1) tendency rate
倾向率
1.
This article makes an analysis of the variation tendency of the hydrologicalelements of Nansi Lake in the past 40 years, using the tendency rate for quantitative description based on the date of measured rainfall, water gage of the lake calculated flow into the lake, available water, annual water consumptioh etc.
利用实测降水量、水位和计算出的入湖水量、可利用水量、年用水量等资料，分析南四湖近四十年中水文要素的变化趋势，并用倾向率作定量描述。
2.
With the methods of linear analysis and correlation analysis,the tendency rate of the ground temperature for about 50 years in Puyang and the causes are analyzed.
利用线性分析方法和相关分析方法,分析了濮阳近50年地面温度的变化倾向率及成因。
2) climate tendency rate
气候倾向率
1.
Based on the monthly mean air tempetature data of 29 stations in Hunan Province in the recent 40 years(in 1960-1999),and using the climate tendency coefficient,climate tendency rate,cumulative departure,power spectrum methods,the temporal-spatial change characteristis of air tempetature of interannual and four seasons over the region are analyzed.
利用湖南省29个站点1960～1999年的月气温资料,采用气候趋势系数、气候倾向率、累积距平、连续功率谱估计等方法,对湖南省年、季气温的时空变化特征进行了分析,结果表明:年、季气温的时空变化特征各不相同,冬季变暖,夏季降温,且气温空间变化受到地形的影响;年、季气温变化周期各不相同,年气温变化存在准22年的周期,与海尔周期相当一致。
2.
Based on the daily ground temperature data from 107 stations in the Yangtze River Basin from 1961 to 2000,characteristics of spatial-temporal variability of mean ground temperature in the Yangtze River Basin were investigated with the methods of calculating climate tendency rate and temperature changes per decade of mean ground temperature in Yangtze Basin.
选取长江流域107个测站1961～2000年逐日平均地温资料(0㎝),利用最小二乘法通过计算气候倾向率和年代际变化的方法,对长江流域年、季平均地温的时空分布和变化特征进行了研究。
3) linear trend
气候倾向率
1.
The variation trend,abrupt change and anomalous years of annual and seasonal mean soil temperatures at shallow layers in Lhasa were investigated during the period from 1961 to 2005 by using modern statistical diagnostic methods such as linear trend analysis,accumulated variance and signal noise ratio methods.
利用1961-2005年拉萨0～40cm各层逐月平均地温,采用气候倾向率、累积距平、信噪比等气候统计方法,研究了近45年拉萨浅层平均地温的变化趋势、气候突变和异常年份等。
2.
Using the data of monthly sunshine duration,mean cloudiness,surface vapor pressure and precipitation at 25 meteorological stations over Tibet from 1971 to 2005,the trend variation of the sunshine duration are analyzed by using linear trend analysis.
采用气候倾向率方法,对西藏25个站1971～2005年逐月日照时数以及对日照有影响的总云量、低云量、水汽压和降水量等资料进行了统计分析。
4) climatic trend rate
气候倾向率
1.
The climatic trend rate of annual precipitation was arising at 89.
1 932年～ 1 95 8年和 1 95 9年～ 2 0 0 0年年降水量的气候倾向率分别为 89。
5) temperature tendency
气温倾向率
6) slope values of solar radiation
太阳辐射倾向率
补充资料：电导率(见电阻率)
电导率(见电阻率)
conductivity
d!日nd日O}已电导率(eonduetivity)见电阻率。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条