The weather in siberia is typically continental . 西伯利亚的气候是典型的大陆性气候。
In the east, they have a dry continental climate with severe winters . 他们东边是干燥的大陆性气候,冬季严寒。
The altitude of most area is over 1200m 属于暖温带大陆性气候,一年四季分明。
There is a continental climate in that place 在那个地方是大陆性气候。
Zhengzhou has a temperate and monsoonal climate with four clearly distinct seasons 郑州地区属暖温带大陆性气候,四季分明
The country has a continental type of climate characterized by extreme temperatures , irregular rainfall and low relative humidity 巴基斯坦为大陆性气候,其特点是温度极冷极热、降雨变化剧烈和相对湿度较低。
Areas that are well protected from the ocean experience a more continental type of climate with warmer summers , colder winters , greater daily and seasonal tempe - rature ranges , and generally lower relative humidity 种植区域逐渐由海洋性气候变为大陆性气候,夏天炎热,冬季寒冷,每日和季节性的温差较大,并且湿度相对较低。
Sichuan is one of the agricultural province , locates in the area between the continental climate and oceanic climate , the distribution of precipitation is always disproportional due to the influence of atmosphere circumfluence , the existence of drought and floodwater plus water pollution have produced huge menace to agriculture , water resources utilization , soil erosion and even the life and properties of human being 解决水资源的诸多问题,是摆在全党、全社会和全国人民面前一项刻不容缓的重大战略任务。四川作为贫水国的一个农业大省,由于地处海洋性气候与大陆性气候交接地带,受大气环流影响,降水时空分布不均,水旱灾害极为频繁,尤其是干旱对农业生产的威胁最大。
( 2 ) parts of the area show apparent local climatic properties because of the influence of topography , landcover , and so on . precipitation in mountainous and forest area is usually more affluent than in vicinity , this creates a typical mosaic structure of precipitation distribution like the islands . ( 3 ) soil water is the most significant form of water resources , which is the only water for vegetation uptake 分析结果显示: ( 1 )黄土高原地区的降水分布自东向西、自南向北逐渐减少,东南部可达900多毫米,西北部最低则仅约100毫米,表现出显著的大陆性气候特征; ( 2 )由于地形等因素的影响,山地森林等局部地区小气候特征明显,降水量高于周围地区,结果形成降水的岛状镶嵌结构; ( 3 )土壤水是黄土高原最重要的水资源之一,它是该区植被水分利用的重要资源。
The temperature of upper reach is higher than that of lower reach , therefore , the river freezes up from lower reach to upper reach and breaks up from upper reach to lower reach . secondly , inner mongolia reach lies in inland area . it is far from ocean and controlled by mongolia high - pressure 其次,内蒙段处于内陆地带,离海洋距离远,暖湿气流难以到达,常为蒙古高压控制,呈典型的大陆性气候,年降水量少,夏季盛热短暂,冬季严寒漫长,河流结冰期长达4 - 5个月,大部分为稳定封冻河段。