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Development, Validation, and Potential Enhancements to the Second-Generation Operational Aerosol Product at the National Environmental Satellite, Data, and Information Service of the National Oceanic and Atmospheric Administration

机译:国家海洋和大气管理局国家环境卫星,数据和信息服务处第二代可操作气溶胶产品的开发,验证和潜在增强

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摘要

A revised (phase 2) single-channel algorithm for aerosol optical thickness, tau(sup A)(sub SAT), retrieval over oceans from radiances in channel 1 (0.63 microns) of the Advanced Very High Resolution Radiometer (AVHRR) has been implemented at the National Oceanic and Atmospheric Administration's National Environmental Satellite Data and Information Service for the NOAA 14 satellite launched December 30, 1994. It is based on careful validation of its operational predecessor (phase 1 algorithm), implemented for NOAA 14 in 1989. Both algorithms scale the upward satellite radiances in cloud-free conditions to aerosol optical thickness using an updated radiative transfer model of the ocean and atmosphere. Application of the phase 2 algorithm to three matchup Sun-photometer and satellite data sets, one with NOAA 9 in 1988 and two with NOAA 11 in 1989 and 1991, respectively, show systematic error is less than 10%, with a random error of sigma(sub tau) approx. equal 0.04. First results of tau(sup A)(sub SAT) retrievals from NOAA 14 using the phase 2 algorithm, and from checking its internal consistency, are presented. The potential two-channel (phase 3) algorithm for the retrieval of an aerosol size parameter, such as the Junge size distribution exponent, by adding either channel 2 (0.83 microns) from the current AVHRR instrument, or a 1.6-microns channel to be available on the Tropical Rainfall Measurement Mission and the NOAA-KLM satellites by 1997 is under investigation. The possibility of using this additional information in the retrieval of a more accurate estimate of aerosol optical thickness is being explored.
机译:实施了修订版(第2阶段)气溶胶光学厚度tau(sup A)(sub SAT)的单通道算法,该方法是从高级甚高分辨率辐射仪(AVHRR)的通道1(0.63微米)的辐射中提取出来的。是在1994年12月30日发射的美国国家海洋和大气管理局的国家环境卫星数据和信息服务局(NOAA 14)上进行的。它是基于对已于1989年为国家海洋与大气管理局(NOAA)14实施的其运行前身(第1阶段算法)进行仔细验证的基础。使用更新的海洋和大气辐射传输模型,将无云条件下的向上卫星辐射缩放为气溶胶光学厚度。将阶段2算法应用到三个配对太阳光度计和卫星数据集上,其中一个分别于1988年使用NOAA 9和两个在1989年和1991年使用NOAA 11,显示系统误差小于10%,随机误差为sigma (sub tau)约等于0.04。提出了使用阶段2算法并通过检查其内部一致性从NOAA 14中检索tau(sup A)(sub SAT)的结果。通过添加当前AVHRR仪器的通道2(0.83微米)或要添加的1.6微米通道,可以检索气溶胶尺寸参数(例如Junge尺寸分布指数)的潜在两通道(阶段3)算法。正在研究热带雨量测量团和NOAA-KLM卫星在1997年之前提供的卫星。正在探索在获取更精确的气溶胶光学厚度估算值时使用此附加信息的可能性。

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