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  climatic type
Climatic type I, hyperthermal throughout the year, occurs in the tropics south of latitude 20° N.
      
Climatic type II, hyperthermal in the hottest month and comfortable in the coldest month, extends over latitudes from 20° to 30° N except in the highlands.
      
Climatic type III, hyperthermal in the hottest month and hypothermal in the coldest month, encompasses temperate zones of East Asia and subtropical arid areas of northwestern India.
      
Climatic type V, comfortable in the hottest month and hypothermal in coldest month, occurs near the southeast coast of the Soviet Union and in the highlands of the Himalayas.
      
Few climatic type of karstification may produce patterns different from those above.
      
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  climate type
However, it is found that the tropical climate type occupies only a peripheral part of southern China, though it firmly represents a distinctive type of climate that is subsequently associated with a great economic importance for China.
      
As such, the tropical climate type was mostly identified with its agro-climatological significance, that is by giving favourable growing conditions all-year round for perennial crops with a great heat demand.
      
Relevance of individual characteristics for human heat stress response is dependent on exercise intensity and climate type
      
Professionalism was the most reported and efficiency was the least reported ethical climate type in the organization.
      
A survey of managerial employees in Russia (n = 136) indicates that "rules" was the most reported and "independence" was the least reported ethical climate type.
      
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  climatic patterns
In addition, a shift of the climatic patterns in the form of larger area falling under the influence of rains was observed.
      
Late-glacial vegetational ecotones and climatic patterns in Western Norway
      
Climatic patterns and the distribution of C4 grasses in North America
      
We conclude that local responses of wildlife populations to changing climate may not be adequately explained by models that project large-scale climatic patterns.
      
Broader-scale climatic patterns were more important for the other two species.
      
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The Hengduan Mountain area Lies in Southwest China, including Parts of East Tibet, West Sichuan and Northwest Yunnan, and has a varied topogra-phy.The average altitude of it is over 3,000m a.s.l, The climatic change during Historical Time in this area has not been studied because of the lack of data.By field investigation, the authors have got a large quantity of tree ring specimens in the area. After preliminary dating and necessary dendrochro-nological processing, twelve standardized deadrochronologies have...

The Hengduan Mountain area Lies in Southwest China, including Parts of East Tibet, West Sichuan and Northwest Yunnan, and has a varied topogra-phy.The average altitude of it is over 3,000m a.s.l, The climatic change during Historical Time in this area has not been studied because of the lack of data.By field investigation, the authors have got a large quantity of tree ring specimens in the area. After preliminary dating and necessary dendrochro-nological processing, twelve standardized deadrochronologies have been built Baaed on these chronologies, two curves including the fluctuations of the air temperature and the annual precipitation during the last hundreds of years in the mountain area were drawn,Some significant cold/warm and dry/wet periods could be divided also.A combined analysis between dendrochronologies and historical literature data which have five classes could help us to understand the successive variations of each climatic pattern since 1600 A.D. In addition the amplitude and periodicity of climatic change in the area have been calculated in this paper.It is obvious that the chief characteristies oi the modern climatic change in Kengduan Mountains might be concluded as follows.1)The temperature fluctuation during the last four hundred years in the area is similar to that in Tibetan Plateau, and the coldest period occurred in the first half of the 17th century.2)The long-term oscillation of precipitation is more obvious than that of air temperature.3) The statistical feature in the present century is, on the average ,lower temperature and lower precipitation, but the climate pattern with high temperature and low precipitation has been increasing since 1950's,4)The amplitude of climatic variation in the area is smaller than tha t in Tibet or in the plain area located on the east of Tibet Plateau.5)By carrying out analysis on various series, some periodicities have been found, such as ''quasi two year pulse'' , s. 6 years, 35 years and so on.

横断山地处我国西南的藏东、川西和滇西北一带,境内地形复杂,平均海拔在3000米以上。长期以来,由于资料短缺,对该地区历史时期气候变化研究甚少。经实地考察,作者获取若干树木年轮标本,辅以其它类型资料,对该地区最近数百年来的温度、降水变化及气候类型演替,予以初步分析。并论及气候变化的振幅与周期性。

In year, The observation of 10 sorts of corn hybrids with different maturing dates called early, medium and late corns and with their different leaf angles such as erectophile and planophile have been taken in Beijing, Yanqing County (Beijing area), Taian (Shandong Province) , GongZhuling (Jilin Province) and Shihezi(Xinjiang Aitononous Region), Based on the data obtained from the observations,a normal growing function was derived on the princplie laws of th accumulated dry matterW=(1 + e8.56-13.52)-1In accordance...

In year, The observation of 10 sorts of corn hybrids with different maturing dates called early, medium and late corns and with their different leaf angles such as erectophile and planophile have been taken in Beijing, Yanqing County (Beijing area), Taian (Shandong Province) , GongZhuling (Jilin Province) and Shihezi(Xinjiang Aitononous Region), Based on the data obtained from the observations,a normal growing function was derived on the princplie laws of th accumulated dry matterW=(1 + e8.56-13.52)-1In accordance with the function, the authors built up a model of the potentiol maximum biomass dependent on the accumulated temperature. Bmax/kg·mu-1= 100+1.11∑Tm. The model was applied to estimate the potential corn yield of the hybrids different maturing and the results in assessing the impact of climatic change are discussed.

依据于物质积累的基本规律,用包括早、中、晚熟和紧凑、平展两类株型的10个玉米杂交种在北京、延庆、泰安、公主岭、石河子5个不同气候类型地区的试验观察数据,模拟出玉米的标准生长函数W=[1+e~(3.56-13.52μ)]~(-1)。据此建立潜在生物量与品种所需积温的关系:B_(max)/kg·亩~(-1) =100+1.1∑T_m。用此模式估算了不同熟性品种的潜在产量,讨论了模拟结果在气候变化影响评价中的应用。

Agricultural climatic region in the river valley area in Tibet was classified into 5 patterns on the basis of 11 climatic factors which affected the crop growth, systematic collection and analysis of about 20-year climatic references from 16 wheather stations with the methods of Ward's,Centroid,Group average linkage and Flexible group average linkage. Also the classification results were discussed.

选用11个影响作物生长发育的气候因子,利用16个气象台站约20年的平均气象资料,分别采用华德法、重心法、类平均法和可变类平均法进行系统聚类,将西藏河谷地区农业气候区分为5个农业气候类型,并对其区划结果进行了讨论。

 
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