Resum
Risk management has reduced vulnerability to floods and droughts globally1,2, yet their impacts are still increasing3. An improved understanding of the causes of changing impacts is therefore needed, but has been hampered by a lack of empirical data4,5. On the basis of a global dataset of 45 pairs of events that occurred within the same area, we show that risk management generally reduces the impacts of floods and droughts but faces difficulties in reducing the impacts of unprecedented events of a magnitude not previously experienced. If the second event was much more hazardous than the first, its impact was almost always higher. This is because management was not designed to deal with such extreme events: for example, they exceeded the design levels of levees and reservoirs. In two success stories, the impact of the second, more hazardous, event was lower, as a result of improved risk management governance and high investment in integrated management. The observed difficulty of managing unprecedented events is alarming, given that more extreme hydrological events are projected owing to climate change3.
Idioma original | Anglès |
---|---|
Pàgines (de-a) | 80-86 |
Nombre de pàgines | 7 |
Revista | Nature |
Volum | 608 |
Número | 7921 |
DOIs | |
Estat de la publicació | Publicada - 4 d’ag. 2022 |
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In: Nature, Vol. 608, Núm. 7921, 04.08.2022, pàg. 80-86.
Producció científica: Article en revista indexada › Article › Avaluat per experts
TY - JOUR
T1 - The challenge of unprecedented floods and droughts in risk management
AU - Kreibich, Heidi
AU - Van Loon, Anne F.
AU - Schröter, Kai
AU - Ward, Philip J.
AU - Mazzoleni, Maurizio
AU - Sairam, Nivedita
AU - Abeshu, Guta Wakbulcho
AU - Agafonova, Svetlana
AU - AghaKouchak, Amir
AU - Aksoy, Hafzullah
AU - Alvarez-Garreton, Camila
AU - Aznar, Blanca
AU - Balkhi, Laila
AU - Barendrecht, Marlies H.
AU - Biancamaria, Sylvain
AU - Bos-Burgering, Liduin
AU - Bradley, Chris
AU - Budiyono, Yus
AU - Buytaert, Wouter
AU - Capewell, Lucinda
AU - Carlson, Hayley
AU - Cavus, Yonca
AU - Couasnon, Anaïs
AU - Coxon, Gemma
AU - Daliakopoulos, Ioannis
AU - de Ruiter, Marleen C.
AU - Delus, Claire
AU - Erfurt, Mathilde
AU - Esposito, Giuseppe
AU - François, Didier
AU - Frappart, Frédéric
AU - Freer, Jim
AU - Frolova, Natalia
AU - Gain, Animesh K.
AU - Grillakis, Manolis
AU - Grima, Jordi Oriol
AU - Guzmán, Diego A.
AU - Huning, Laurie S.
AU - Ionita, Monica
AU - Kharlamov, Maxim
AU - Khoi, Dao Nguyen
AU - Kieboom, Natalie
AU - Kireeva, Maria
AU - Koutroulis, Aristeidis
AU - Lavado-Casimiro, Waldo
AU - Li, Hong Yi
AU - LLasat, María Carmen
AU - Macdonald, David
AU - Mård, Johanna
AU - Mathew-Richards, Hannah
AU - McKenzie, Andrew
AU - Mejia, Alfonso
AU - Mendiondo, Eduardo Mario
AU - Mens, Marjolein
AU - Mobini, Shifteh
AU - Mohor, Guilherme Samprogna
AU - Nagavciuc, Viorica
AU - Ngo-Duc, Thanh
AU - Thao Nguyen Huynh, Thi
AU - Nhi, Pham Thi Thao
AU - Petrucci, Olga
AU - Nguyen, Hong Quan
AU - Quintana-Seguí, Pere
AU - Razavi, Saman
AU - Ridolfi, Elena
AU - Riegel, Jannik
AU - Sadik, Md Shibly
AU - Savelli, Elisa
AU - Sazonov, Alexey
AU - Sharma, Sanjib
AU - Sörensen, Johanna
AU - Arguello Souza, Felipe Augusto
AU - Stahl, Kerstin
AU - Steinhausen, Max
AU - Stoelzle, Michael
AU - Szalińska, Wiwiana
AU - Tang, Qiuhong
AU - Tian, Fuqiang
AU - Tokarczyk, Tamara
AU - Tovar, Carolina
AU - Tran, Thi Van Thu
AU - Van Huijgevoort, Marjolein H.J.
