Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe

Over the past decades, different drought indices have been suggested in the literature. This study tackles the problem of how to characterize droughts by defining a framework and proposing a generalized family of drought indices that is flexible regarding the use of different hydrological fluxes in...

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Main Authors: Christoph C. Raible, Oliver Bärenbold, Juan José Gómez-navarro
Format: Article
Language:English
Published: Stockholm University Press 2017-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://dx.doi.org/10.1080/16000870.2017.1296226
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author Christoph C. Raible
Oliver Bärenbold
Juan José Gómez-navarro
author_facet Christoph C. Raible
Oliver Bärenbold
Juan José Gómez-navarro
author_sort Christoph C. Raible
collection DOAJ
description Over the past decades, different drought indices have been suggested in the literature. This study tackles the problem of how to characterize droughts by defining a framework and proposing a generalized family of drought indices that is flexible regarding the use of different hydrological fluxes in the water balance. The sensitivity of various indices and its skill to represent drought conditions is evaluated using a regional model simulation for Europe spanning the last two millennia as test bed. The framework combines an exponentially damped memory with a normalization method based on quantile mapping. Both approaches are more robust and physically meaningful compared to the existing methods used to define drought indices. Still, the framework is flexible with respect to hydrological fluxes used for the water balance, enabling users to adapt the index formulation to the data availability of different locations. Based on it, indices using different hydrological fluxes in the water balance are compared with each other showing that a drought index considering only precipitation in the water balance is sufficient for western to central Europe. In the Mediterranean, temperature effects via evapotranspiration rather than potential evapotranspiration, need to be considered to produce meaningful indices representative of water deficit. In addition, our results indicate that in north-eastern Europe and Scandinavia, snow and run-off effects need to be considered simultaneously in the index definition to obtain accurate results.
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spelling doaj.art-8489c56d23a64b759bfcfb0bf0b6ec472022-12-22T02:56:30ZengStockholm University PressTellus: Series A, Dynamic Meteorology and Oceanography1600-08702017-01-0169110.1080/16000870.2017.12962261296226Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for EuropeChristoph C. Raible0Oliver Bärenbold1Juan José Gómez-navarro2University of BernUniversity of BernUniversity of BernOver the past decades, different drought indices have been suggested in the literature. This study tackles the problem of how to characterize droughts by defining a framework and proposing a generalized family of drought indices that is flexible regarding the use of different hydrological fluxes in the water balance. The sensitivity of various indices and its skill to represent drought conditions is evaluated using a regional model simulation for Europe spanning the last two millennia as test bed. The framework combines an exponentially damped memory with a normalization method based on quantile mapping. Both approaches are more robust and physically meaningful compared to the existing methods used to define drought indices. Still, the framework is flexible with respect to hydrological fluxes used for the water balance, enabling users to adapt the index formulation to the data availability of different locations. Based on it, indices using different hydrological fluxes in the water balance are compared with each other showing that a drought index considering only precipitation in the water balance is sufficient for western to central Europe. In the Mediterranean, temperature effects via evapotranspiration rather than potential evapotranspiration, need to be considered to produce meaningful indices representative of water deficit. In addition, our results indicate that in north-eastern Europe and Scandinavia, snow and run-off effects need to be considered simultaneously in the index definition to obtain accurate results.http://dx.doi.org/10.1080/16000870.2017.1296226drought indicespotential evopotranspirationEuroperegional modelling
spellingShingle Christoph C. Raible
Oliver Bärenbold
Juan José Gómez-navarro
Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
Tellus: Series A, Dynamic Meteorology and Oceanography
drought indices
potential evopotranspiration
Europe
regional modelling
title Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
title_full Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
title_fullStr Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
title_full_unstemmed Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
title_short Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe
title_sort drought indices revisited improving and testing of drought indices in a simulation of the last two millennia for europe
topic drought indices
potential evopotranspiration
Europe
regional modelling
url http://dx.doi.org/10.1080/16000870.2017.1296226
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