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- W2353235929 abstract "Analysis of a sustaining storm rainfall in southern China in June 2005 reveals that when the quasi-longitudinal South Asia High ridge line is stable around 22 °N and the quasi-longitudinal upper jet axis maintains around 35 °N,it is beneficial for the growth of sustaining storm rainfall in southern China and for the forming of double rain-bands between 22～28 °N.The forming of northern rain-band is related to the divergence field of South Asia High.The Gravity Inertial Wave Instability of transversal waves may exist in the northern rain-band and the mixed Vortex Rossby Wave Instability may exist in the southern rain-band.The transformation of baroclinic potential vorticity to barotropic potential vorticity results in the increase of vorticity in lower layers and leads to the precipitation.The transformation of barotropic potential vorticity to baroclinic potential vorticity also happens in lower layers of the southern rain-band.The decrease of barotropic potential vorticity may also result in the increase of positive vorticity and it is beneficial for the development of precipitation." @default.
- W2353235929 created "2016-06-24" @default.
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- W2353235929 date "2008-01-01" @default.
- W2353235929 modified "2023-09-28" @default.
- W2353235929 title "RESEARCH ON THE REASON OF THE DOUBLE RAIN-BANDS’ FORMING IN A SUSTAINING STORM RAINFALL OF SOUTH CHINA" @default.
- W2353235929 hasPublicationYear "2008" @default.
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