蒙古高压

  • 网络Mongolian high
蒙古高压蒙古高压
  1. 结果表明,东亚的地形动力作用对以下天气系统有重要影响:(1)蒙古高压的生成、发展;

    It shows that the mountain dynamic effect plays important role in four weather-systems over the East-Asia : ( 1 ) forming and developing of the Mongolian High ;

  2. 华北地区冬季气温偏低、偏高年的北半球环流形势存在明显的差异,亚洲区极涡面积、乌拉尔山东部高压脊、东亚大槽及蒙古高压是重要的影响因子;

    There were differences in atmospheric general circulation patterns between cold and warm years , and polar vortex , with the high-pressure ridge around Ural Mountains , the East Asian trough , and the Mongolian high pressure being important influence factors ;

  3. 冬季,蒙古高压北部减弱,南部稍有增强;

    The north of Siberian high becomes weak and the south of it strengthens in winter .

  4. 0801南方雪灾与同期蒙古高压中期活动的关系

    Contemporaneous Relationship between " 0801 Snow Storm over Southern China " and Medium-term Activities of Mongolian High

  5. 冬季在强大的蒙古高压的笼罩之下,北方的寒冷甚于版图中的其他地区。

    Under the powerful Siberian high winter in north China . It is more unbearable than any other places .

  6. 这里常年受蒙古高压控制,是典型的内陆气候。

    Controlled by high atmospheric pressure from Mongolia all the year round , the place has a typical inland climate .

  7. 冷锋过境后受蒙古高压前部控制时,平均最大混合层厚度最高为(946m)。

    But it was maximum ( 946 m ) when Lanzhou Proper was controlled by the front of a high pressure system after cold front passage .

  8. 对东亚季风气候具有决定性影响的系统,如副热带高压、蒙古高压、印度低压以及西风急流等也模拟得比较好。

    The large scale systems such as Subtropical High , Mongolia High , Indian Low which have important influence on the East Asia Monsoon are also simulated pretty well .

  9. 由于受下垫面地理特征、蒙古高压和青藏高原东北侧反气旋(小高压)的影响,降水梯度西南大于东北。

    Because of the effect of geography characteristic and Mongolia high pressure and anticyclone of the northeast of Qinghai-Xizang Plateau , the grads of precipitation is greater in the southwest than in the northeast .

  10. 冬季受西伯利亚-蒙古高压的影响,呈现干燥寒冷的气候特征,而夏季则受东亚夏季风的影响,表现为高温多雨,雨热同季的气候特征。

    Winter climate here , under the influence of Siberia-Mongolia high , is characterized by dry and cold . while in summer its hot and rainy , rain in hot season , by the effect of East Asian summer monsoon .

  11. PDO和SAIB区域的海温变化,尤其是前期(特别是夏季)SAIB区的正海温异常可能对东亚冬季风(蒙古冷高压)的加强活动有指示意义。

    Since the SSTA mode is relatively stationary , the PDO and SST anomaly in the SAIB region could be the factor to predict the Mongolia high activity in winter ( East Asian winter monsoon ) .

  12. 华北冬季气温与蒙古冷高压异常、东亚大槽异常、极涡面积异常密切相关。

    Winter air temperature in North China has important relationship with the Mongolia high anomaly , the East Asian trough anomaly and the acreage of polar vortex anomaly .

  13. 对1998年3月新疆强切变线天气的分析表明,蒙古阻塞高压对切变线形成起决定性作用,切变线是一个冷性结构的风辐合带,白天较弱,夜晚较强。

    Analyzed a case of severe shear line in Xinjiang in March in 1998 , it is shown that Mongolia blocking anticyclone act decisively on the shear line ; the shear line is a cold wind convergence zone , which is weaker in the day than at night .

  14. 进一步证实高北纬极地气候可以通过西风带和蒙古、西伯利亚高压系统传输到东亚东亚季风区。

    Further , they verify that high-latitude climate can transfer to East Asia monsoon region via the westerly and Mongolia and Siberian high pressure system .