. Furthermore, bottom water conditions are linked to atmospheric forcing, rather than changes of intermediate water masses.
We present the results of several independent proxies of summer SST and upwelling SST from the...
