| Wu Longye,Wu Yongsen,Sun Yuxing,Wang Zhenxian.Remote sensing studies in the Haikou Bay Calculation of the deposition parameters[J].Acta Oceanologica Sinica,1998,(3):321-326 |
| Remote sensing studies in the Haikou Bay Calculation of the deposition parameters |
| Remote sensing studies in the Haikou Bay Calculation of the deposition parameters |
| 投稿时间：1997-08-31 修订日期：1997-09-15 |
| DOI： |
| 中文关键词: Deposition parameter remote sensing information model |
| 英文关键词:Deposition parameter remote sensing information model |
| 基金项目: |
| 作者 | 单位 | | Wu Longye | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Wu Yongsen | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Sun Yuxing | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Wang Zhenxian | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
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| 中文摘要: |
| By making use of the distinguishing features of repetitive imagery of the same area by sateVite remote sensing, a method of extracting water areas at different tidal levels from the images of bays at different times was adopted to establish a calculating model for tidal surface and a method of finding a sum by layers was used to establish a calculating model for the deposition parameter.Moreover, by making use of the calculating models for the deposition parameter and for tidal level, the deposition parameter for the sea area less than 0 m was calculated for the Haikou Bay at two different periods of time:during the period of 1965-1984 the total amount of deposits was 4.8×106 m3, and the sedimentation rate was 2.5×105 m3/a:during the period from 1984 to 1990, the total amount of deposits was -8.9×105 m3 and the sedimentation rate was -1.5×105 m3/a. |
| 英文摘要: |
| By making use of the distinguishing features of repetitive imagery of the same area by sateVite remote sensing, a method of extracting water areas at different tidal levels from the images of bays at different times was adopted to establish a calculating model for tidal surface and a method of finding a sum by layers was used to establish a calculating model for the deposition parameter.Moreover, by making use of the calculating models for the deposition parameter and for tidal level, the deposition parameter for the sea area less than 0 m was calculated for the Haikou Bay at two different periods of time:during the period of 1965-1984 the total amount of deposits was 4.8×106 m3, and the sedimentation rate was 2.5×105 m3/a:during the period from 1984 to 1990, the total amount of deposits was -8.9×105 m3 and the sedimentation rate was -1.5×105 m3/a. |
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