NUMERICAL SIMULATIONS OF HEATING ANOMALY EFFECTS OF TIBETAN PLATEAU ON CIRCULATION IN SUMMER

A 5-layer numerical model with p-σ incorporated coordinate system and primitive equations is used to simulate the effects of heating anomaly at and over the Tibetan(Qinghai-Xizang)Plateau on the circulations in East Asia in sum- mer,The model is described briefly in the text and the results are analysed in somewhat detail.Results show that the sur- face albedo,the drag coefficient,the evaporation rate and the ground temperature all have large influences on the circula- tion near the Plateau and in East Asia.When the heating at the surface increases,the Tibetan high in the upper troposphere intensifies,too.Its area enlarges and its axis tilts to northwest.The upper tropical easterly increase and shifts to north.The southwesterly in the lower troposphere,in consistence,also increases.The cross-equatorial low-lev- el currents along Somali and South India are influenced to increase their speeds while those over North Australia de- crease.The land low over the Asian Continent deepens.Meanwhile the upward motions over the land of east China and over the Indo-China Peninsula intensify and therefore the precipitation over those areas increases.However,along the coastal area of China the upward motions and therefore the precipitation decrease. Atmospheric heat source anomaly has large influence on the circulation,too.Simulated results indicate that heat source anomaly in the lower atmosphere over the Plateau influences the intensity and the position of the monsoon circu- lation while that in the upper atmosphere only affects the intensity.The heating status over the Plateau has slight influ- ence on the westerly jet,north of the Plateau,while it has strong effect on the subtropical jet at the mid and low latitudes.

RESPONSE OF TROPICAL ATMOSPHERIC CIRCULATION TO THE OCEAN-LAND SURFACE HEATING——AN ANALYTICAL SIMULATION

A linear steady model is constructed to investigate the response of the tropical atmosphere to diabatic heating.The basic equations are similar to those used by Gill(1980),but the long-wave approximation is removed and periodic boundary conditions are taken in longitude.According to the features of the underlying surface temperature(including oceans and land),the heat sources(sinks)are given.Using this analytical model,we have simulated the climatological fields of wind and air pressure in the lower layers of the tropical and subtropical atmosphere in summer(June—August)and winter(December—February). The main features of observations are depicted in simulated fields.

EFFECTS OF THREE-DIMENSIONAL STRUCTURE OF HEATING FIELD ON THE SUMMER MONSOON CIRCULATION IN ASIA

In this paper,a primitive equation linear wave model is used to examine the effects of three-dimen- sional structure of heating field on the behavior of stationary planetary waves in summer and to compare the roles of different heating functions for the formation and maintenance of summer monsoon circulation in Asia.It is shown that the aloft heating connected with the latent heating,especially the deep condensation heating associated with the cumulus convection in low latitudes,plays a crucial part in the Asian summer mon- soon and the structures of planetary wave responses are quite sensitive to the vertical distribution of heating.

Propagation and Mechanisms of the Quasi-Biweekly Oscillation over the Asian Summer Monsoon Region

The propagation and underlying mechanisms of the boreal summer quasi-biweekly oscillation（QBWO）over the entire Asian monsoon region are investigated,based on ECMWF Interim reanalysis（ERA-Interim）data,GPCP precipitation data,and an atmospheric general circulation model（AGCM）.Statistical analyses indicate that the QBWO over the Asian monsoon region derives its main origin from the equatorial western Pacific and moves northwestward to the Bay of Bengal and northern India,and then northward to the Tibetan Plateau（TP）area,with a baroclinic vertical structure.Northward propagation of the QBWO is promoted by three main mechanisms：barotropic vorticity,boundary moisture advection,and surface sensible heating（SSH）.It is dominated by the barotropic vorticity effect when the QBWO signals are situated to the south of 20°N.During the propagation taking place farther north toward the TP,the boundary moisture advection and SSH are the leading mechanisms.We use an AGCM to verify the importance of SSH on the northward propagation of the QBWO.Numerical simulations confirm the diagnostic conclusion that the equatorial western Pacific is the source of the QBWO.Importantly,the model can accurately simulate the propagation pathway of the QBWO signals over the Asian monsoon region.Simultaneously,sensitivity experiments demonstrate that the SSH over northern India and the southern slope of the TP greatly contributes to the northward propagation of the QBWO as far as the TP area.

Treatment of Severe Cholestatic Hepatitis by Integrating Traditional Chinese and Western Medicines

Objective: To study the curative effect of Chinese medicines in treating severe cholestatic hepatitis (SCH).Methods: Three hundred and fifty patients of SCH with total bilirubin level 171 μmol/L were treated with Chinese medicines. Those with Blood Stasis Syndrome were treated with the recipe mainly consisting of Radix Paeoniae Rubra, and those accompanied by blood Heat, fluid retention in the epigastric region, dampness disseminated in Sanjiao ( ) or Yang deficiency of both Spleen and Kidney were treated with recipe modified according to the symptoms and signs.Results: The treatment was markedly effective in 288 cases and effective in 26 cases, the total effective rate being 89.7%.Conclusion: It is difficult to treat severe cholestatic hepatitis, es pecially the chronic cholestatic good effect of Chinese herbal medicine in eliminating jaundice.