Spiers Gary D, Menzies Robert T, Jacob Joseph C
Appl Opt. 2016 Mar 10;55(8):1978-86. doi: 10.1364/AO.55.001978.
We report airborne measurements of lidar directional reflectance (backscatter) from land surfaces at a wavelength in the 2.05 μm CO₂ absorption band, with emphasis on snow-covered surfaces in various natural environments. Lidar backscatter measurements using this instrument provide insight into the capabilities of lidar for both airborne and future global-scale CO₂ measurements from low Earth orbit pertinent to the NASA Active Sensing of CO₂ Emissions over Nights, Days, and Seasons mission. Lidar measurement capability is particularly useful when the use of solar scattering spectroscopy is not feasible for high-accuracy atmospheric CO₂ measurements. Consequently, performance in high-latitude and winter season environments is an emphasis. Snow-covered surfaces are known to be dark in the CO₂ band spectral regions. The quantitative backscatter data from these field measurements help to elucidate the range of backscatter values that can be expected in natural environments.
我们报告了在2.05μm CO₂吸收带波长下对陆地表面激光雷达方向反射率(后向散射)的机载测量,重点是各种自然环境中被雪覆盖的表面。使用该仪器进行的激光雷达后向散射测量有助于深入了解激光雷达在机载以及未来与美国国家航空航天局“夜间、白天和季节二氧化碳排放主动遥感”任务相关的低地球轨道全球尺度二氧化碳测量方面的能力。当使用太阳散射光谱法进行高精度大气二氧化碳测量不可行时,激光雷达测量能力就特别有用。因此,高纬度和冬季环境中的性能是重点。众所周知,被雪覆盖的表面在CO₂波段光谱区域是暗的。这些实地测量的定量后向散射数据有助于阐明自然环境中预期的后向散射值范围。