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   east xinjiang 在 气象学 分类中 的翻译结果: 查询用时:0.591秒
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east xinjiang
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  东疆
    Analysis of Sandstorm in East Xinjiang
    东疆沙尘暴天气的分析
短句来源
    4. 1992-2000, the degree of land-cover trended improvement obviously in the East Xinjiang.
    显著。 4.1992-2000年,东疆地表植被覆盖的程度改善趋势比较明显;
短句来源
    The precipitation increasing degree in the east Xinjiang is the biggest, gets to 17.42%. The humidity increasing degree in the South Xinjiang is the biggest, gets to 1.68%.
    东疆降水量增幅最大,增加了17.42%,南疆年平均湿度增幅最大,增加了1.68%;
短句来源
    The spatial and temporal distribution character of gale was analyzed using 39 years data from 1961 to 1999 at 90 weather stations in Xinjiang. The results are follow:(1)The gale occurrence is more frequently in north-western of North Xinjiang , East Xinjiang and west of South Xinjiang, most at Alashankou and Dabancheng, lest in the center of Zhunger Basin and the southern periphery of Tarim Basin.
    统计了1961~1999年39a新疆90个气象观测站的气表—1资料,给出新疆大风的时空分布特征,结果表明:(1)年平均大风日数的高值区在北疆西北部、东疆和南疆西部,阿拉山口、达坂城大风最多,准噶尔盆地中心、塔里木盆地南缘最少。
短句来源
    Based on the observation data collected by 77 hydrologic and meteorological stations in Xinjiang, the analyzed results show that the air temperature in Xinjiang has increased in recent 50 years, and the average increase amplitude is 0.27 ℃. 10·a -1 . The average annual temperature has obviously increased since 1987 than that before 1986, especially the increase amplitudes are as high as 0.6~1.6 ℃ in the western and northern parts of north Xinjiang and in east Xinjiang.
    结果表明 ,新疆近 5 0a来的气温呈上升趋势 ,平均增长率为 0 .2 7℃·10a-1.1987年以后的平均气温较 1986年以前有明显升高 ,尤其是北疆西部、北部和东疆地区增幅较大 ,达 0 .6~ 1.6℃ .
短句来源
更多       
  东疆
    Analysis of Sandstorm in East Xinjiang
    东疆沙尘暴天气的分析
短句来源
    4. 1992-2000, the degree of land-cover trended improvement obviously in the East Xinjiang.
    显著。 4.1992-2000年,东疆地表植被覆盖的程度改善趋势比较明显;
短句来源
    The precipitation increasing degree in the east Xinjiang is the biggest, gets to 17.42%. The humidity increasing degree in the South Xinjiang is the biggest, gets to 1.68%.
    东疆降水量增幅最大,增加了17.42%,南疆年平均湿度增幅最大,增加了1.68%;
短句来源
    The spatial and temporal distribution character of gale was analyzed using 39 years data from 1961 to 1999 at 90 weather stations in Xinjiang. The results are follow:(1)The gale occurrence is more frequently in north-western of North Xinjiang , East Xinjiang and west of South Xinjiang, most at Alashankou and Dabancheng, lest in the center of Zhunger Basin and the southern periphery of Tarim Basin.
    统计了1961~1999年39a新疆90个气象观测站的气表—1资料,给出新疆大风的时空分布特征,结果表明:(1)年平均大风日数的高值区在北疆西北部、东疆和南疆西部,阿拉山口、达坂城大风最多,准噶尔盆地中心、塔里木盆地南缘最少。
短句来源
    Based on the observation data collected by 77 hydrologic and meteorological stations in Xinjiang, the analyzed results show that the air temperature in Xinjiang has increased in recent 50 years, and the average increase amplitude is 0.27 ℃. 10·a -1 . The average annual temperature has obviously increased since 1987 than that before 1986, especially the increase amplitudes are as high as 0.6~1.6 ℃ in the western and northern parts of north Xinjiang and in east Xinjiang.
    结果表明 ,新疆近 5 0a来的气温呈上升趋势 ,平均增长率为 0 .2 7℃·10a-1.1987年以后的平均气温较 1986年以前有明显升高 ,尤其是北疆西部、北部和东疆地区增幅较大 ,达 0 .6~ 1.6℃ .
短句来源
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  “east xinjiang”译为未确定词的双语例句
    Distributive features of wind pressure in Xinjiang are:wind pressures in north Xinjiang are bigger than those in south Xinjiang, wind pressures in west and east Xinjiang are bigger than those in middle Xinjiang;
    新疆风压分布特征为 :北疆大于南疆 ,西部、东部大于中部 ;
短句来源
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  east xinjiang
More than twenty mafic-ultramafic complexes, which host several mediumor large-sized Cu-Ni deposits, occur along the Huangshan-Jingerquan (HJ) belt in East Xinjiang.
      
