Abstract

Remotely sensed data can be used to model the fractional cover of green vegetation (GV), non-photosynthetic vegetation (NPV), and soil in natural and agricultural ecosystems. NPV and soil cover are difficult to estimate accurately since absorption by lignin, cellulose, and other organic molecules cannot be resolved by broadband multispectral data. A new generation of satellite hyperspectral imagers will provide contiguous narrowband coverage, enabling new, more accurate, and potentially global fractional cover products. We used six field spectroscopy datasets collected in prior experiments from sites with partial crop, grass, shrub, and low-stature resprouting tree cover to simulate satellite hyperspectral data, including sensor noise and atmospheric correction artifacts. The combined dataset was used to compare hyperspectral index-based and spectroscopic methods for estimating GV, NPV, and soil fractional cover. GV fractional cover was estimated most accurately. NPV and soil fractions were more difficult to estimate, with spectroscopic methods like partial least squares (PLS) regression, spectral feature analysis (SFA), and multiple endmember spectral mixture analysis (MESMA) typically outperforming hyperspectral indices. Using an independent validation dataset, the lowest root mean squared error (RMSE) values were 0.115 for GV using either normalized difference vegetation index (NDVI) or SFA, 0.164 for NPV using PLS, and 0.126 for soil using PLS. PLS also had the lowest RMSE averaged across all three cover types. This work highlights the need for more extensive and diverse fine spatial scale measurements of fractional cover, to improve methodologies for estimating cover in preparation for future hyperspectral global monitoring missions.

Highlights

  • Terrestrial vegetation is dynamic, with both photosynthetically active and inactive vegetation cover varying on seasonal, annual, and decadal time scales

  • green vegetation (GV) fractional cover was estimated with lower error in comparison to non-photosynthesizing vegetation (NPV) and soil fractional cover (Table 4)

  • normalized difference vegetation index (NDVI), one of the most basic vegetation indices, and spectral feature analysis (SFA), a spectroscopic method focusing solely on a chlorophyll absorption feature in this case, outperformed the other metrics when applied to the validation library

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Summary

Introduction

Terrestrial vegetation is dynamic, with both photosynthetically active and inactive vegetation cover varying on seasonal, annual, and decadal time scales. To quantify spatial and temporal variations in vegetation cover, previous studies have modeled cover in natural and agricultural ecosystems as having three fractional components that sum to 100% cover: photosynthesizing or “green” vegetation (GV), non-photosynthesizing vegetation (NPV), and bare soil [1,2,3,4]. NPV cover includes dead and senescent leaves and needles, plant litter, and non-photosynthesizing branch and stem tissues. A transition from GV to NPV or soil cover is a hallmark of both seasonal and long-term drought. Grasslands senesce during periods of drought, resulting in a decrease in GV cover and a corresponding increase in NPV cover [5]. Long-term drought can result in canopy dieback and mortality, producing similar changes in fractional cover [6]

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