magnitude of deviation 中文意思是什麼
magnitude of deviation
解釋
差異量-
Standard deviation in statistics, a measure of the dispersion of a frequency distribution : it is the average magnitude of deviations from the center of normal curve, calculated by squaring all the deviations, calculating their mean, then finding the square root of the mean
標準偏差：統計中，一種衡量數據組分佈的分散或變化情況的數據，是偏離正態分佈中間位置數據大小的平均值。 -
And more aperture extension is achieved in this novel esprit - based two - dimensional angle estimatio n scheme using a uniform rectangular array of vector hydrophones spaced much farther apart than a half - wavelength. this proposed scheme and the attendant vector - hydrophone array outperform a uniform half - wavelength spaced pressure hydrophone array with the same aperture and slightly greater number of component hydrophones by an order of magnitude in estimation standard deviation
結合實際的應用情況，對矢量水聽器構成的陣列進行了初步的探討，利用本文前面部分所分析的基於單矢量水聽器的方法，實現了陣元間距突破半波長上限的局限，並解決了角度估計的循環模糊問題，以較小的硬體代價和運算代價實現陣列孔徑的擴展，提高估計精度。 -
The examples in abroad and home indicate that the viscous remanent magnetization is a convenient tool for orientation determination of drilled cores. it can be used on samples for which the geological age is not known. the only information required is well position, the direction and magnitude of well deviation and the " right way up " for the core sample
結合國內外的研究實例和自己的研究實例，對利用粘滯剩磁確定巖心方向進行了較深入的研究，進一步證明了粘滯剩磁巖心定向是一種不用考慮復雜的地殼運動和地質年代，只需要井位的井斜數據和取心方向標記的簡單、方便值得推崇的方法。 -
But if there is a topographic heterogeneity, the maximum relative difference of surface grid effective infrared radiation is about 30 % ~ 40 %. the magnitude of deviation is mainly determined by grid average elevation
而當考慮海拔高度的非均勻性時，有效輻射通量計算的相對誤差可達30 40 ，取決于平均高度和變差系數大小。 -
But due to the limit of the observed data, the magnitude of deviation is ca n ' t calculated easily
但由於理論上的不成熟及實測資料的缺乏，實際情況有待于進一步的研究。 -
Using " identity " idea and anomaly criterion of slave function, remain curve and original curve deviation etc, a set of medium - term, short - term and imminent term anomaly of the moderately strong earthquakes, especially those with intensity v above magnitude 5 earthquakes are extracted
運用「同一化」思路、從屬函數、剩餘曲線及原始曲線均方差等異常判定方法，提取了中等以上地震，特別是5級以上地震的中、短、臨異常實例。
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