北极海冰密集度数据融合研究OA北大核心
A study of data fusion on Arctic sea ice concentration
海冰密集度数据是开展全球海洋监测和应对气候变化研究的重要数据源,为了研制出分辨率更高,误差更小的北极海冰密集度融合资料,本文使用了多源海冰密集度资料,以 OSTIA(Operational Sea Surface Temperature and Ice Analysis)数据集为融合背景场,采用以下方案开展融合研究.首先,对现有5种海冰资料进行质量控制;其次,以OSI SAF(Ocean and Sea Ice Satellite Application Facility)资料为基准,采用概率密度匹配法订正各资料的系统误差;然后,利用小波分解将各资料分解为低频信息和高频信息,对低频信息和高频信息分别计算融合权重和卡尔曼滤波处理;最后,利用小波重构将各资料进行融合,生成 0.05°分辨率的北极逐日海冰密集度融合资料.通过对比国际上广泛认可的 OISST(Optimum Interpolation Sea Surface Temperature)、OSTIA海冰密集度资料,验证结果显示:融合资料与OISST、OSTIA海冰密集度资料在北极的空间分布上高度一致,相关系数均超过 0.967.相对于前人的研究,本融合资料与 OISST 的偏差由-1.170%减少到-0.108%,与 OSTIA 的偏差由 0.276%减少到-0.156%;与OISST和OSTIA的均方根误差分别由9.835%减少为8.010%以及由7.427%减少为5.140%.本融合资料的偏差以及均方根误差都得到了显著的提升,具有较高的质量.
Sea ice concentration data are important for global ocean monitoring and climate-change-response re-search.To develop Arctic sea ice concentration fusion data with higher resolution and smaller errors,this study uses multisource sea ice concentration data,with Operational Sea Surface Temperature and Ice Analysis(OSTIA)data as the fusion background field.The following scheme is adopted to perform the fusion study.First,quality control of the existing five sea ice data is performed;second,the systematic error in each data is revised via the probability density matching method using the Ocean and Sea Ice Satellite Application Facility(OSI SAF)data as the bench-mark;thereafter,the data are decomposed into low-frequency and high-frequency information by means of wavelet decomposition,and fusion is calculated for both these types of information.Thereafter,wavelet decomposition is used to decompose the data into low-frequency information and high-frequency information,and the low-frequency information and high-frequency information are calculated and processed via Kalman filtering.Finally,wavelet reconstruction is employed to fuse the data to generate the fusion data of day-by-day Arctic sea ice density with a resolution of 0.05°.Upon comparing with the internationally recognized Optimum Interpolation Sea Surface Tem-perature(OISST)data and OSTIA sea ice density data,the validation results demonstrate that the fusion data,OISST sea surface temperature data,and OSTIA sea ice density data are highly consistent in the spatial distribution of the Arctic,with the correlation coefficients exceeding 0.967.Compared with previous research results,deviation of the fusion data from OISST data is reduced from-1.170%to-0.108%and that from OSTIA data is reduced from 0.276%to-0.156%;in addition,the root mean square error(RMSE)between the fusion data and OISST data is reduced from 9.835%to 8.010%and that between the fusion data and OSTIA data is reduced from 7.427%to 5.140%.The bias as well as RMSE of these fusion data has been significantly improved with high quality.
王安;何宜军;殷千惠
南京信息工程大学 电子与信息工程学院,江苏 南京 210044自然资源部空间海洋遥感与应用重点实验室,北京 100081||南京信息工程大学 海洋科学学院,江苏 南京 210044南京信息工程大学 海洋科学学院,江苏 南京 210044
海洋科学
海冰密集度小波变换卡尔曼滤波概率密度函数匹配法
sea ice concentrationwavelet transformKalman filteringprobability density function matching method
《海洋科学》 2025 (2)
25-33,9
国家重点研究与发展计划项目(2021YFC2803301)江苏省研究生研究与实践创新计划项目(Nos.KYCX23_1347)National Key Research and Development Program of China,No.2021YFC2803301Postgraduate Research&Practice Innovation Pro-gram of Jiangsu Province,No.KYCX23_1347
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