...
首页> 外文期刊>Journal of atmospheric and oceanic technology >Four Years of TRMM/VIRS On-Orbit Calibrations and Characterization Using Lunar Models and Data from Terra/MODIS
【24h】

Four Years of TRMM/VIRS On-Orbit Calibrations and Characterization Using Lunar Models and Data from Terra/MODIS

机译:使用月球模型和Terra / MODIS数据对TRMM / VIRS进行四年的轨道定标和表征

获取原文
获取原文并翻译 | 示例
           

摘要

Four years of on-orbit solar calibration data have been used to quantify the temporal degradation of the two reflected solar bands of the Visible and Infrared Scanner (VIRS) aboard the Tropical Rainfall Measuring Mission (TRMM) satellite. Solar calibrations, performed using an onboard solar diffuser, show no significant changes in the VIRS 1.61-μm data. The responsivity (digital counts per radiance unit) of the 0.62-μm band has changed and, as a function of days since 1998, is given by R_1 (day) = 69.782 ― 0.0022 X day, with an annual degradation of 1.15%. Four years of on-orbit lunar measurements were also examined in an attempt to quantify any degradation in the solar diffuser. The integrated lunar reflectance with phase angles ranging from 1.6°to 106°were fit with the lunar photometric model of Hapke. A good fit was made to the 0.62-μm data, but overall, the quality of the data did not support efforts to quantify any diffuser degradation. The quality of the VIRS radiometry was also examined by comparing data from the five VIRS spectral bands with similar Terra/Moderate Resolution Imaging Spectroradiometer (MODIS) bands while viewing near-coincident nadir scenes. The median reflectance differences, VIRS ― MODIS, are ―1.4% and ―12.1% for the solar bands (VIRS 0.62 and 1.61 μm; MODIS 0.65 and 1.64 μm). The median brightness temperature differences for the thermal bands at 3.78, 10.83, and 12.03 μm, respectively, are ―0.53, 0.04, and ―0.76 K. These values compare well with the values from Minnis et al. The large difference in the 1.61-μm bands and day―night differences in the thermal emissive bands are discussed.
机译:四年的在轨太阳校准数据已用于量化热带雨量测量任务(TRMM)卫星上可见光和红外扫描仪(VIRS)的两个反射太阳波段的时间衰减。使用板载太阳能扩散器进行的太阳能校准未显示VIRS1.61-μm数据有明显变化。 0.62-μm波段的响应度(每辐射单位的数字计数)已经改变,并且,作为1998年以来天数的函数,R_1(天数)= 69.782〜0.0022 X天,年衰减为1.15%。还检查了四年的在轨月球测量,以试图量化太阳漫射器的任何退化。 Hapke的月球光度模型拟合了相角范围为1.6°至106°的综合月球反射率。 0.62μm数据非常合适,但总的来说,数据质量不支持量化扩散器退化的工作。在查看近乎一致的最低点场景时,还通过将五个VIRS光谱带的数据与相似的Terra /中等分辨率成像光谱仪(MODIS)进行比较,来检查VIRS辐射质量。太阳波段(VIRS 0.62和1.61μm; MODIS 0.65和1.64μm)的中值反射率差异VIRS ― MODIS为―1.4%和―12.1%。热带在3.78、10.83和12.03μm处的平均亮度温差分别为-0.53、0.04和-0.76K。这些值与Minnis等人的值相比较。讨论了1.61μm波段的巨大差异和热发射波段的昼夜差异。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号