The University of Southampton
University of Southampton Institutional Repository

Global multimodel analysis of drought in runofffor the second half of the twentieth century

Global multimodel analysis of drought in runofffor the second half of the twentieth century
Global multimodel analysis of drought in runofffor the second half of the twentieth century

During the past decades large-scale models have been developed to simulate global and continental terrestrial water cycles. It is an open question whether thesemodels are suitable to capture hydrological drought, in terms of runoff, on a global scale. Amultimodel ensemble analysis was carried out to evaluate if 10 such large-scalemodels agree on major drought events during the second half of the twentieth century. Time series of monthly precipitation, monthly total runofffrom 10 global hydrologicalmodels, and their ensemblemedian have been used to identify drought. Temporal development of area in drought for various regions across the globe was investigated. Model spread was largest in regions with low runoffand smallest in regions with high runoff. In vast regions, correlation between runoffdrought derived from the models and meteorological drought was found to be low. This indicated that models add information to the signal derived from precipitation and that runoffdrought cannot directly be determined from precipitation data alone in global drought analyses with a constant aggregation period. However, duration and spatial extent of major drought events differed between models. Some models showed a fast runoffresponse to rainfall, which led to deviations from reported drought events in slowly responding hydrological systems. By using an ensemble of models, this fast runoffresponse was partly overcome and delay in drought propagating from meteorological drought to drought in runoffwas included. Finally, an ensemble of models also allows for consideration of uncertainty associated with individual model structures.

1525-755X
1535-1552
Van Huijgevoort, M. H.J.
0ec5c477-0d08-4ec0-ae2b-4fa76fe67fe1
Hazenberg, P.
8c6ec713-84ea-4fe7-8fed-e4257338736c
Van Lanen, H. A.J.
b6b14260-5c51-41e4-9361-0a6e3d0f46ef
Teuling, A. J.
eae6f7db-4bec-40ea-80f3-5976aabdecb0
Clark, D. B.
537f80e8-cbe6-41eb-b1d4-31af1f0e6393
Folwell, S.
810773c3-b406-4d08-9638-dbe294a38c58
Gosling, S. N.
327615f9-814d-4b64-9809-d8b4496ac1ca
Hanasaki, N.
8273e2e4-cadd-4ac6-8bf6-645bf61b2db6
Heinke, J.
40d11c87-5dcb-4d16-8fb1-522e08f5c584
Koirala, S.
ec3c3aac-c9da-4149-823b-59079b468d33
Stacke, T.
ef78557a-1980-4788-bd79-ba7c81ee92f2
Voss, F.
688c42b7-3563-43b2-89c2-f5f153c75967
Sheffield, J.
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Uijlenhoet, R.
8dcc493a-9931-45a6-a7b6-7fe161bd0fd0
Van Huijgevoort, M. H.J.
0ec5c477-0d08-4ec0-ae2b-4fa76fe67fe1
Hazenberg, P.
8c6ec713-84ea-4fe7-8fed-e4257338736c
Van Lanen, H. A.J.
b6b14260-5c51-41e4-9361-0a6e3d0f46ef
Teuling, A. J.
eae6f7db-4bec-40ea-80f3-5976aabdecb0
Clark, D. B.
537f80e8-cbe6-41eb-b1d4-31af1f0e6393
Folwell, S.
810773c3-b406-4d08-9638-dbe294a38c58
Gosling, S. N.
327615f9-814d-4b64-9809-d8b4496ac1ca
Hanasaki, N.
8273e2e4-cadd-4ac6-8bf6-645bf61b2db6
Heinke, J.
40d11c87-5dcb-4d16-8fb1-522e08f5c584
Koirala, S.
ec3c3aac-c9da-4149-823b-59079b468d33
Stacke, T.
ef78557a-1980-4788-bd79-ba7c81ee92f2
Voss, F.
688c42b7-3563-43b2-89c2-f5f153c75967
Sheffield, J.
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Uijlenhoet, R.
8dcc493a-9931-45a6-a7b6-7fe161bd0fd0

Van Huijgevoort, M. H.J., Hazenberg, P., Van Lanen, H. A.J., Teuling, A. J., Clark, D. B., Folwell, S., Gosling, S. N., Hanasaki, N., Heinke, J., Koirala, S., Stacke, T., Voss, F., Sheffield, J. and Uijlenhoet, R. (2013) Global multimodel analysis of drought in runofffor the second half of the twentieth century. Journal of Hydrometeorology, 14 (5), 1535-1552. (doi:10.1175/JHM-D-12-0186.1).

Record type: Article

Abstract

During the past decades large-scale models have been developed to simulate global and continental terrestrial water cycles. It is an open question whether thesemodels are suitable to capture hydrological drought, in terms of runoff, on a global scale. Amultimodel ensemble analysis was carried out to evaluate if 10 such large-scalemodels agree on major drought events during the second half of the twentieth century. Time series of monthly precipitation, monthly total runofffrom 10 global hydrologicalmodels, and their ensemblemedian have been used to identify drought. Temporal development of area in drought for various regions across the globe was investigated. Model spread was largest in regions with low runoffand smallest in regions with high runoff. In vast regions, correlation between runoffdrought derived from the models and meteorological drought was found to be low. This indicated that models add information to the signal derived from precipitation and that runoffdrought cannot directly be determined from precipitation data alone in global drought analyses with a constant aggregation period. However, duration and spatial extent of major drought events differed between models. Some models showed a fast runoffresponse to rainfall, which led to deviations from reported drought events in slowly responding hydrological systems. By using an ensemble of models, this fast runoffresponse was partly overcome and delay in drought propagating from meteorological drought to drought in runoffwas included. Finally, an ensemble of models also allows for consideration of uncertainty associated with individual model structures.

This record has no associated files available for download.

More information

Published date: 2013

Identifiers

Local EPrints ID: 480465
URI: http://eprints.soton.ac.uk/id/eprint/480465
ISSN: 1525-755X
PURE UUID: 7a91e1b6-0dfc-4f01-8587-1f3acf966c0e
ORCID for J. Sheffield: ORCID iD orcid.org/0000-0003-2400-0630

Catalogue record

Date deposited: 02 Aug 2023 17:10
Last modified: 17 Mar 2024 03:40

Export record

Altmetrics

Contributors

Author: M. H.J. Van Huijgevoort
Author: P. Hazenberg
Author: H. A.J. Van Lanen
Author: A. J. Teuling
Author: D. B. Clark
Author: S. Folwell
Author: S. N. Gosling
Author: N. Hanasaki
Author: J. Heinke
Author: S. Koirala
Author: T. Stacke
Author: F. Voss
Author: J. Sheffield ORCID iD
Author: R. Uijlenhoet

Download statistics

Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.

View more statistics

Atom RSS 1.0 RSS 2.0

Contact ePrints Soton: eprints@soton.ac.uk

ePrints Soton supports OAI 2.0 with a base URL of http://eprints.soton.ac.uk/cgi/oai2

This repository has been built using EPrints software, developed at the University of Southampton, but available to everyone to use.

We use cookies to ensure that we give you the best experience on our website. If you continue without changing your settings, we will assume that you are happy to receive cookies on the University of Southampton website.

×