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本文引用的文献

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CALIPSO Lidar Calibration at 532 nm: Version 4 Nighttime Algorithm.CALIPSO激光雷达在532纳米处的校准:第4版夜间算法
Atmos Meas Tech. 2018 Mar;11(3):1459-1479. doi: 10.5194/amt-11-1459-2018. Epub 2018 Mar 14.
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The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2).现代时代研究与应用回顾分析第2版(MERRA-2)
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Seasonally Transported Aerosol Layers over Southeast Atlantic are Closer to Underlying Clouds than Previously Reported.东南大西洋上空季节性传输的气溶胶层比之前报道的更靠近下层云。
Geophys Res Lett. 2017 Jun 12;Volume 44(Iss 11):5818-5825. doi: 10.1002/2017gl073559.
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9
Aerosol and cloud backscatter at 1.06, 1.54, and 0.53 mum by airborne hard-target-calibrated Nd:YAG /methane Raman lidar.通过机载硬目标校准的Nd:YAG/甲烷拉曼激光雷达测量1.06、1.54和0.53微米处的气溶胶和云后向散射。
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云气溶胶传输系统(CATS)1064纳米校准与验证

Cloud Aerosol Transport System (CATS) 1064 nm Calibration and Validation.

作者信息

Pauly Rebecca M, Yorks John E, Hlavka Dennis L, McGill Matthew J, Amiridis Vassilis, Palm Stephen P, Rodier Sharon D, Vaughan Mark A, Selmer Patrick A, Kupchock Andrew W, Baars Holger, Gialitaki Anna

机构信息

Science Systems and Applications Inc., Lanham, 20706, United States.

NASA Godard Space Flight Center, Greenbelt, 20771, United States.

出版信息

Atmos Meas Tech. 2019 Nov 28;12(11):6241-6258. doi: 10.5194/amt-12-6241-2019.

DOI:10.5194/amt-12-6241-2019
PMID:33414857
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7786814/
Abstract

The Cloud-Aerosol Transport System (CATS) lidar on board the International Space Station (ISS) operated from 10 February 2015 to 30 October 2017 providing range-resolved vertical backscatter profiles of Earth's atmosphere at 1064 and 532 nm. The CATS instrument design and ISS orbit lead to a higher 1064 nm signal-to-noise ratio than previous space-based lidars, allowing for direct atmospheric calibration of the 1064 nm signals. Nighttime CATS Version 3-00 data were calibrated by scaling the measured data to a model of the expected atmospheric backscatter between 22 and 26 km above mean sea level (AMSL). The CATS atmospheric model is constructed using molecular backscatter profiles derived from Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) re-analysis data and aerosol scattering ratios measured by the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP). The nighttime normalization altitude region was chosen to simultaneously minimize aerosol loading and variability within the CATS data frame, which extends from 28 km to -2 km AMSL. Daytime CATS Version 3-00 data were calibrated through comparisons with nighttime measurements of the layer integrated attenuated total backscatter (iATB) from strongly scattering, rapidly attenuating opaque cirrus clouds. The CATS nighttime 1064 nm attenuated total backscatter (ATB) uncertainties for clouds and aerosols are primarily related to the uncertainties in the CATS nighttime calibration technique, which are estimated to be 9%. Median CATS V3-00 1064 nm ATB relative uncertainty at night within cloud and aerosol layers is 7%, slightly lower than these calibration uncertainty estimates. CATS median daytime 1064 nm ATB relative uncertainty is 21% in cloud and aerosol layers, similar to the estimated 16-18% uncertainty in the CATS daytime cirrus cloud calibration transfer technique. Coincident daytime comparisons between CATS and the Cloud Physics Lidar (CPL) during the CATS-CALIPSO Airborne Validation Experiment (CCAVE) project show good agreement in mean ATB profiles for clear-air regions. Eight nighttime comparisons between CATS and the Polly ground based lidars also show good agreement in clear-air regions between 3-12 km, with CATS having a mean ATB of 19.7 % lower than Polly. Agreement between the two instruments (7%) is even better within an aerosol layer. Six-month comparisons of nighttime ATB values between CATS and the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) also show that iATB comparisons of opaque cirrus clouds agree to within 19%. Overall, CATS has demonstrated that direct calibration of the 1064 nm channel is possible from a space based lidar using the atmospheric normalization technique.

摘要

国际空间站(ISS)上的云和气溶胶传输系统(CATS)激光雷达于2015年2月10日至2017年10月30日运行,提供了1064纳米和532纳米波长下地球大气的距离分辨垂直后向散射剖面。CATS仪器设计和国际空间站轨道使得1064纳米波长的信噪比高于以往的天基激光雷达,从而能够对1064纳米信号进行直接大气校准。夜间CATS 3-00版本数据通过将测量数据按比例缩放至平均海平面(AMSL)以上22至26千米处预期大气后向散射模型进行校准。CATS大气模型是利用从现代时代回顾性分析研究与应用版本2(MERRA-2)再分析数据得出的分子后向散射剖面以及由正交极化云和气溶胶激光雷达(CALIOP)测量的气溶胶散射比构建的。夜间归一化高度区域的选择是为了同时最小化CATS数据帧内的气溶胶负荷和变异性,该数据帧范围从AMSL的28千米到-2千米。白天CATS 3-00版本数据通过与强散射、快速衰减的不透明卷云的层积分衰减总后向散射(iATB)夜间测量值进行比较来校准。CATS夜间1064纳米波长下云和气溶胶的衰减总后向散射(ATB)不确定性主要与CATS夜间校准技术的不确定性有关,估计约为9%。CATS V3-00夜间在云层和气溶胶层内1064纳米ATB的相对不确定性中位数为7%,略低于这些校准不确定性估计值。CATS白天在云层和气溶胶层内1064纳米ATB的相对不确定性中位数为21%,与CATS白天卷云校准转移技术中估计的16 - 18%不确定性相似。在CATS - CALIPSO机载验证实验(CCAVE)项目期间,CATS与云物理激光雷达(CPL)的白天同步比较显示,晴空区域的平均ATB剖面吻合良好。CATS与基于地面的波利激光雷达的八次夜间比较也显示,在3 - 12千米的晴空区域吻合良好,CATS的平均ATB比波利低19.7%。在气溶胶层内,两种仪器之间的吻合度(约7%)甚至更好。CATS与正交极化云和气溶胶激光雷达(CALIOP)夜间ATB值的六个月比较还表明,不透明卷云的iATB比较吻合度在19%以内。总体而言,CATS已证明使用大气归一化技术从天基激光雷达对1064纳米通道进行直接校准是可行的。