AU - van Vliet, Michelle T.H.
AU - Vorogushyn, Sergiy
AU - Wagener, Thorsten
AU - Wang, Yueling
AU - Wendt, Doris E.
AU - Wickham, Elliot
AU - Yang, Long
AU - Zambrano-Bigiarini, Mauricio
AU - Blöschl, Günter
AU - Di Baldassarre, Giuliano
N1 - Funding Information: The presented work was developed by the Panta Rhei Working Groups 'Changes in flood risk' and 'Drought in the Anthropocene' within the framework of the Panta Rhei Research Initiative of the International Association of Hydrological Sciences. We thank the Barcelona Cicle de l’Aigua S.A., Barcelona City Council, Environment Agency (United Kingdom), Länsförsäkringar Skåne, Steering Centre for Urban Flood Control Programme in HCMC (Vietnam), VA SYD and the West Berkshire Council (United Kingdom) for data. The work was partly undertaken under the framework of the following projects: Alexander von Humboldt Foundation Professorship endowed by the German Federal Ministry of Education and Research (BMBF); British Geological Survey’s Groundwater Resources Topic (core science funding); C3-RiskMed (no. PID2020-113638RB-C22), financed by the Ministry of Science and Innovation of Spain; Centre for Climate and Resilience Research (no. ANID/FONDAP/15110009); CNES, through the TOSCA GRANT SWHYM; DECIDER (BMBF, no. 01LZ1703G); Deltares research programme on water resources; Dutch Research Council VIDI grant (no. 016.161.324); FLOOD (no. BMBF 01LP1903E), as part of the ClimXtreme Research Network. Funding was provided by the Dutch Ministry of Economic Affairs and Climate; Global Water Futures programme of University of Saskatchewan; GlobalHydroPressure (Water JPI); HUMID project (no. CGL2017-85687-R, AEI/FEDER, UE); HydroSocialExtremes (ERC Consolidator Grant no. 771678); MYRIAD-EU (European Union’s Horizon 2020 research and innovation programme under grant agreement no. 101003276); PerfectSTORM (no. ERC-2020-StG 948601); Project EFA210/16 PIRAGUA, co-founded by ERDF through the POCTEFA 2014–2020 programme of the European Union; Research project nos. ANID/FSEQ210001 and ANID/NSFC190018, funded by the National Research and Development Agency of Chile; SECurITY (Marie Skłodowska-Curie grant agreement no. 787419); SPATE (FWF project I 4776-N, DFG research group FOR 2416); the UK Natural Environment Research Council-funded project Land Management in Lowland Catchments for Integrated Flood Risk Reduction (LANDWISE, grant no. NE/R004668/1); UK NERC grant no. NE/S013210/1 (RAHU) (W.B.); Vietnam National Foundation for Science and Technology Development under grant no. 105.06-2019.20.; and Vietnam National University–HCMC under grant no. C2018-48-01. D.M. and A. McKenzie publish with the permission of the Director, British Geological Survey. The views expressed in this paper are those of the authors and not the organizations for which they work. Funding Information: The presented work was developed by the Panta Rhei Working Groups 'Changes in flood risk' and 'Drought in the Anthropocene' within the framework of the Panta Rhei Research Initiative of the International Association of Hydrological Sciences. We thank the Barcelona Cicle de l’Aigua S.A., Barcelona City Council, Environment Agency (United Kingdom), Länsförsäkringar Skåne, Steering Centre for Urban Flood Control Programme in HCMC (Vietnam), VA SYD and the West Berkshire Council (United Kingdom) for data. The work was partly undertaken under the framework of the following projects: Alexander von Humboldt Foundation Professorship endowed by the German Federal Ministry of Education and Research (BMBF); British Geological Survey’s Groundwater Resources Topic (core science funding); C3-RiskMed (no. PID2020-113638RB-C22), financed by the Ministry of Science and Innovation of Spain; Centre for Climate and Resilience Research (no. ANID/FONDAP/15110009); CNES, through the TOSCA GRANT SWHYM; DECIDER (BMBF, no. 01LZ1703G); Deltares research programme on water resources; Dutch Research Council VIDI grant (no. 016.161.324); FLOOD (no. BMBF 01LP1903E), as