Abstract

Synthetic Aperture Radar (SAR) backscatter measurements are sensitive to forest aboveground biomass (AGB), and the observations from space can be used for mapping AGB globally. However, the radar sensitivity saturates at higher AGB values depending on the wavelength and geometry of radar measurements, and is influenced by the structure of the forest and environmental conditions. Here, we examine the sensitivity of SAR at the L-band frequency (~25 cm wavelength) to AGB in order to examine the performance of future joint National Aeronautics and Space Administration, Indian Space Research Organisation NASA-ISRO SAR mission in mapping the AGB of global forests. For SAR data, we use the Phased Array L-Band SAR (PALSAR) backscatter from the Advanced Land Observing Satellite (ALOS) aggregated at a 100-m spatial resolution; and for AGB data, we use more than three million AGB values derived from the Geoscience Laser Altimeter System (GLAS) LiDAR height metrics at about 0.16–0.25 ha footprints across eleven different forest types globally. The results from statistical analysis show that, over all eleven forest types, saturation level of L-band radar at HV polarization on average remains ≥100 Mg·ha−1. Fresh water swamp forests have the lowest saturation with AGB at ~80 Mg·ha−1, while needleleaf forests have the highest saturation at ~250 Mg·ha−1. Swamp forests show a strong backscatter from the vegetation-surface specular reflection due to inundation that requires to be treated separately from those on terra firme. Our results demonstrate that L-Band backscatter relations to AGB can be significantly different depending on forest types and environmental effects, requiring multiple algorithms to map AGB from time series of satellite radar observations globally.

Highlights

  • Forests play an important role in the global carbon cycle both by storing carbon and by functioning as a sink for roughly a quarter of the annual anthropogenic emissions of carbon dioxide to the atmosphere [1,2]

  • Many sources of error can contribute to this high level of noise at the pixel level: speckle noise in radar backscatter, error in Geoscience Laser Altimeter System (GLAS)-derived aboveground biomass (AGB), mismatch between Advanced Land Observing Satellite (ALOS) pixel size and GLAS footprint size, geo-location errors between GLAS shots and ALOS pixels

  • It is important that forest types are considered separately when using L-band radar backscatter to study AGB

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Summary

Introduction

Forests play an important role in the global carbon cycle both by storing carbon and by functioning as a sink for roughly a quarter of the annual anthropogenic emissions of carbon dioxide to the atmosphere [1,2]. (1) deforestation and degradation that reduces the forest biomass from its original state at time t0 to a reduced state in the case of degradation and to approximately zero in the case of deforestation at time t1 ; (2) recovery through the process of regeneration and afforestation after time t1 towards its original state. These two trajectories are often related to human activities on changing the land use and land cover (LULC). The global biomass in vegetation is distributed in different forest types or in a mosaic of shrubs and trees over landscapes with a large diversity of Remote Sens. 2016, 8, 522; doi:10.3390/rs8060522 www.mdpi.com/journal/remotesensing

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