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一种改进的尺度因子算法用于GRACE/GRACE-FO时变重力信号恢复
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作者 陈威 钟敏 +2 位作者 C.K.Shum 李权国 段淑娟 《地球物理学报》 北大核心 2025年第5期1633-1646,共14页
准确恢复GRACE(Gravity Recovery and Climate Experiment)及其后续任务GRACE-FO(GRACE Follow-On)卫星观测的时变重力信号,对于揭示全球陆地海洋水量交换过程、监测区域水量收支平衡及预测局部旱涝灾害等具有重要科学意义.尺度因子法... 准确恢复GRACE(Gravity Recovery and Climate Experiment)及其后续任务GRACE-FO(GRACE Follow-On)卫星观测的时变重力信号,对于揭示全球陆地海洋水量交换过程、监测区域水量收支平衡及预测局部旱涝灾害等具有重要科学意义.尺度因子法作为恢复GRACE/GRACE-FO卫星观测信号中真实陆地水储量变化的一种常用手段,存在以下缺陷:不同水文模型推导出的尺度因子存在较大差异,缺乏一致性;即便在统一滤波处理条件下,传统方法往往未充分考虑GRACE/GRACE-FO数据中“条带”误差和高频信号的影响;滤波强度的选择具有主观性,难以保证恢复结果的最优性与稳定性.针对这些问题,我们提出了改进的尺度因子算法,主要包括:(1)引入贝叶斯三角帽方法,对多套水文模型加权融合,构建统一的融合后水文数据集,增强尺度因子的鲁棒性;(2)在水文模型滤波过程中考虑“条带”误差和高频信号的影响,提升滤波后信号的保真度;(3)引入评价性指标体系,从DDK1—DDK7滤波范围中确定了DDK4为最佳滤波方案,并基于迭代思想构建了改进尺度因子.改进尺度因子恢复的陆地水储量变化与CSR Mascon、JPL Mascon的结果吻合较好,相关系数分别为0.984和0.970,均方根误差分别为2.13 mm和3.54 mm.在线性趋势、周年振幅及相位值的时空分布上,改进尺度因子恢复的陆地水储量变化与CSR Mascon、JPL Mascon的结果基本一致. 展开更多
关键词 尺度因子 GRACE/GRACE-FO 陆地水储量 贝叶斯三角帽方法(BTCH)
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贝叶斯三角帽法的GRACE/GRACE-FO组合模型及其不确定性 被引量:1
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作者 黄飞龙 谷延超 +3 位作者 何祖建 黄俊 袁洪波 高崇钦 《大地测量与地球动力学》 CSCD 北大核心 2024年第4期417-422,共6页
利用贝叶斯三角帽法将多个GRACE/GRACE-FO重构模型进行融合,提升基于深度学习的地表质量变化重构模型的精度,为高精度填补及重构GRACE/GRACE-FO数据提供参考。实验表明,组合模型估算的全球陆地水储量变化的不确定性最低,其结果在多数流... 利用贝叶斯三角帽法将多个GRACE/GRACE-FO重构模型进行融合,提升基于深度学习的地表质量变化重构模型的精度,为高精度填补及重构GRACE/GRACE-FO数据提供参考。实验表明,组合模型估算的全球陆地水储量变化的不确定性最低,其结果在多数流域与参考模型的一致性更佳;较最优的重构模型,组合模型全球及流域的不确定性降低约15%,纳什效率系数(NSE)提升约5%,尤其在半干旱、半湿润及湿润区域,其精度提升更明显。 展开更多
关键词 GRACE/GRACE-FO 地表质量变化模型 模型组合 贝叶斯三角帽法
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A Thorough Evaluation of the Passive Microwave Radiometer Measurements onboard Three Fengyun-3 Satellites 被引量:3
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作者 Xinran XIA Wenying HE +4 位作者 Shengli WU Disong FU Wei SHAO Peng ZHANG Xiangao XIA 《Journal of Meteorological Research》 SCIE CSCD 2023年第4期573-588,共16页
Microwave Radiometer Imager(MWRI) is a key payload of China’s second generation polar meteorological satellite, i.e., Fengyun-3 series(FY-3). Up to now, 5 satellites including FY-3A(2008), FY-3B(2010), FY-3C(2013), F... Microwave Radiometer Imager(MWRI) is a key payload of China’s second generation polar meteorological satellite, i.e., Fengyun-3 series(FY-3). Up to now, 5 satellites including FY-3A(2008), FY-3B(2010), FY-3C(2013), FY-3D(2018), and FY-3E(2021) have been launched successfully to provide multiwavelength, all-weather, and global data for decades. Much progress has been made on the calibration of MWRI and a recalibrated MWRI brightness temperature(BT) product(V2) was recently released. This study thoroughly evaluates the accuracy of this new product from FY-3B, 3C, and 3D by using the simultaneous collocated Global Precipitation Measurement(GPM)Microwave Imager(GMI) measurements as a reference. The results show that the mean biases(MBEs) of the BT between MWRI and GMI are generally less than 0.5 K and the root mean squares(RMSs) between them are less than1.5 K. The previous notable ascending and descending difference of the MWRI has disappeared. This indicates that the new MWRI recalibration procedure is very effective in removing potential errors associated with the emission of the hot-load reflector. Analysis of the dependence of MBE on the latitude and earth scene temperature shows that MBE decreases with decreasing latitude over ocean. Furthermore, MBE over ocean decreases linearly with increasing scene temperature for almost all channels, whereas this does not occur over land. A linear regression fitting is then used to modify MWRI, which can reduce the MBE over ocean to be within 0.2 K. The standard deviation of error of GMI, FY-3B, and FY-3D MWRI BT data derived by using the three-cornered hat method(TCH) shows that GMI has the best overall performance over ocean except at 10.65 GHz where its standard deviation of error is slightly larger than that of FY-3D. Over land, the standard deviation of error of FY-3D is the lowest at almost all channels except at 89V. MWRI onboard FY-3 series satellites would serve as an important passive microwave radiometer member of the constellation to monitor key surface and atmospheric properties. 展开更多
关键词 Microwave Radiometer Imager(MWRI) Global Precipitation Measurement(GPM)Microwave Imager(GMI) brightness temperature(BT) the three-cornered hat method(TCH)
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