Annual flood sensitivities to El Nino-Southern Oscillation at the global scale

被引:116
作者
Ward, P. J. [1 ,2 ]
Eisner, S. [3 ]
Floerke, M. [3 ]
Dettinger, M. D. [4 ,5 ]
Kummu, M. [6 ]
机构
[1] Vrije Univ Amsterdam, Inst Environm Studies IVM, Amsterdam, Netherlands
[2] Vrije Univ Amsterdam, Amsterdam Global Change Inst, Amsterdam, Netherlands
[3] Univ Kassel, Ctr Environm Syst Res, Kassel, Germany
[4] US Geol Survey, La Jolla, CA USA
[5] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[6] Aalto Univ, Water & Dev Res Grp, Espoo, Finland
基金
芬兰科学院;
关键词
UNITED-STATES; INTERDECADAL CHANGES; LA-NINA; ENSO; VARIABILITY; CLIMATE; STREAMFLOW; DROUGHT; TRENDS; WATER;
D O I
10.5194/hess-18-47-2014
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Floods are amongst the most dangerous natural hazards in terms of economic damage. Whilst a growing number of studies have examined how river floods are influenced by climate change, the role of natural modes of interannual climate variability remains poorly understood. We present the first global assessment of the influence of El Nino-Southern Oscillation (ENSO) on annual river floods, defined here as the peak daily discharge in a given year. The analysis was carried out by simulating daily gridded discharges using the WaterGAP model (Water - a Global Assessment and Prognosis), and examining statistical relationships between these discharges and ENSO indices. We found that, over the period 1958-2000, ENSO exerted a significant influence on annual floods in river basins covering over a third of the world's land surface, and that its influence on annual floods has been much greater than its influence on average flows. We show that there are more areas in which annual floods intensify with La Nina and decline with El Nino than vice versa. However, we also found that in many regions the strength of the relationships between ENSO and annual floods have been non-stationary, with either strengthening or weakening trends during the study period. We discuss the implications of these findings for science and management. Given the strong relationships between ENSO and annual floods, we suggest that more research is needed to assess relationships between ENSO and flood impacts (e. g. loss of lives or economic damage). Moreover, we suggest that in those regions where useful relationships exist, this information could be combined with ongoing advances in ENSO prediction research, in order to provide year-to-year probabilistic flood risk forecasts.
引用
收藏
页码:47 / 66
页数:20
相关论文
共 95 条
[1]   Development and testing of the WaterGAP 2 global model of water use and availability [J].
Alcamo, J ;
Döll, P ;
Henrichs, T ;
Kaspar, F ;
Lehner, B ;
Rösch, T ;
Siebert, S .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2003, 48 (03) :317-337
[2]   Global warming increases flood risk in mountainous areas [J].
Allamano, P. ;
Claps, P. ;
Laio, F. .
GEOPHYSICAL RESEARCH LETTERS, 2009, 36
[3]  
[Anonymous], 2011, GLOB ASS REP DIS RIS
[4]  
[Anonymous], 2013, CLIM CHAG 2013 PHYS, DOI DOI 10.1017/CBO9781107415324
[5]   Joint Spatiotemporal Variability of Global Sea Surface Temperatures and Global Palmer Drought Severity Index Values [J].
Apipattanavis, Somkiat ;
McCabe, Gregory J. ;
Rajagopalan, Balaji ;
Gangopadhyay, Subhrendu .
JOURNAL OF CLIMATE, 2009, 22 (23) :6251-6267
[6]   Variation in the relationship between snowmelt runoff in Oregon and ENSO and PDO [J].
Beebee, RA ;
Manga, M .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 2004, 40 (04) :1011-1024
[7]  
BELL GD, 1995, B AM METEOROL SOC, V76, P681, DOI 10.1175/1520-0477(1995)076<0681:ACAWTM>2.0.CO
[8]  
2
[9]   Global assessment of El Nino's disaster burden [J].
Bouma, MJ ;
Kovats, RS ;
Goubet, SA ;
Cox, JSH ;
Haines, A .
LANCET, 1997, 350 (9089) :1435-1438
[10]   Regional sensitivities of mean and peak river discharge to climate variability in Europe [J].
Bouwer, Laurens M. ;
Vermaat, Jan E. ;
Aerts, Jeroen C. J. H. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D19)