temperature anomaly field 气温距平场
high anomaly field 高度距平
geochemical anomaly field 地球化学异常场
sst anomaly field 海温距平场
height anomaly field 高度距平场
gravity anomaly field 重力异常场
climate anomaly field 气候异常态场
Regional anomaly field 区域异常场
Thus anomaly field may be calculated by means of accumulational charge.
这样,异常场便可借助于积累电荷来计算。
In addition, there were different characteristics in height anomaly field.
另外,高度距平场也有不同特征。
Results show that the climate and anomaly field of monthly mean temperature is characterized by low-order.
分析揭示了月平均温度气候及其异常场集具有低阶、低维的特征。
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