Abstract

Abstract. Human impacts on global terrestrial hydrology have been accelerating during the 20th century. These human impacts include the effects of reservoir building and human water use, as well as land cover change. To date, many global studies have focussed on human water use, but only a few focus on or include the impact of land cover change. Here we use PCR-GLOBWB, a combined global hydrological and water resources model, to assess the impacts of land cover change as well as human water use globally in different climatic zones. Our results show that land cover change has a strong effect on the global hydrological cycle, on the same order of magnitude as the effect of human water use (applying irrigation, abstracting water, for industrial use for example, including reservoirs, etc.). When globally averaged, changing the land cover from that of 1850 to that of 2000 increases discharge through reduced evapotranspiration. The effect of land cover change shows large spatial variability in magnitude and sign of change depending on, for example, the specific land cover change and climate zone. Overall, land cover effects on evapotranspiration are largest for the transition of tall natural vegetation to crops in energy-limited equatorial and warm temperate regions. In contrast, the inclusion of irrigation, water abstraction and reservoirs reduces global discharge through enhanced evaporation over irrigated areas and reservoirs as well as through water consumption. Hence, in some areas land cover change and water distribution both reduce discharge, while in other areas the effects may partly cancel out. The relative importance of both types of impacts varies spatially across climatic zones. From this study we conclude that land cover change needs to be considered when studying anthropogenic impacts on water resources.

Highlights

  • The anthropogenic impact on the global terrestrial hydrological cycle has many aspects

  • We describe the impact of land cover change on the terrestrial hydrological cycle and compare this to the impact of human water use, by looking at differences in the results of LC2000 vs. LC1850 as well as HUM2000 vs. LC2000

  • The largest discharge changes occur in arid climates (B), especially when tall natural vegetation is replaced by crops

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Summary

Introduction

The anthropogenic impact on the global terrestrial hydrological cycle has many aspects. Humans have altered a large part of the land surface, replacing 33 % (Vitousek et al, 1997) or even 41 % (Sterling et al, 2013) of natural vegetation by anthropogenic land cover such as crop fields or pasture Such land cover change can affect terrestrial hydrology by changing the evaporation-to-runoff ratio. We compare the effects of land cover change, mainly the expansion of crop and pasture at the expense of natural vegetation, to human water use, i.e., water abstraction for irrigation and non-irrigation use as well as reservoir building We compare these effects globally as well as spatially, providing an indepth analysis across climatic zones

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