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並列摘要


An attempt is made to prove the principal difference between the distribution law of wind power increments and the corresponding law of the wind speed increments. The distribution law of wind power increments is close to an asymmetric triangle in the medium range and with zero values at low and high average values of the wind speed. The wind power increments found by the selected increment method are much more frequent than those determined by the simple increment method. The theoretical functional relations were proved, based on the real recorded wind power data.

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