part of the ClimXtreme Research Network. Funding was provided by the Dutch Ministry of Economic Affairs and Climate; Global Water Futures programme of University of Saskatchewan; GlobalHydroPressure (Water JPI); HUMID project (no. CGL2017-85687-R, AEI/FEDER, UE); HydroSocialExtremes (ERC Consolidator Grant no. 771678); MYRIAD-EU (European Union’s Horizon 2020 research and innovation programme under grant agreement no. 101003276); PerfectSTORM (no. ERC-2020-StG 948601); Project EFA210/16 PIRAGUA, co-founded by ERDF through the POCTEFA 2014–2020 programme of the European Union; Research project nos. ANID/FSEQ210001 and ANID/NSFC190018, funded by the National Research and Development Agency of Chile; SECurITY (Marie Skłodowska-Curie grant agreement no. 787419); SPATE (FWF project I 4776-N, DFG research group FOR 2416); the UK Natural Environment Research Council-funded project Land Management in Lowland Catchments for Integrated Flood Risk Reduction (LANDWISE, grant no. NE/R004668/1); UK NERC grant no. NE/S013210/1 (RAHU) (W.B.); Vietnam National Foundation for Science and Technology Development under grant no. 105.06-2019.20.; and Vietnam National University–HCMC under grant no. C2018-48-01. D.M. and A. McKenzie publish with the permission of the Director, British Geological Survey. The views expressed in this paper are those of the authors and not the organizations for which they work. Publisher Copyright: © 2022, The Author(s).
PY - 2022/8/4
Y1 - 2022/8/4
N2 - Risk management has reduced vulnerability to floods and droughts globally1,2, yet their impacts are still increasing3. An improved understanding of the causes of changing impacts is therefore needed, but has been hampered by a lack of empirical data4,5. On the basis of a global dataset of 45 pairs of events that occurred within the same area, we show that risk management generally reduces the impacts of floods and droughts but faces difficulties in reducing the impacts of unprecedented events of a magnitude not previously experienced. If the second event was much more hazardous than the first, its impact was almost always higher. This is because management was not designed to deal with such extreme events: for example, they exceeded the design levels of levees and reservoirs. In two success stories, the impact of the second, more hazardous, event was lower, as a result of improved risk management governance and high investment in integrated management. The observed difficulty of managing unprecedented events is alarming, given that more extreme hydrological events are projected owing to climate change3.
AB - Risk management has reduced vulnerability to floods and droughts globally1,2, yet their impacts are still increasing3. An improved understanding of the causes of changing impacts is therefore needed, but has been hampered by a lack of empirical data4,5. On the basis of a global dataset of 45 pairs of events that occurred within the same area, we show that risk management generally reduces the impacts of floods and droughts but faces difficulties in reducing the impacts of unprecedented events of a magnitude not previously experienced. If the second event was much more hazardous than the first, its impact was almost always higher. This is because management was not designed to deal with such extreme events: for example, they exceeded the design levels of levees and reservoirs. In two success stories, the impact of the second, more hazardous, event was lower, as a result of improved risk management governance and high investment in integrated management. The observed difficulty of managing unprecedented events is alarming, given that more extreme hydrological events are projected owing to climate change3.
UR - http://www.scopus.com/inward/record.url?scp=85135317182&partnerID=8YFLogxK
U2 - 10.1038/s41586-022-04917-5
DO - 10.1038/s41586-022-04917-5
M3 - Article
C2 - 35922501
AN - SCOPUS:85135317182
SN - 0028-0836
VL - 608
SP - 80
EP - 86
JO - Nature
JF - Nature
IS - 7921
ER -