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1)  climatic hierarchy
气候层次
1.
After decreasing wavelet transformation s boundary effect, the prediction law and assessment standard are put up based on the theory of climatic hierarchy and wavelet analysis.
论述了子波气候诊断中的边界效应和非周期性对趋势预报的影响,在消除子波变换边界效应基础上,将气候层次理论和子波诊断技术相结合,提出了气候多层次趋势预报法则和评判标准,最后利用若干气候资料进行了多层次趋势预报。
2)  levels of climatic variation
气候变化层次
3)  climate sequence
气候层序
1.
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
研究结果表明,前陆盆地内发育有两种层序模式,即构造层序和气候层序。
2.
The model of the development of the climate sequence is put forward.
对存在于塔里木盆地志留-泥盆系台盆区的气候转变进行了深入分析,总结了气候在可容空间变化中的作用和以气候为主控因素的层序发育模式,提出了"气候层序发育模式",并且分析了气候层序发育过程中气候对层序发育的控制过程。
4)  climatic stratigraphy
气候地层
1.
Analyses of the two boreholes include OSL and U-series dating,pollen and microfossils,tending to reconstruct the high resolution climatic stratigraphy,and therefore to define the chronostratigraphy of the Late Quaternary.
根据对长江三角洲地区两个以细颗粒沉积为主的晚第四纪钻孔进行OSL测年、U系测年、孢粉分析和微体古生物分析,试图建立高分辨率气候地层,从而建立本区晚第四纪的年代地层框架,并探讨本区晚第四纪的标志层和期间发生的两次海侵及其机制。
2.
Based on this information,the lithostratigraphy,biostratigraphy and climatic stratigraphy since Late Pleistocene in the North China Plain had been further studied,the age borderline between Holocene and Pleistocene of the North China Plain had been determined.
在此基础上,对华北平原晚更新世以来的岩石地层、生物地层及气候地层进行了进一步的研究,厘定了华北平原全新世与晚更新世地层的年龄界线。
5)  climatolith
气候层
6)  climate influenced layer
气候影响层
1.
Initially, the paper determines that the thickness of climate influenced layer is 4m and that thickness of severe layer is 2.
结合南昆铁路膨胀性红土和膨胀泥岩两处路基工程试验,通过现场含水量测试,本文探讨了岩土含水量及其变幅随深度变化的规律,以及地温及其变幅与深度的关系,初步确定广西膨胀岩土的气候影响层厚度为4m、剧烈影响层厚度为2。
补充资料:东北平原农业气候资源利用(见农业气候资源利用)


东北平原农业气候资源利用(见农业气候资源利用)


  默军爵攫戳猛罚胃植和l用2 iyuanl心yong 见农业气候资
  
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