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寒冷期的英文

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"寒冷期"怎么读用"寒冷期"造句

英文翻译手机手机版

  • algid stage
  • cold period

例句与用法

  • Cold times in the north typically brought drought to saharan africa and india
    北方的寒冷期通常会为非洲的撒哈拉地区及印度带来乾旱。
  • The climate , which had changed in huizong and qinzong periods , is changing dramatically into a new cold stage in this district
    建中靖国元年前后,该地气候突然发生明显变化而进入了新的寒冷期
  • At that time , the climate alternated between warm stage and cold stage , including several alternative short periods
    其间尽管这里的气候在徽宗、钦宗年间曾出现过由温暖期向寒冷期的突变,但总体上是一个渐进的变化过程。
  • However , the changing period of the third cold stage , which is explained that existed in the early period of the song dynasty according to zhu kezhen , does happen in the period of huizong monarch
    其转变为第三个寒冷期的时间不是如近几十年来学者们承竺可桢所说的北宋前期,而是在北宋后期的徽宗初年。
  • The dry / wet changes of surrounding area of bohai sea during past 500 years are divided into 7 stages , based on dry / wet indexes ( d / w ) of this area from 1470 to 1985 then , the changes of dry / wet spatial types ( d / wst ) and its related dry / wet regional different iation ( d / wrd ) features among different stages are analyzed . the results show that there are 4 main kinds of d / wst in this area , whose notability and spatial distribution features in different stages are apparently different , which reflects , very well , the changing process of the d / wrd of this region in past500 years . further analysis also presents that , in warmer period , the d / wst and the d / wrd patterns are relatively unsteady , meanwhile , the dry / wet changing difference among different parts of the region is relatively great , but , in colder period , it is just on the contrary . however , in the most severely cold period of the little ice age , t he area ' s d / wst and the d / wrd pattern sareveryu nsteady , and its d / wrd extenti salsot he high estin the whole past 500 years
    用研究区1470 1985年的旱涝等级资料,划分了该地区500年来旱涝变化的7个阶段,讨论了不同阶段间旱涝型的变化及其旱涝区域分异意义,结果表明, 500年来研究区有4类主要旱涝型,各型旱涝在不同阶段的重要程度及场型特征均有较大差异,深刻反映了该地区500年来旱涝区域分异特征的变化,通过对500年来旱涝变化与温度变化的对比发现,较温暖期,研究区的旱涝型及旱涝区域分异格局较多变,旱涝变化的区域差异性较大,较寒冷期,旱涝型及区域分异格局较稳定,旱涝变化的区域差异性较小,而在小冰期最寒冷阶段,旱涝型及旱涝区域分异格局的变动十分频繁,旱涝变化的区域差异性亦最大
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