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Review and classification of indicators of green water availability and scarcity

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Corrigendum to Hydrol. Earth Syst. Sci., 19, 4581–4608, 2015 www.hydrol-earth-syst-sci.net/19/4581/2015/

doi:10.5194/hess-19-4581-2015-corrigendum © Author(s) 2016. CC Attribution 3.0 License.

Corrigendum to

“Review and classification of indicators of green water availability

and scarcity” published in Hydrol. Earth Syst. Sci., 19, 4581–4608,

2015

J. F. Schyns, A. Y. Hoekstra, and M. J. Booij

Twente Water Centre, University of Twente, Enschede, the Netherlands

Correspondence to: J. F. Schyns (j.f.schyns@utwente.nl)

Published: 18 February 2016

Three equations in Table A3 were erroneously displayed. This is the correct equation for ADD:

L X i=1 day θ ≤ θ wp .

This is the correct equation for KU:

X day S < Sthres .

This is the correct equation for SMDI:

365

X

i=1

S.

Furthermore, the description of the EDI in Table B1 should read follows:

“Ratio of the difference between the 5-day running mean of effective precipitation (EP, calculated from equations based on precipitation) and its climatological mean value over the standard deviation of this difference, measured per day.”

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[1] Roveri et al., 2014, The Messinian Salinity Crisis: Past and future of a great challenge for marine sciences, Marine Geology. [2] García-Veigas et al., 2018, Geochemical