Numerical simulations of asian dust-aerosols and regional impact on weather and climate- part I: Control case-prcm simulation without dust-aerosols

NCUIR > College of Earth Sciences > Department of Atmospheric Sciences > journal & Dissertation > Item 987654321/100054

Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/100054

Title:	Numerical simulations of asian dust-aerosols and regional impact on weather and climate- part I: Control case-prcm simulation without dust-aerosols
Authors:	林能暉;Sun, Wen-Yih;Yang, Kate Jr-Shiuan;Lin, Neng-Huei
Contributors:	地球科學學院大氣科學學系
Date:	2013-12-01
Issue Date:	2026-04-21 13:47:12 (UTC+8)
Publisher:	AAGR Aerosol and Air Quality Research;Cham: Springer International Publishing
Abstract:	摘要： Aerosol particles affect atmospheric radiation and cloud microphysics, and are considered a major uncertainty in climate forcing. At the same time, accurate simulation and prediction of meteorological conditions are necessary to simulate the distribution and chemical reaction of the aerosols. Distribution of pollutions can also be used to validate meteorological models. This paper consists of two parts: Part I: Numerical simulation of weather and soil conditions from the Purdue Regional Climate Model (PRCM); and Part II: Numerical modeling of online interaction between dust and weather/climate. Both parts were integrated continuously from April 08 to 24, 1998 without nudging or restarting. The detailed treatment of soil and the planetary boundary layer (PBL), using the semi-conserved ice-potential temperature and total water substance as prognostic variables, a local reference to calculate the pressure gradient, and the accurate advection scheme, allowed the PRCM to well reproduce the movements of the fronts/cyclones, downslope wind, upper/mid-level-jet, vertical mixing, and the low-level convergence over a complex terrain. They are crucial to the lift, dispersion, and transport of dusts over the Gobi Desert, the Taklimakan Desert, and the downstream regions. The dust model in Part II calculated the production, mixing, transport/removal, and radiative property of the dusts using the meteorology generated by the PRCM. The radiative effects of the dusts calculated from the dust model were then fed back to the PRCM. Because no nudging or restarting was applied during 17 continuous days of integration, the conservation laws of momentum, energy, and mass (including dry air, water substances and dusts) are valid. Hence, the PRCM provides data that are consistent for studying the movement of aerosols and the interactions among the aerosols, weather, and soil. 其他題名： Aerosol Air Qual. Res 出版者： Cham: Springer International Publishing 出版日期： 2013-12-01 出處： Aerosol and air quality research, 2013-12, Vol.13 (6), p.1630-1640 版權： Taiwan Association for Aerosol Research 2013 識別號： ISSN: 1680-8584 識別號： ISSN: 2071-1409 識別號： EISSN: 2071-1409 識別號： DOI: 10.4209/aaqr.2013.06.0207
Appears in Collections:	[Department of Atmospheric Sciences] journal & Dissertation

Files in This Item:

File	Description	Size	Format
index.html		0Kb	HTML	21	View/Open

社群 sharing

Loading...