1. Anticyclones cause cloudless blue skies and high temperatures in summer.

2. The anticyclone brought bright sunshine and calm conditions to most areas.

3. Only on the very last day did an anticyclone grace our shores.

4. A center of high atmospheric pressure ; an anticyclone.

5. The results show that Mongolia anticyclone is the main synoptic system impacting dust-storm .

6. The left and right cyclone and anticyclone rotation of the bow echo on its forward way decides the direction of developing or decreasing of the future strong convection weather.

7. In contrast, the aestival circulation shows the anticyclone pattern and its vertical structure has few changes in that season.

8. The anticyclone weather situations are more favorable than the cyclonic ones.

9. In the Southern Hemisphere an anticyclone circulates counterclockwise around the high-pressure center, as contrasted to the Northern Hemisphere.

10. There is a mesoscale anticyclone addy near Qingdao and Shidao.

11. Second is anticyclone this happens when winds form a wind system around a high.

12. Subject to the anticyclone anchored in central China, 21W will move along its southeastern periphery in a SW to WSW direction in the next 72 hours.

13. The Pacific subtropical anticyclone appears strong and large, its position leans toward south, and its ridge extends to west.

14. As interactions with JANGMI steering flow from the anticyclone in southern China and moves WNW.

15. Unlike a low-pressure center, which may be composed of two or more air masses, an anticyclone usually consists of a single air mass.

16. Summer rainfall anomalies in North China relates to the Indian summer monsoon, the South sea monsoon, Sub-tropical anticyclone, South Asian anticyclone and cold air anomaly.

17. The sinking motion on the western side of subtropical anticyclone is favourable to the increase of the warm dry lid.

18. Tianjin's climate is characterized by hot, humid summers, due to the monsoon, and dry, cold winters, due to the Siberian anticyclone.

19. The various terms in the potential vorticity equations have made very different contributions to the evolution of the anticyclone.

20. According to the weather system the rain of Wenzhou are classified into cold air, inverse trough, southwest low vortex, Mei-Yu, typhoon, convection on edge of subtropical anticyclone.

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21. The heavy fogs of Shangqiu are formed by the weather situations: continental anticyclone, warm zone in front of cold front, uniform pressure field, and low pressure with an inverted trough.

22. Assuming constant heating source, it is found that in upper layer the anticyclone is the result of the development of typhoon.

23. The formation of the warm dry lid over the southeast coastal region of china is mainly due to the advection of warm and dry air along the western side of subtropical anticyclone.

24. This generates ascent as well as negative vorticity source, which corresponds to a strongly anomaly anticyclone center appearing to the north of the heating region.