Deep space observations of conditionally averaged global reflectance patterns

Alexander Kostinski, A. Marshak, T. Várnai
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Abstract

The Deep Space Climate Observatory (DSCOVR) spacecraft drifts about the Lagrangian point ≈ 1.4 − 1.6 × 106 km from Earth, where its Earth Polychromatic Imaging Camera (EPIC) observes the entire sunlit face of Earth every 1–2 h. In an attempt to detect “signals,” i.e., longer-term changes and semi-permanent features such as the ever-present ocean glitter, while suppressing geographic “noise,” in this study, we introduce temporally and conditionally averaged reflectance images, performed on a fixed grid of pixels and uniquely suited to the DSCOVR/EPIC observational circumstances. The resulting images (maps), averaged in time over months and conditioned on surface/cover type such as land, ocean, or clouds, show seasonal dependence literally at a glance, e.g., by an apparent extent of polar caps. Clear ocean-only aggregate maps feature central patches of ocean glitter, linking directly to surface roughness and, thereby, global winds. When combined with clouds, these blue planet “moving average” maps also serve as diagnostic tools for cloud retrieval algorithms. Land-only images convey the prominence of Earth’s deserts and the variable opacity of the atmosphere at different wavelengths. Insights into climate science and diagnostic and educational tools are likely to emerge from such average reflectance maps.
对条件平均全球反射模式的深空观测
深空气候观测站(DSCOVR)航天器在距离地球 ≈ 1.4 - 1.6 × 106 km 的拉格朗日点附近漂移,其地球多色成像相机(EPIC)每隔 1-2 h 对地球的整个日照面进行观测、为了探测 "信号",即较长期的变化和半永久性特征(如无处不在的海洋闪光),同时抑制地理 "噪声",在本研究中,我们引入了时间和条件平均反射率图像,在固定的像素网格上进行,非常适合 DSCOVR/EPIC 的观测环境。由此产生的图像(地图)按月进行时间平均,并以陆地、海洋或云层等表面/覆盖类型为条件,一目了然地显示出季节相关性,如极地帽的明显范围。清晰的纯海洋集合图显示了海洋闪烁的中心斑块,与地表粗糙度直接相关,进而与全球风向相关。当与云层结合时,这些蓝色星球 "移动平均 "图还可作为云层检索算法的诊断工具。纯陆地图像可显示地球沙漠的显著位置,以及不同波长下大气的不透明度。这种平均反射率地图很可能会为气候科学以及诊断和教育工具提供启示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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