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1)  Droughts/floods climate change
旱涝气候变化
2)  climatological system
旱涝气候
1.
Based on the theory of chaotic dynamics for nonlinear systems,and according to the yearly drought and flood level data within 1624 a(from 380~2003) in Xi’an area,a study on the chaotic characteristics and the predictability of the climatological system were investigated by calculating the associated dimension,Kolmogorov entropy and Lyapunov index of climatological attractor.
根据西安地区旱涝气候等级近1 624 a(380~2003年)资料序列,运用非线性系统混沌动力学理论,通过计算气候吸引子的关联维数、Kolmogorov熵和Lyapunov指数,对西安区域旱涝气候的混沌特性和可预报性进行研究。
3)  changes of the dryness and wetness
旱涝变化
1.
From the analyses,we can draw some conclusions as follows:(1)There existed some primary periods in the changes of the dryness and wetness in Guangdong from the viewpoint of the historical course,such as 7 years,15 years and 23 years and so on.
分析认为,从历史时期来看,广东的旱涝变化主要存在准7年、15年、23年左右的准周期,不同的历史时期主要影响周期不尽相同。
4)  drought and flooding disasters
旱涝气候灾害
1.
The characteristics of the interdecadal variations of drought and flooding disasters in China are analyzed by using the observed data.
作者还从东亚气候系统的年代际变化系统地分析了发生在我国旱涝气候灾害年代际变化的机理。
5)  Oscilations of flood/drought climate
旱涝气候准周期
6)  arid climate change
干旱气候变化
1.
Study on influence of arid climate change to drought disaster in Gansu and technique of preventing drought and reducing disaster;
干旱气候变化对甘肃省干旱灾害的影响及防旱减灾技术的研究
2.
It is found that the main features of arid climate change is that precipitation decreased obviously in the 1990s and aridity took place in the north,mainly in Hebei,Shanxi,Shandong provinces and the east part of Northwest.
通过分析中国北方50 a来的降水资料,结果表明:干旱气候变化的主要特征表现在20世纪90年代夏季降水量有明显的减少趋势,干旱化趋势主要发生在北方,主要包括河北、山西、山东和西北地区东部。
补充资料:一涝
1.犹言一并;全部。
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