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climatic相关的网络例句

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The most serious desertification occurred in southeast of MuSu Desert,then appeared inferior degree in midst,north,south and east,anddegression degree in other directions.6.The changes of environment in Mu Su Desert in historical times havebeen controlled by climatic changes in temperature and drought-wetwithin hundreds or thousands years.At present,it came into being suchspatial structure and environmental characteristics fordesertification land because of being relative to other naturalgeographic characters and human activities.In all that,physiognomyand hiemal wind are the driving factors.The sandy matter in stratumis the physical fountain factor.The depravation of surface water inthis region is one of representations of environmental changes, meanwhile,it is also the factor which leads to the degradation ofvegetation and desertification.On the whole,human activity has actedupon these natural elements,becoming a dominant factor in the regionalenvironment changes since Ming and Qing dynasty.7.Influencing of human activities on the environment of Mu Su Deserthad occurred before Qin dynasty,and its intensity of earlier influencewas so slight that it could not cause a large scope and long timeenvironmental changes.

沙漠化的程度是东南部最强,中北部、南部和东部次之,而后向其他方向递减。6、毛乌素沙地历史时期的环境变化是受百年乃至千年尺度的气候冷暖、干湿变化控制的,之所以形成目前这样的沙漠化土地空间分布格局和环境特征,则与其地的自然地理特征和人类活动有密切关系,其中地貌及冬季风是动力因素;地层中的沙物质是物源因素;地表水环境恶化是区域环境变化的表现之一,同时又是植被退化和沙漠化的引致因素;人类活动总体上是叠加在自然因素之上的,只是明清以来在局地环境变化中成为主导因素。7、毛乌素沙地人类活动的环境影响在先秦时期就已出现,早期的影响程度是轻微的,不足以造成大范围、长时段的环境变化。

These are indications that the fauna Hipparion survive geological period, Linxia palaeogeomorphic Basin and climatic conditions have been the middle and lower reaches of the Yellow River region and differentiated.

上述迹象表明,在三趾马动物群生存的地质时期,临夏盆地的古地貌和气候条件已经和黄河中下游地区有所区别。

In addition, the two lithological strata containing fossils are differences in typical Baode the so-called "red Hipparion" climate temperature and humidity is a product of the period, and in the Linxia basin is close to a very sallow loess earthy heap, it may be reflected in a more dry and cold climatic conditions.

此外,两地含化石地层的岩性也有差异,在保德地区典型的所谓&三趾马红土&,是气候比较温湿时期的产物,而在临夏盆地则是一种很接近黄土的灰黄色土状堆积,它所反映的气候条件可能更为干冷。

The natural touring resources in Liangshan autonomous perfecture, such as geological and geomorphological, hydrographical, climatic and metorolgical, and ecological sceneries, engage people in cultural activities with their aesthetical feature.

凉山自然旅游资源如地质地貌景观、水文景观、气候气象景观、生态景观等以其美学特征引起人们文化活动,具有丰富的文化内涵。

In the qualitative and quantitative analyses, four kinds of methods such as cause analysis, vector statistics, fuzzy analysis and systematic cluster were synthesized and the applicability of them analyzed. Finally, in combination with the hydrometeorological characteristic of the north slope climatic zone of Tian Mountain and the operation of the reservoir, the flood season range are divided: 10 July 30 July flood season as main flood season and 1 August 15 August as later flood season. The result?

针对高山冰川作用下流域水库汛期分期的实际问题,以玛纳斯河流域夹河子水库为研究对象,识别汛期划分的主要影响因素,选择汛期划分依据,采用定性和定量分析相结合的方式,综合成因数理统计、矢量统计、模糊分析、系统聚类4种汛期分期方法,分析各种方法适用性,提取合理成分,结合天山北坡气候带的水文气象特征和水库控制运用特点,确定汛期范围:7月10日至7月30日为前汛期, 8月1日至8月15日为后汛期。

In this paper, the standard accelerated hygrothermal aging spectrum for military aircraft composite structures is given based on the domestic climatic environment and the developing aircraft properties, and the aging effects for our composite material system are systematically studied, and the conclusion for guiding and modifying the structure design are given.

本文根据我国气候环境和在研型号性能,编制了适用于军机复合材料结构的标准加速湿热老化谱,并系统研究了国产材料体系的老化效应,得出了指导和修改结构设计的有益结论。

Results showed diural variations of leaf Pn displayed bipeaked curve model, indicating the depression of photosynthesis at noon. Leaf Pn rate in June was higher than in September; Compared to leaf Pn, Cs had a similar changing curve, Cs in June was higher than in September. While diural variations of intercellular CO2 concentration were opposite to that of leaf Pn and Cs, decreased before 1200,increased after 1200, decreased again at 1600,after 1600 increased again; diural variations of climatic factors displayed single peaked curve model, peakedvalue occurred at 1400,and their influences on physiological factors were indirected and integrated.

结果表明,光合速率的日变化具有双峰型,存在光合午休现象,6月的光合速率高于9月;沙棘的气孔导度较低,其日变化与光合速率有相似的变化趋势,6月的气孔导度大于9月;细胞间CO2浓度的日变化与光合速率和气孔导度的日变化相反,1200之前下降,之后上升,1600下降,然后上升;气象因子的日变化具有单峰型,峰值1400出现,对生理因子的影响是间接且综合的。

First, on the base of Koppen Classification, the dissertation classifies the world climate into 13 types and analyzes the vernacular architecture and its climatic strategies corresponding to each type, especially how the buildings adapt to the local climate, make use of the native materials and adopt appropriate techniques under the condition of poor economy, low technology and limited resources and labor.

一、论文以柯本气候分类法为依据,将全球气候分成热带雨林气候等13种气候型,并针对每种气候型来分析与之对应的乡土建筑及气候策略,特别是对于经济、技术相对落后,人力、资源都很匮乏的条件下,建筑是如何适应当地气候、使用本土材料、采用适宜技术等方面进行了较为系统的总结。

The order of the effect of the climatic factors on the increment of Larix leptolepis was The precipitation of last summer, 10 cm groud temperature of Spring, the relative humidity from September to October in last year,≥10℃ accumulative air temperature ,10 cm groud temperature from September to October in last year, sunligh hours, relative moisruer of Februry, precipitation of November, the average temperature from April to May last year, the average temperature of last Winter.

按气象因子在回归方程中出现的次数频率将气象因子对日本落叶松生长量影响程度排序为:上年6~7月降水量、当年3~4月10cm地温、上年9~10月相对湿度、≥10℃积温、上年9~10月10cm地温、年光照时数、当年2月平均相对湿度、上年11月降水量、上年4~5月平均气温、上年11月~当年1月平均气温。

The order of the effect of the climatic factors on the increment of Larix leptolepis was the relative humidity from September to October in last year, precipitation of November, relative moistuer of Februry, The precipitation of last summer, sunligh hours, 10 cm groud temperature of Spring,≥10℃ accumulative air temperature, the average temperature from April to May last year, the average temperature of last Winter, 10 cm groud temperature from September to October in last year.

按最大关联度出现的次数频率将气象因子对日本落叶松生长量影响程度排序为:上年9~10月相对湿度、上年11月降水量、当年2月平均相对湿度、上年6~7月降水量、年光照时数、当年3~4月10cm地温、≥10℃积温、上年4~5月平均气温、上年11月~当年1月平均气温或、上年9~10月10cm地温。

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