首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Simulation of ATSR-2 optical data and estimates of land surface reflectance using simple atmospheric corrections
【24h】

Simulation of ATSR-2 optical data and estimates of land surface reflectance using simple atmospheric corrections

机译:使用简单的大气校正方法模拟ATSR-2光学数据并估算地面反射率

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The author presents simulations of ATSR-2 optical data using a combined orbit and scan model and model atmospheres. The atmospheric profiles are taken from LOWTRAN, but the author has converted these into a form suitable for a discrete ordinates radiative transfer code. All scattering processes are taken into account. The major approximations used are that the atmosphere is plane parallel, and that polarization is not taken into account. Cloud-free conditions are assumed. The author assumes ATSR-2 observations over the Earth with a constant atmosphere, and different types of reflecting ground in order to see what the implications are for retrieving ground reflectances. It was found that in the winter months, surface reflectance estimation will be difficult except at low latitudes. In the northern winter, the ATSR-2 forward scan sees large reflectances from aerosols in the atmosphere. These are not seen in the southern winter, but at 55/spl deg/ S, the Sun is more than 80/spl deg/ from the zenith point at ATSR-2 crossing times, and the atmosphere is still bright. The results from two simple reflectance retrieval algorithms and their region of validity are also examined . First, the author looks at a simulated retrieval for a Lambertian reflectance covering the globe at all times of year. Then the author looks at a simulated retrieval of a BRDF at a particular location using pairs of overpasses over a period of one year. It is predicted that the simple algorithms work well for ATSR-2 Sun/Sensor configurations except in the far northern and southern winters. The failure in the southern winter might be avoided if the Rayleigh/aerosol interaction is taken into account. It is als predicted that the forward scan data for the northern winter is unlikely to be useful for land surface studies, but might be useful for aerosol sounding, provided this is restricted to areas where there is no snow or frost. In this study of the BRDF at one location, it was found that if certain types of model BRDF are used, Sun synchronous orbits will severely limit the kinds of information that can be estimated.
机译:作者介绍了使用组合的轨道和扫描模型以及大气模型对ATSR-2光学数据进行的模拟。大气廓线取自LOWTRAN,但作者已将其转换为适合离散坐标辐射传递代码的形式。考虑所有散射过程。使用的主要近似值是大气是平面平行的,并且不考虑极化。假设无云条件。作者假设在大气层恒定的情况下对地球进行ATSR-2观测,并使用了不同类型的反射地面,以便了解其对获取地面反射率的影响。已经发现,在冬季,除了低纬度以外,表面反射率的估算将很困难。在北部冬季,ATSR-2正向扫描会看到大气中的气溶胶产生大量反射。这些在南部冬季没有出现,但在55 / spl deg / S时,太阳距ATSR-2穿越天顶点的天顶点超过80 / spl deg /,且大气仍很明亮。还研究了来自两种简单的反射率检索算法的结果及其有效性区域。首先,作者对一年四季都覆盖全球的朗伯反射率进行了模拟检索。然后,作者研究了在一年中使用一对立交桥对特定位置的BRDF进行的模拟检索。据预测,简单的算法对于ATSR-2太阳/传感器配置非常有效,除了北部和南部的冬季。如果考虑瑞利/气溶胶相互作用,可以避免南部冬季的失败。我们还预测,北部冬季的前向扫描数据不太可能用于陆地表面研究,但可能对气溶胶探测有用,前提是这仅限于无雪或无霜的地区。在对BRDF的一项研究中,发现如果使用某些类型的BRDF模型,Sun同步轨道将严重限制可以估计的信息种类。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号