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Forcing mechanisms of orbital-scale changes in winter rainfall over northwestern China during the Holocene.
Zhang, X., Jin, Liya, Huang, W. and Chen, F. (2016) Forcing mechanisms of orbital-scale changes in winter rainfall over northwestern China during the Holocene. The Holocene, 26 (4). pp. 549-555. DOI 10.1177/0959683615612569.
Full text not available from this repository.Abstract
The moisture history in arid central Asia (ACA) differs from that in the Asian monsoon region during the Holocene. Much less is known about causes of Holocene moisture changes in ACA than Asian monsoon precipitation changes, hampering our understanding of their spatiotemporal differences. In this study, orbital-scale evolution of winter rainfall in northwestern China (a part of the core zone in ACA) during the Holocene and possible driving mechanisms are investigated using results from a long-term transient simulation performed by an atmosphere–ocean–sea-ice coupled general circulation model, the Kiel Climate Model, forced by orbital variations. Our results reveal a persistent wetting trend in northwestern China in winter throughout the Holocene, which is in response to winter insolation at mid-northern latitudes. Winter insolation can influence the rainfall via three ways. First, increasing latitudinal gradient of the incoming solar insolation at mid-latitudes strengthens the westerly intensity. Second, the evaporation is enhanced because of insolation-induced winter temperature rising, resulting in an increase in the air humidity. Intensified westerly winds and the increased water vapour together are conductive to enhance moisture transport towards northwestern China and thus increase winter precipitation in this area. Third, the increasing trend of winter insolation weakens the East Asian winter monsoon, which is favourable for the formation of rainfall via crippling the Siberian High that is beneficial for atmospheric lifting motion.
Document Type: | Article |
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Keywords: | arid central Asia, Holocene, insolation, paleoclimate simulation, precipitation, westerly winds |
Research affiliation: | OceanRep > The Future Ocean - Cluster of Excellence > FO-R09 OceanRep > The Future Ocean - Cluster of Excellence Kiel University |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | SAGE Publications |
Projects: | Future Ocean |
Date Deposited: | 22 Mar 2017 11:17 |
Last Modified: | 17 May 2019 11:48 |
URI: | https://oceanrep.geomar.de/id/eprint/37103 |
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