鍦扮悊鐮旂┒ 鈥衡�� 1985, Vol. 4 鈥衡�� Issue (1): 63-70.DOI: 10.11821/yj1985010007

鈥� 鐮旂┒鎶ュ憡 鈥� 涓婁竴绡�    涓嬩竴绡�

澶╁北澶╂睜灞辫胺椋庣殑姘斿�欑爺绌�

鏋椾箣鍏�1, 鏉庢槧姹�2   

  1. 1. 鍥藉姘旇薄灞�鐮旂┒闄�;
    2. 鏂扮枂缁村惥灏旇嚜娌诲尯鏄屽悏宸炴皵璞″眬
  • 鏀剁鏃ユ湡:1983-09-19 淇洖鏃ユ湡:1984-06-04 鍑虹増鏃ユ湡:1985-03-15 鍙戝竷鏃ユ湡:1985-03-15

THE CLIMATOLOGICAL RESEARCH OF THE MOUNTAIN-VALLEY BREEZE IN TIANSHAN MOUNTAINS

Lin Zhiguang1, Li Yingjiang2   

  1. 1. Academy of Meteorological Science, National Meteorlogical Bureau;
    2. Changji District Meteorogical Bureau, Xin Jiang
  • Received:1983-09-19 Revised:1984-06-04 Online:1985-03-15 Published:1985-03-15

鎽樿锛� 鏈枃璁ㄨ浜嗗ぉ灞卞ぉ姹犲北璋烽鐨勯鍚戙�侀閫熴�佽浆鎹㈡湡銆佸鑺傚彉鍖栧強瀵规俯婀垮害鏃ュ彉鍖栫殑褰卞搷銆�

Abstract: 1.There is a typical phenomenon of mountain-valley breeze in Tianchi. The direction of the moutain breeze is southeast, and the valley breeze northwest, the frequency of mountain breeze is the largest in winter and that of the valley breeze in May and June.2.The velocity of mountain breeze is larger than the valley breeze, this phenomenon is abnormal.3.There are two transitional periods between mountain and valley breezes. The time of occurence of them has a seasonal change, the time of the transitional period from mountain to valley breeze is about three hours later than the sunrise, but from valley to mountain breeze, a little earlier than the sunset.4. The days of mountain-valley breeze in summer is more than in winter.5. After the time of the transitional period (from mountain to valley breeze), the air temperature increses 2-6鈩� and the relative humidity decreses 10-20% suddenly; and from valley to mountain breeze, the air temperature decreses 2-4鈩�, ley, to mountain breeze,the air temperature decrese 2-4鈩�, and the relative humidity increses 15-25% suddenly.6.The wind velocity of mountain valley breeze changes with diurnal range of air temperature, the larger the diurnal range, the larger the wind velocity.