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首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Estimation and Correction of Geolocation Errors in FengYun-3C Microwave Radiation Imager Data
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Estimation and Correction of Geolocation Errors in FengYun-3C Microwave Radiation Imager Data

机译:FengYun-3C微波辐射成像仪数据中地理位置误差的估计和校正

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摘要

Microwave Radiation Imager (MWRI) onboard the FengYun (FY)-3C satellite provides measurements of the Earth's atmosphere and surface at 10.65, 18.7, 23.8, 36.5, and 89.0 GHz with dual polarization. While FY MWRI data have been widely distributed to the user community, their geolocation accuracy has not been documented. In this paper, the coastline inflection method is used to estimate MWRI geolocation errors. Three coastal regions where MWRI brightness temperature exhibits a large contrast are selected for the geolocation analysis. A total of 720 MWRI data points are identified that cross the coastlines. The latitudes and longitudes at these data points are compared with the fine-resolution database of the Global Self-consistent, Hierarchical, High-resolution Shoreline (GSHHS). It is found that the mean geolocation errors in along- and cross-track directions are approximately 5–6 km at 89 GHz. This magnitude of errors is more than 30% of the field-of-view size at 89 GHz. Such a geolocation error must be corrected so that the MWRI data can be more useful for quantitative remote sensing. Thus, the mean geolocation errors are further utilized to adjust the satellite attitude angles (e.g., pitch, roll, and raw). After the attitude angle correction, the MWRI geolocation is very accurate at 89 GHz, and errors in other MWRI channels may be corrected through their co-registration relationships to the 89-GHz channel.
机译:风云(FY)-3C卫星上的微波辐射成像仪(MWRI)提供了双极化的10.65、18.7、23.8、36.5和89.0 GHz地球大气和地表的测量值。尽管FY MWRI数据已广泛分发给用户社区,但其地理位置准确性尚未得到记录。在本文中,使用海岸线变形方法来估算MWRI地理位置误差。 MWRI亮度温度表现出较大对比度的三个沿海地区被选择用于地理位置分析。总共确定了720个跨海岸线的MWRI数据点。将这些数据点的纬度和经度与全球自洽,分层,高分辨率海岸线(GSHHS)的高分辨率数据库进行比较。发现在89 GHz时,沿航迹方向和跨航迹方向的平均地理位置误差约为5–6 km。在89 GHz时,这种误差幅度超过了视野大小的30%。必须纠正这种地理位置错误,以便MWRI数据对于定量遥感更有用。因此,平均地理位置误差被进一步用于调整卫星姿态角(例如,俯仰,滚动和原始)。姿态角校正之后,MWRI的地理位置在89 GHz处非常准确,并且其他MWRI通道中的错误可以通过它们与89 GHz通道的共配准关系进行校正。

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