共振潮 的英文怎麼說
中文拼音 [gòngzhèncháo]
共振潮
英文
co oscillating tides-
The numerical results indicate that the deformation within the solid inner core is very small. however, in the fluid outer core, the changes of the displacement with relatively low spherical harmonic degree ( n < 10 ) is very complicated via the radius, due to the resonance near the eigenfrequenies of the core long - period oscillations. while the spherical harmonic degree of the loading is larger than 10, the deformation and the gravitational perturbation in the core are very small, and the earth ' s deformation response is dominantly represented as the radial displacement in the elastic mantle
研究了地球在日月引潮力和表面負荷作用下的形變特徵，數值計算結果表明，在固體內核中的形變很小，由於在長周期核模本徵頻率附近的共振，液核中低階（ n 10 ）位移隨半徑的變化非常復雜，當負荷階數超過10時，地核中的形變和擾動位都很小，地球的響應主要表現為彈性地幔中的徑向位移，且隨深度增加急劇減弱，地表負荷love數與信號頻率的依賴關系很弱，給出了體潮love數計算的一種有效的近似處理方案。4. the tidal gravity observations, recorded with a scg at wuhan, are employed to investigate the influences of the ocean tide loading on the fitted fcn parameters and the local characteristics of the nearly diurnal resonance on the tidal gravity observations. it is found that the influence of different co - tides on the fitted eigenperiod and the real part of the resonance strength of the fcn is very small
結果表明，不同海潮模型對擬合的fcn周期和共振強度實部影響甚微，差異主要表現在品質因子和共振強度虛部的擬合，通過不同海潮模型改正後重力潮汐觀測資料的迭積，可減小海潮模型不確定性的影響，獲得fcn共振參數。Fang, g., w. zheng, z. chen and j. wang, 1986. analysis and prediction of tides and tidal currents. china ocean press, beijing, 474pp
方國洪、鄭文振、陳宗鏞、王驥， 1986 .潮汐和潮流的分析和預報.海洋出版社.共474頁The quality factor is about 9543, which, compared with those determined based on the tidal gravity observations in the previous studies, more closes to those obtained by using the vlbi data. the complex resonance strength is ( - 6. 10x10 - 4, - 0. 01x10 - 4 )
以武漢臺超導重力儀觀測資料為例，研究了海潮負荷對fcn共振參數擬合的影響和重力潮汐觀測中近周日共振的區域性特徵。分享友人