1 It is suggested that topography and diabatic heating play important roles in the motion of landfall TCs.

2 In tropical cyclone, the driving factor is diabatic heating, while in extratropical cyclone, the relatively important factor is the torque relating to the baroclinic instability of frontal zone.

3 The warm advection and diabatic heating can increase the curvature.

4 Maj or contribution came from the diabatic heating term especially at where heavy precipitation occurred.

5 The diabatic input sampling circuit is put on every flip flop to use both receving data input and isolating it from external input during holding data.

6 Considering diabatic heating is the most notable feature of moist Q vector, and the difference among moist Q vectors is caused by differing conductional methods of diabatic heating.

7 In night, the diabatic heating term is dominant factor which results in frontolysis.

8 The wind field is residual circulation calculated from diabatic rate.

9 The overall diabatic heating is positive in the whole troposphere in summer, with the most intense heating located in the boundary layer.

10 The diabatic heating decreased when the vortex moving away from the plateau.

11 In this paper, the effect of upper course was discussed that is excited by diabatic heating region moving with wave.

12 Based on certain assumptions, three different definitions of efficiency were proposed, that is adiabatic efficiency, diabatic efficiency and heat efficiency.

13 Phase trajectores of well - posed systems are analysed under simple diabatic conditions.

14 It is shown that to the north of a heating region, although there is no diabatic heating, there still exists deep negative vorticity forcing due to the horizontal inhomogeneous in the westerly flow.

15 The fouling of heat-exchange equipments is usual, which consists in the nature, daily life and different kinds of industrial production process, especially in the various diabatic processes.

16 What is presented in Part I is a theoretical analysis on the effects of diabatic heating and the horizontal temperature distribution.

17 The NCEP/NCAR reanalysis data are employed to analyze the diurnal variation of the diabatic heating and atmospheric circulation over the Tibetan Plateau and it's surrounding areas.

18 First, in the field of atmospheric dynamics the developments in dynamics of diabatic waves and low frequency waves, the dispersive effects of turbulence and nonlinear atmospheric waves are reviewed.