Clim. Past, 7, 847-868, 2011
www.clim-past.net/7/847/2011/
doi:10.5194/cp-7-847-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Regional climate model experiments to investigate the Asian monsoon in the Late Miocene
H. Tang1, A. Micheels2,3, J. Eronen1, and M. Fortelius1
1Department of Geosciences and Geography, P.O. Box 64, 00014, University of Helsinki, Finland
2Biodiversity and Climate Research Centre (LOEWE BiK-F), Senckenberganlage 25, 60325, Frankfurt/Main, Germany
3Senckenberg Research Institute and Nature Museum, Senckenberganlage 25, 60325, Frankfurt/Main, Germany

Abstract. The Late Miocene (11.6–5.3 Ma) is a crucial period in the history of the Asian monsoon. Significant changes in the Asian climate regime have been documented for this period, which saw the formation of the modern Asian monsoon system. However, the spatiotemporal structure of these changes is still ambiguous, and the associated mechanisms are debated. Here, we present a simulation of the average state of the Asian monsoon climate for the Tortonian (11–7 Ma) using the regional climate model CCLM3.2. We employ relatively high spatial resolution (1° × 1°) and adapt the physical boundary conditions such as topography, land-sea distribution and vegetation in the regional model to represent the Late Miocene. As climatological forcing, the output of a Tortonian run with a fully-coupled atmosphere-ocean general circulation model is used. Our regional Tortonian run shows a stronger-than-present East Asian winter monsoon wind as a result of the enhanced mid-latitude westerly wind of our global forcing and the lowered present-day northern Tibetan Plateau in the regional model. The summer monsoon circulation is generally weakened in our regional Tortonian run compared to today. However, the changes of summer monsoon precipitation exhibit major regional differences. Precipitation decreases in northern China and northern India, but increases in southern China, the western coast and the southern tip of India. This can be attributed to the changes in both the regional topography (e.g. the lower northern Tibetan Plateau) and the global climate conditions (e.g. the higher sea surface temperature). The spread of dry summer conditions over northern China and northern Pakistan in our Tortonian run further implies that the monsoonal climate may not have been fully established in these regions in the Tortonian. Compared with the global model, the high resolution regional model highlights the spatial differences of the Asian monsoon climate in the Tortonian, and better characterizes the convective activity and its response to regional topographical changes. It therefore provides a useful and compared to global models, a complementary tool to improve our understanding of the Asian monsoon evolution in the Late Miocene.

Citation: Tang, H., Micheels, A., Eronen, J., and Fortelius, M.: Regional climate model experiments to investigate the Asian monsoon in the Late Miocene, Clim. Past, 7, 847-868, doi:10.5194/cp-7-847-2011, 2011.
 
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