| Jiang Mingshun,Fang Xinhua.The multifractal characters of temperature finestructures in the equatorial western Pacific Ocean[J].Acta Oceanologica Sinica,1999,(3):293-310 |
| The multifractal characters of temperature finestructures in the equatorial western Pacific Ocean |
| The multifractal characters of temperature finestructures in the equatorial western Pacific Ocean |
| 投稿时间：1998-07-28 修订日期：1998-12-30 |
| DOI： |
| 中文关键词: Multifractal characters ocean finestructures equatorial western Pacific Ocean |
| 英文关键词:Multifractal characters ocean finestructures equatorial western Pacific Ocean |
| 基金项目:The study was supported by the National Natural Science Foundation of China under contracts No. 49376257, No. 4950/6071 and No. 49676275, and the Research Fund for Doctorial Program of Higher Education under contracts No. 9542309 and No.98042306. |
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| 中文摘要: |
| By using part of CTD data collected at 2°S,155°E during the fall cruise of TOGA project in 1992,the multifractal characters of temperature finestructures are investigated.The absolute temperature gradients are supposed to be multifractal and their moments are computed by conventional box-counting method.It is found that these momeets have power dependence on the box size.This power dependence has two different scaling regimes,called S regime and I-regime respectively,with different scaling exponents.This is consistent with the combined effects of internal waves and mixing.Accordingly,the generalized fractal dimensions (Renyi dimension) of temperature gradients are derived.A nonlinear curve of the scaling exponents suggest a possible multifractal apptnach of the temperature shear.In fact,both regimes can be approximated by Besicovitch-Cantor model,respectively,by suitably chosen model parameters.A phenomenological model is developed on the basis of this two-regime mechanism.The model is compared with field data and Qood agreement is achieved. |
| 英文摘要: |
| By using part of CTD data collected at 2°S,155°E during the fall cruise of TOGA project in 1992,the multifractal characters of temperature finestructures are investigated.The absolute temperature gradients are supposed to be multifractal and their moments are computed by conventional box-counting method.It is found that these momeets have power dependence on the box size.This power dependence has two different scaling regimes,called S regime and I-regime respectively,with different scaling exponents.This is consistent with the combined effects of internal waves and mixing.Accordingly,the generalized fractal dimensions (Renyi dimension) of temperature gradients are derived.A nonlinear curve of the scaling exponents suggest a possible multifractal apptnach of the temperature shear.In fact,both regimes can be approximated by Besicovitch-Cantor model,respectively,by suitably chosen model parameters.A phenomenological model is developed on the basis of this two-regime mechanism.The model is compared with field data and Qood agreement is achieved. |
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