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DOI | 10.1175/JAS-D-19-0039.1 |
Application of the Compressible, Nonhydrostatic, Balanced Omega Equation in Estimating Diabatic Forcing for Parameterization of Inertia-Gravity Waves: Case Study of Moist Baroclinic Waves Using WRF | |
Haghighatnasab, Mahnoosh1; Mirzaei, Mohammad1; Mohebalhojeh, Ali R.1; Zuelicke, Christoph2; Plougonven, Riwal3 | |
2020 | |
发表期刊 | JOURNAL OF THE ATMOSPHERIC SCIENCES |
ISSN | 0022-4928 |
EISSN | 1520-0469 |
出版年 | 2020 |
卷号 | 77期号:1页码:113-129 |
文章类型 | Article |
语种 | 英语 |
国家 | Iran; Germany; France |
英文摘要 | The parameterization of inertia-gravity waves (IGWs) is of considerable importance in general circulation models. Among the challenging issues faced in studies concerned with parameterization of IGWs is the estimation of diabatic forcing in a way independent of the physics parameterization schemes, in particular, convection. The requirement is to estimate the diabatic heating associated with balanced motion. This can be done by comparing estimates of balanced vertical motion with and without diabatic effects. The omega equation provides the natural method of estimating balanced vertical motion without diabatic effects, and several methods for including diabatic effects are compared. To this end, the assumption of spatial-scale separation between IGWs and balanced flows is combined with a suitable form of the balanced omega equation. To test the methods constructed for estimating diabatic heating, an idealized numerical simulation of the moist baroclinic waves is performed using the Weather Research and Forecasting (WRF) Model in a channel on the f plane. In overall agreement with the diabatic heating of the WRF Model, in the omega-equation-based estimates, the maxima of heating appear in the warm sector of the baroclinic wave and in the exit region of the upper-level jet. The omega-equation-based method with spatial smoothing for estimating balanced vertical motion is thus presented as the proper way to evaluate diabatic forcing for parameterization of IGWs. |
英文关键词 | Inertia-gravity waves |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000501238300002 |
WOS关键词 | POTENTIAL-VORTICITY INVERSION ; NUMERICAL SIMULATIONS ; GENERATION MECHANISMS ; LIFE-CYCLE ; PART I ; CONVECTION ; IMBALANCE ; MODELS ; STRATOSPHERE ; DYNAMICS |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/280250 |
专题 | 地球科学 |
作者单位 | 1.Univ Tehran, Inst Geophys, Tehran, Iran; 2.Univ Rostock, Leibniz Inst Atmospher Phys, Rostock, Germany; 3.Univ Paris Saclay, Lab Meteorol Dynam, CNRS, Ecole Polytech,IPSL, Palaiseau, France |
推荐引用方式 GB/T 7714 | Haghighatnasab, Mahnoosh,Mirzaei, Mohammad,Mohebalhojeh, Ali R.,et al. Application of the Compressible, Nonhydrostatic, Balanced Omega Equation in Estimating Diabatic Forcing for Parameterization of Inertia-Gravity Waves: Case Study of Moist Baroclinic Waves Using WRF[J]. JOURNAL OF THE ATMOSPHERIC SCIENCES,2020,77(1):113-129. |
APA | Haghighatnasab, Mahnoosh,Mirzaei, Mohammad,Mohebalhojeh, Ali R.,Zuelicke, Christoph,&Plougonven, Riwal.(2020).Application of the Compressible, Nonhydrostatic, Balanced Omega Equation in Estimating Diabatic Forcing for Parameterization of Inertia-Gravity Waves: Case Study of Moist Baroclinic Waves Using WRF.JOURNAL OF THE ATMOSPHERIC SCIENCES,77(1),113-129. |
MLA | Haghighatnasab, Mahnoosh,et al."Application of the Compressible, Nonhydrostatic, Balanced Omega Equation in Estimating Diabatic Forcing for Parameterization of Inertia-Gravity Waves: Case Study of Moist Baroclinic Waves Using WRF".JOURNAL OF THE ATMOSPHERIC SCIENCES 77.1(2020):113-129. |
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