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1)  anomalous years
异常年份
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.
The variation trend,abrupt change and anomalous years of annual and seasonal mean soil temperatures at 0.
2m逐月平均地温资料,采用气候倾向率等现代统计诊断方法,研究了近35年西藏年、季平均地温的变化趋势、气候突变和异常年份
3.
The variation trend,anomalous years and abrupt change of annual and seasonal mean soil temperature at shallow layers during the period of 1962~2007 in Linfen were investigated by using modern statistical diagnostic methods such as linear trend analysis,the moving t-test method.
利用临汾1962年~2007年0 cm~20 cm各层逐月平均地温,采用气候倾向率、滑动t检验等气候统计方法,研究了近46年临汾浅层平均地温的变化趋势、异常年份和气候突变等。
2)  Interannual anomaly
年际异常
1.
Results show that the interannual anomaly of FCproduced nor.
结果表明,北半球夏半年FC的月平均海平面气压(SLP)年际异常较C的小,而全球或南半球FC与C的SLP无明显差别。
2.
Diagnosis is undertaken of the genesis and maintenance of interannual anomaly in summer monsoon with the aid of the departure vorticity equation in the context of 1980~1986 ECMWF 200hPa gridded u-and v-winds.
使用 ECMWF 200 hPa 1980~1986年格点资料(u,v),利用距平涡度方程对季风年际异常的形成和维持机制作了涡度收支方面的诊断。
3)  Anntal anomaly
年度异常
4)  The especially drought and flood years
旱涝异常年
5)  1997-1998 anomalous years
1997-1998异常年
6)  yearly dynamic anomaly
年动态异常
1.
The relationship between Helium′s yearly dynamic anomaly and earthquake;
氦的年动态异常与地震的关系
补充资料:年份
1.见"年分"。
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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