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Functional relation of land surface albedo with climatological variables: a review on remote sensing techniques and recent research developments

机译:地表反照率与气候变量的功能关系:遥感技术和最新研究进展的综述

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Surface albedo has been documented as one of the Essential Climate Variables (ECV) of the Global Climate Observing System (GCOS) that governs the Earth’s Radiation Budget. The availability of surface albedo data is necessary for a comprehensive environmental modelling study. Thus, both temporal and spatial scale issues need to be rectified. This study reports about the availability of surface albedo data through in-situ and remote sensing satellite observations. In this paper, we reviewed the existing models for surface albedo derivation and various initiatives taken by related environmental agencies in order to understand the issues of climate with respect to surface albedo. This investigation evaluated the major activities on albedo-related research specifically for the retrieval methods used to derive the albedo values. Two main existing albedo measurement methods are derived through in-situ measurement and remotely sensed observations. In-situ measurement supported with number of instruments and techniques such aspyrheliometers, pyranometers and Baseline Surface Radiation Network (BSRN) and remotely sensed observations using angularly integrated Bidirectional Reflectance Distribution Function (BRDF) by both geostationary and polar orbit satellites. The investigation results reveals that the temporal and spatial scaling is the major issues when the albedo values are needed for microclimatic study, i.e. high-resolution time-series analyses and at heterogeneity and impervious surface. Thus, an improved technique of albedo retrieval at better spatial and temporal scale is required to fulfil the need for such kind of studies. Amongst many others, there are two downscaling methods that have been identified to be used in resolving the spatial scaling biased issues: Smoothing Filter-based Intensity Modulation (SFIM) and Pixel Block Intensity Modulation (PBIM). The temporal issues can be resolved using the multiple regression techniques of land surface temperature, selected air quality parameters, aerosol and daily skylight.
机译:地表反照率已被证明是控制地球辐射预算的全球气候观测系统(GCOS)的基本气候变量(ECV)之一。表面反照率数据的可用性对于全面的环境建模研究是必要的。因此,时间和空间尺度问题都需要纠正。这项研究报告了通过原位和遥感卫星观测获得的地表反照率数据的情况。在本文中,我们回顾了地表反照率推导的现有模型以及相关环境机构采取的各种举措,以了解与地表反照率有关的气候问题。这项调查评估了与反照率相关研究的主要活动,特别是用于推导反照率值的检索方法。现有的两种主要反照率测量方法是通过原位测量和遥感观测得出的。地热测量得到了许多仪器和技术的支持,例如高温计,日射强度计和基线表面辐射网络(BSRN),以及对地静止和极地轨道卫星使用角度积分双向反射分布函数(BRDF)进行的遥感观测。调查结果表明,当微气候研究需要高分辨率,时间序列分析以及非均质性和不透水表面的反照率值时,时空尺度是主要问题。因此,需要一种在更好的时空尺度上改进反照率的技术来满足这类研究的需要。在许多其他方法中,已经确定有两种缩小比例的方法可用于解决空间比例缩放的问题:基于平滑滤波器的强度调制(SFIM)和像素块强度调制(PBIM)。可以使用土地表面温度,选定的空气质量参数,气溶胶和每日天窗的多元回归技术解决时间问题。

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