OpenAccessBelV2, Main, Exploration, bibRecord, 000673

Evapotranspiration amplifies European summer drought

Identifieur interne : 000673 ( Main/Exploration ); précédent : 000672; suivant : 000674

Evapotranspiration amplifies European summer drought

Auteurs : Adriaan J. Teuling [Pays-Bas] ; Anne F. Van Loon [Pays-Bas] ; Sonia I. Seneviratne [Suisse] ; Irene Lehner [Suisse, Suède] ; Marc Aubinet [Belgique] ; Bernard Heinesch [Belgique] ; Christian Bernhofer [Allemagne] ; Thomas Grünwald [Allemagne] ; Heiko Prasse [Allemagne] ; Uwe Spank [Allemagne]

Source :

Geophysical Research Letters [ 0094-8276 ] ; 2013-05-28.

RBID : ISTEX:A35CB0CF91C0F71585437120DD28D87DE082BDFE

Abstract

Drought is typically associated with a lack of precipitation, whereas the contribution of evapotranspiration and runoff to drought evolution is not well understood. Here we use unique long‐term observations made in four headwater catchments in central and western Europe to reconstruct storage anomalies and study the drivers of storage anomaly evolution during drought. We provide observational evidence for the “drought‐paradox” in that region: a consistent and significant increase in evapotranspiration during drought episodes, which acts to amplify the storage anomalies. In contrast, decreases in runoff act to limit storage anomalies. Our findings stress the need for the correct representation of evapotranspiration and runoff processes in drought indices.

Url:

https://api.istex.fr/document/A35CB0CF91C0F71585437120DD28D87DE082BDFE/fulltext/pdf

DOI: 10.1002/grl.50495

Affiliations:

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Le document en format XML

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<front><div type="abstract">Drought is typically associated with a lack of precipitation, whereas the contribution of evapotranspiration and runoff to drought evolution is not well understood. Here we use unique long‐term observations made in four headwater catchments in central and western Europe to reconstruct storage anomalies and study the drivers of storage anomaly evolution during drought. We provide observational evidence for the “drought‐paradox” in that region: a consistent and significant increase in evapotranspiration during drought episodes, which acts to amplify the storage anomalies. In contrast, decreases in runoff act to limit storage anomalies. Our findings stress the need for the correct representation of evapotranspiration and runoff processes in drought indices.</div>
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Evapotranspiration amplifies European summer drought

Evapotranspiration amplifies European summer drought

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