Geology and genesis of the mafic-ultramafic complexes in the Huangshan-Jingerquan (HJ) belt, East Xinjiang
      


A scientific division of China's cotton cultivated area is favourable to the country's cotton production in accordance with the principle of adopting suitable measures to local conditions, practicing reasonable allocation and guiding production according to various types.According to ecological and srio-economic conditions, basic characteristics of cotton production and current state of allocation, China's cotton cultivated area can be divided into five major cotton regions and twelve cotton subre-gions. They...

A scientific division of China's cotton cultivated area is favourable to the country's cotton production in accordance with the principle of adopting suitable measures to local conditions, practicing reasonable allocation and guiding production according to various types.According to ecological and srio-economic conditions, basic characteristics of cotton production and current state of allocation, China's cotton cultivated area can be divided into five major cotton regions and twelve cotton subre-gions. They are: 1 ) the Huanghe Valley cotton region (including four subre-gions: North China plain, Huang-Huai plain, Fen-Wei-Luo Plain, and Beijing-Tianjin-Tangshan area); 2) the Yangtze Valley cotton region (including five subregions. the Lower Yangtze Valley, the Middle Yangtez Valley, the Upper Yangtze Valley, the Nanyang-Xiangyang basin, and the Southern Red Earth Hilly area); 3 ) the Northwestern In terior cotton region (including three subregions. south Xinjiang, East Xinjiang,and North Xinjiang-Hexi Corridor); 4 ) the early-maturing cotton region; and 5 ) South China cotton region.The North China Plain is a famous cotton area of our country, Possessing the optimum ecological conditions very suitable for the cotton cultivation with great potential in increasing production .South Xinjiang and the Huang Huai Plain are also cotton-production areas known for their optimum ecological conditions, but the current status of cotton development is handicapped by the Relatively low level of economic and technical conditions, yet they have great potentialities.The Lower and Middle Yangtze Valley Plain is a large high-yield cotton-cultivated area distrbuted intensively with cotton fields.It is suitable to cotton cullivation but with limited potential in development .The Fen-Wei-Luo Plain, North Xinjiang,and Nanyang-Xiangyang Basin are also main cotton production areas but they have less potential .The Upper Yangtze Valley, the Southern Red Earth Hilly Area, South China, and Northern Early-Maturing Cotton Regions are ecologically less suitable to cotton production; Cotton field there are small in acreage and distributed separately .From strategic point of view of allocation, the future development of China's cotton-producing areas should take into account the following measures, i.e.to consolidate and improve cotton concentrated areas of Lower and Middle Yangtze Valley Regions,to actively construct the cotton producing area of North China Plain, to develop gradually new cotton area of the Huang-Huai Plain, to create conditions to explore high-quality cotton area in South Xinjiang,to adjust and diminish cotton acreage of the regions where ecologically unfavorable to cotton cultivation and to concentrate properly the dispersedistributed cotton acreage, so as to establish a rational alloction system of cotton development.

