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1)  Climatic ensure rate
气候保证率
2)  climate verification and examination
气候论证
1.
This paper introduces the main content and the technical method of climate verification and examination according to the practical work experience,and provides the references for speeding up the steps of climate verification and examination in Guangxi and improving the quality of climate verification and examination.
气候论证是《中华人民共和国气象法》赋予气象部门的职责。
3)  climate protection
气候保护
1.
Economic effect analysis of climate protection policy based on increasing carbon sink.;
增汇型气候保护的经济影响模拟分析
2.
This paper supplements the literature about the effects of reducing carbon dioxide emission in an attempt to simulate the international GDP spillovers as a result of climate protection policy.
基于气候保护模型(State-contingent模型与Demeter模型)和GDP溢出模型(Mundell-Fleming模型),对中美两国在实施控制性气候保护措施之后所导致的GDP溢出影响的变化进行了模拟分析。
3.
Two macro model systems were adopted,which are the decision support system of climate protection in China and the Computable General Equilibrium(CGE) model of Chinese economy.
系统地给出了中国实施增汇型CO2减排政策对宏观经济影响的模拟结果,所采用的模拟系统包括基于Pizer,Demeter,Zwaan工作发展的中国气候保护决策支持系统和中国经济可计算一般均衡(CGE)系统。
4)  climate probability
气候概率
1.
This paper describes the splendid prospect of the sunrise on Taishan Mountain, and according to the meteorological conditions and climate probability of the sunrise on Taishan Mountain, points out the best occasion for enjoying the sight of the sunrise on Taishan Mountain.
描述了泰山日出的壮丽景观,根据泰山日出的气象条件及气候概率,指出了泰山日出的最佳观赏时机。
5)  climatic variability
气候变率
6)  Climate variability
气候变率
1.
Significant progress has been made in studies on climate variability at millennial time scales during the last quarter of the 20th century.
2 0世纪后期 ,千年 (ka)尺度气候变率的研究取得了重要的进展 ,这表现在以下几个方面 :(1)格陵兰冰芯及深海沉积证明 ,在末次冰期中普遍存在平均周期为 1 5ka的循环 ,有人认为全新世也存在这种循环 ,小冰期就是最近一个循环的冷期。
2.
A study is undertaken of the climate base state of the northern winter sea level pressure (SLP) and its climate variability and temporal evolution, indicating that the base state has its high-val- ue region of means quare deviation in the Aleutian low, the northwest part of the Iceland s low and the Siberian high.
研究了近100多年冬季北半球海平面气压场的气候基本态、气候变率的特征及时间演变规律。
3.
We focus mainly on climate variability of the both thermodynamic and dynamic necessary conditions which influence TC formation in response to global warming.
主要研究结果如下:首先,研究过去60(1949-2008)年热带北太平洋TC生成的主要初始起源地-大尺度ITCZ(Intertropical Convergence Zone)的气候变率,利用NCEP再分析资料的分析研究发现,依照信风辐合类型和地理位置,北太平洋ITCZ清楚地分成三段,即1)位于西北太平洋100-140°E,10-20°N附近的季风辐合带(简称ITCZ-Ⅰ);2)位于140°E-140。
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
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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