Abstract

Abstract. Land-surface albedo plays a critical role in the earth's radiant energy budget studies. Satellite remote sensing provides an effective approach to acquire regional and global albedo observations. Owing to cloud coverage, seasonal snow and sensor malfunctions, spatiotemporally continuous albedo datasets are often inaccessible. The Global LAnd Surface Satellite (GLASS) project aims at providing a suite of key land surface parameter datasets with high temporal resolution and high accuracy for a global change study. The GLASS preliminary albedo datasets are global daily land-surface albedo generated by an angular bin algorithm (Qu et al., 2013). Like other products, the GLASS preliminary albedo datasets are affected by large areas of missing data; beside, sharp fluctuations exist in the time series of the GLASS preliminary albedo due to data noise and algorithm uncertainties. Based on the Bayesian theory, a statistics-based temporal filter (STF) algorithm is proposed in this paper to fill data gaps, smooth albedo time series, and generate the GLASS final albedo product. The results of the STF algorithm are smooth and gapless albedo time series, with uncertainty estimations. The performance of the STF method was tested on one tile (H25V05) and three ground stations. Results show that the STF method has greatly improved the integrity and smoothness of the GLASS final albedo product. Seasonal trends in albedo are well depicted by the GLASS final albedo product. Compared with MODerate resolution Imaging Spectroradiometer (MODIS) product, the GLASS final albedo product has a higher temporal resolution and more competence in capturing the surface albedo variations. It is recommended that the quality flag should be always checked before using the GLASS final albedo product.

Highlights

  • Land-surface albedo refers to the ratio of reflected to incoming solar radiation at the earth’s surface over the solar spectral domain (Dickinson, 1983)

  • The filter parameters are derived from the a priori statistics

  • It is necessary to examine the consistency among the GLASS02A2x products before implementing the statisticsbased temporal filter (STF) algorithm

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Summary

Introduction

Land-surface albedo refers to the ratio of reflected to incoming solar radiation at the earth’s surface over the solar spectral domain (Dickinson, 1983). As one of the fundamental forcing parameters in climate models, surface albedo plays an important role in the earth’s radiant energy budget (Barnes and Roy, 2008, 2010; Liang et al, 2010; ManaloSmith et al, 1998). Spatio-temporal variability in albedo is often associated with environmental change and human activities as well (Bsaibes et al, 2009; Dirmeyer and Shukla, 1994; Jin and Roy, 2005; Moritz et al, 2002). According to the Global Climate Observing System (GCOS), spatiotemporally continuous albedo products with 5 % relative accuracy, 1 km spatial resolution and 1 day temporal resolution are required by climate studies (GCOS, 2011). Take the MODerate resolution Imaging Spectro-radiometer (MODIS) standard albedo product (MCD43B3) as an example, 20 % to 40 % of the global land pixels miss valid shortwave black-sky albedo (Table 1)

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