埃奥卢斯紫外线表面的高灵敏度恢复到表面反射率
L D Labzovskii1, G J van Zadelhoff2, L G Tilstra2
1R&D Satellite and Observations Group, Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands. lev.labzovskii@knmi.nl.
Scientific reports
|October 16, 2023
概括
使用Aeolus激光雷达表面回报 (LSR) 的主动遥感现在可以在全球范围内检索单向紫外线表面反射率. 这种方法有效地检测到土地和雪地覆盖的变化,即使在夜间.
科学领域:
- 地球和太空科学 地球和太空科学
- 大气科学 大气科学
- 遥感 遥感 遥感 遥感
背景情况:
- 全球紫外线 (UV) 表面反射率通常来自被动遥感,集成反射的紫外线光在各种方向.
- 现有的方法依赖于日光观测,可能无法有效捕捉方向表面特性.
研究的目的:
- 为了证明主动遥感,特别是Aeolus激光雷达表面回报 (LSR) 的能力,在全球范围内检索单向紫外线表面反射率.
- 通过使用主动传感技术建立一种用于表征表面反射率的新方法.
主要方法:
- 使用Aeolus激光雷达返回表面 (LSR) 数据来评估对表面特征的灵敏度.
- 将网格式的LSR数据与来自TROPOMI和GOME-2的兰伯特等效反射率 (LER) 气候学进行了比较.
- 分析了36个不同的地区在全球和区域范围内LSR和LER之间的相关性.
主要成果:
- 在撒哈拉沙漠,Aeolus LSR成功地复制了每月的表面反射率变化,与TROPOMI和GOME-2 LER气候学相一致.
- 在全球和区域尺度上实现了格式LSR和LER之间的高相关性 (r > 0.90).
- 从LSR信号中识别出不同的土地覆盖梯度,包括水/土地,植被/干旱地区以及雪/没有雪的区别. 在植被区域 (r < -0.60) 上,在LSR和植被指数之间发现了适度的负相关性.
结论:
- 该研究证明了第一个使用Aeolus检索单向紫外线表面反射率的活跃遥感方法的成功.
- 这种主动传感方法比被动仪器具有优势,可以检测陆地和雪地覆盖的变化,特别是在高度和夜间观测期间.
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