Articles | Volume 13, issue 14
Atmos. Chem. Phys., 13, 6965–6982, 2013
https://doi.org/10.5194/acp-13-6965-2013
Atmos. Chem. Phys., 13, 6965–6982, 2013
https://doi.org/10.5194/acp-13-6965-2013

Research article 23 Jul 2013

Research article | 23 Jul 2013

Impacts of the mountain–plains solenoid and cold pool dynamics on the diurnal variation of warm-season precipitation over northern China

Xinghua Bao1,2 and Fuqing Zhang2 Xinghua Bao and Fuqing Zhang
  • 1State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China
  • 2Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania, USA

Abstract. Convection-permitting numerical experiments using the Weather Research and Forecasting (WRF) model are performed to examine the impact of a thermally driven mountain–plains solenoid (MPS) on the diurnal variation of warm-season precipitation over northern China. The focus of the analyses is a 15-day simulation that uses the 8-day average of the NCEP GFS gridded analyses at 00:00 UT between 17 and 24 June 2004 for the initial conditions and the 8-day averages at 00:00, 06:00, 12:00, and 18:00 UT for the lateral boundary conditions. Despite differences in rainfall intensity and location, the control experiment captures the essence of the observed diurnal variation of warm-season precipitation in northern China. Consistent with observations, the simulated local precipitation peak initiates in the afternoon on the eastern edge and the immediate lee of the mountain ranges due to the upward branch of the MPS. The peak subsequently propagates downslope and southeastward along the steering-level mean flow, reaching the central North China Plain around midnight and early morning hours, resulting in a broad area of nocturnal precipitation maxima over the central plains. Sensitivity experiments show that, besides the impact of the MPS, cold pool dynamics play an essential role in the propagation and maintenance of the precipitation peak over the plains.

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