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1 Introduction More than 16% of the world's population relies on glaciers and snowmelt as a source of water (Barnett et al., 2005). In the tropical and subtropical arid and semi-arid regions, over 80% of the freshwater used by humans comes from mountains (Messerli, 2001; Vuille et al., 2008). Cauvy-Fraunié and Dangles (2019) identified glacier cover and melting rates, among other factors, as key variables that can modulate taxon sensitivity.
Abstract Changes in terrestrial tropical carbon stocks have an important role in the global carbon budget. However, current observational tools do not allow accurate and large-scale monitoring of the spatial distribution and dynamics of carbon stocks1.
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