本文根据自然生态条件、社会经济条件、棉花生产基本特征和布局现状,将我国棉区划分为五个一级棉区(大棉区)和十二个二级棉区(亚区),并对各棉区的条件、基础、存在问题和发展方向进行了分析评价。同时,还按照自然生态因素的地域组合,将各棉区的宜棉程度分为最适宜、适宜、和次适宜三个等级类型。

Maximum wind speed distribution law in building design in Xinjiang is studied by the entropy maximum principle. Some regularities of maximum wind in Xinjiang is studied by analyzing 36a observational data from about 100 meteorological stations .And then,a predicting model on wind pressure coefficient in Xinjiang is built,that is W0 =0.0613e-0.0001h .Distributive feature of wind pressure in Xinjiang is disclosed by prediction model and probability model. The results show that maximum wind...

Maximum wind speed distribution law in building design in Xinjiang is studied by the entropy maximum principle. Some regularities of maximum wind in Xinjiang is studied by analyzing 36a observational data from about 100 meteorological stations .And then,a predicting model on wind pressure coefficient in Xinjiang is built,that is W0 =0.0613e-0.0001h .Distributive feature of wind pressure in Xinjiang is disclosed by prediction model and probability model. The results show that maximum wind speeds at most meteorological stations obey Γ-distribution and wind pressure coefficients decreased exponentially with height above sea level.Distributive features of wind pressure in Xinjiang are:wind pressures in north Xinjiang are bigger than those in south Xinjiang, wind pressures in west and east Xinjiang are bigger than those in middle Xinjiang; wind pressures in plateau and high mountain are bigger than those below middle mountain. Wind pressures in wind and valley of river are maximum. Distributive features of wind pressure in oil field of Talimu are that wind pressures are decline from northeast to southwest.These results are important to building design and other electricity and highway designs.

应用熵最大原理导出的概率模式研究了新疆建筑工程设计中最大风速的分布规律 ,并通过近100个气象观测站36年(1961~1996年)资料的分析 ,发现新疆最大风速若干规律性 ,在此基础上 ,建立了新疆风压系数预测模式为 :W。=0.0613e -0.0001h ,以预测模式和概率模式揭示了新疆风压分布特征。结果表明 :新疆大多数气象观测站的最大风速遵循Г分布 ;新疆风压系数随海拔高度的增加呈指数率减少 ;新疆风压分布特征为 :北疆大于南疆 ,西部、东部大于中部 ;高山和高原地区大于中低山区。风口、河谷风压值最大。塔里木油田地区风压特征为 :由东北向西南递减。这对于新疆建筑工程设计及相关的电力、公路等工程设计都具有重要的科学意义和使用价值。

The spatial and temporal distribution character of gale was analyzed using 39 years data from 1961 to 1999 at 90 weather stations in Xinjiang. The results are follow:(1)The gale occurrence is more frequently in north-western of North Xinjiang , East Xinjiang and west of South Xinjiang, most at Alashankou and Dabancheng, lest in the center of Zhunger Basin and the southern periphery of Tarim Basin. (2) The change of annual days of gale is variable obviously, decreases by degrees since...

The spatial and temporal distribution character of gale was analyzed using 39 years data from 1961 to 1999 at 90 weather stations in Xinjiang. The results are follow:(1)The gale occurrence is more frequently in north-western of North Xinjiang , East Xinjiang and west of South Xinjiang, most at Alashankou and Dabancheng, lest in the center of Zhunger Basin and the southern periphery of Tarim Basin. (2) The change of annual days of gale is variable obviously, decreases by degrees since 1980. (3) The gale mainly occurs in spring and summer, especially in May and June. The gale occurs more frequently from 10 to 23 o'clock, there are over half gale during 1.0 hour, most 0.5 hour.

统计了1961~1999年39a新疆90个气象观测站的气表—1资料,给出新疆大风的时空分布特征,结果表明:(1)年平均大风日数的高值区在北疆西北部、东疆和南疆西部,阿拉山口、达坂城大风最多,准噶尔盆地中心、塔里木盆地南缘最少。(2)大风年总日数的变化有明显的波动性,大部分地区80年代起大风日数有减少的趋势。(3)春、夏季大风最多,以5、6月最为频繁。大风主要出现在上午10时到午夜23时,半数以上的大风持续时间在1h以内,以.5h以内最多。

 
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