Abstract. Although the collapses of several Neolithic cultures in China areconsidered to have been associated with abrupt climate change during the4.2kaBP event (4.2–3.9kaBP), the timing and nature of this event andthe spatial distribution of precipitation between northern and southern Chinaare still controversial. The hydroclimate of this event insoutheastern China is still poorly known, except for a few published recordsfrom the lower reaches of the Yangtze River. In this study, a high-resolutionrecord of monsoon precipitation between 5.3 and 3.57kaBP based on astalagmite from Shennong Cave, Jiangxi Province, southeast China, ispresented. Coherent variations in δ18O and δ13Creveal that the climate in this part of China was dominantly wet between 5.3and 4.5kaBP and mostly dry between 4.5 and 3.57kaBP, interrupted by awet interval (4.2–3.9kaBP). A comparison with other records frommonsoonal China suggests that summer monsoon precipitation decreased innorthern China but increased in southern China during the 4.2kaBP event.We propose that the weakened East Asian summer monsoon controlled by thereduced Atlantic Meridional Overturning Circulation resulted in thiscontrasting distribution of monsoon precipitation between northern andsouthern China. During the 4.2kaBP event the rain belt remained longer atits southern position, giving rise to a pronounced humidity gradient betweennorthern and southern China.
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Regional simulation of Indian summer monsoon intraseasonal oscillations at gray-zone resolution
Abstract. Simulations of the Indian summer monsoon by the cloud-permitting Weather Research and Forecasting (WRF) model at gray-zone resolution are described in this study, with a particular emphasis on the model ability to capture the monsoon intraseasonal oscillations (MISOs). Five boreal summers are simulated from 2007 to 2011 using the ERA-Interim reanalysis as the lateral boundary forcing data. Our experimental setup relies on a horizontal grid spacing of 9km to explicitly simulate deep convection without the use of cumulus parameterizations. When compared to simulations with coarser grid spacing (27km) and using a cumulus scheme, the 9km simulations reduce the biases in mean precipitation and produce more realistic low-frequency variability associated with MISOs. Results show that the model at the 9km gray-zone resolution captures the salient features of the summer monsoon. The spatial distributions and temporal evolutions of monsoon rainfall in the WRF simulations verify qualitatively well against observations from the Tropical Rainfall Measurement Mission (TRMM), with regional maxima located over Western Ghats, central India, Himalaya foothills, and the west coast of Myanmar. The onset, breaks, and withdrawal of the summer monsoon in each year are also realistically captured by the model. The MISO-phase composites of monsoon rainfall, low-level wind, and precipitable water anomalies in the simulations also agree qualitatively with the observations. Both the simulations and observations show a northeastward propagation of the MISOs, with the intensification and weakening of the Somali Jet over the Arabian Sea during the active and break phases of the Indian summer monsoon.
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- PAR ID:
- 10066880
- Date Published:
- Journal Name:
- Atmospheric Chemistry and Physics
- Volume:
- 18
- Issue:
- 2
- ISSN:
- 1680-7324
- Page Range / eLocation ID:
- 1003 to 1022
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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