A Diagnostic Study of Moist Potential Vorticity Generation in an Extratropical Cyclone
A Diagnostic Study of Moist Potential Vorticity Generation in an Extratropical Cyclone ①作者机构:Department of Physics University of Toronto Toronto Ontario Canada
出 版 物:《Advances in Atmospheric Sciences》 (大气科学进展(英文版))
年 卷 期:1998年第15卷第2期
页 面:19-33页
核心收录:
学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学]
主 题:Moist potential vorticity (MPV) generation Extratropical cyclones
摘 要:Moist potential vorticity (MPV) and its generation may be important in the development of mesoscale structures such as rainbands within cyclones. In an adiabatic and frictionless flow, MPV generation is possible if the flow is three-dimensional and the air is unsaturated. Moist potential vorticity can be generated through the combined effects of gradients in the potential temperature and moisture fields. The diagnosis of MPV generation in an extratropical cyclone was performed with the ECMWF objectively analyzed fields for a system that developed during February 1992. It was found that at various stages during the development of the cyclone, negative MPV was generated: at the north end of the cold front; along the occluded front and the cold front; and in the region of the warm core. This pattern of negative MPV generation is in excellent agreement with the predictions of previous theoretical and numerical studies. After the cyclone ceased to deepen, the region of negative MPV generated in the cyclone was horizontally advected into a saturated area. The area of negative MPV generated both along the occluded front in this case study and in the region of the bent-back warm front in a numerical simulation showed a mesoscale structure with a width of about 200-500 km. It was found that the intrusion of moist or dry air into baroclinic zones was important for MPV generation. In addition, baroclinicity increase (adjacent to the area of condensation) in the regions of high moisture gradients led to significant MPV production.