Challenges in the attribution of river flood events

Paolo Scussolini, Linh Nhat Luu, Sjoukje Philip, Wouter R. Berghuijs, Dirk Eilander, Jeroen C. J. H. Aerts, Sarah F. Kew, Geert Jan van Oldenborgh, Willem H. J. Toonen, Jan Volkholz, Dim Coumou
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Abstract

Advances in the field of extreme event attribution allow to estimate how anthropogenic global warming affects the odds of individual climate disasters, such as river floods. Extreme event attribution typically uses precipitation as proxy for flooding. However, hydrological processes and antecedent conditions make the relation between precipitation and floods highly nonlinear. In addition, hydrology acknowledges that changes in floods can be strongly driven by changes in land-cover and by other human interventions in the hydrological system, such as irrigation and construction of dams. These drivers can either amplify, dampen or outweigh the effect of climate change on local flood occurrence. Neglecting these processes and drivers can lead to incorrect flood attribution. Including flooding explicitly, that is, using data and models of hydrology and hydrodynamics that can represent the relevant hydrological processes, will lead to more robust event attribution, and will account for the role of other drivers beyond climate change. Existing attempts are incomplete. We argue that the existing probabilistic framework for extreme event attribution can be extended to explicitly include floods for near-natural cases, where flood occurrence was unlikely to be influenced by land-cover change and human hydrological interventions. However, for the many cases where this assumption is not valid, a multi-driver framework for conditional event attribution needs to be established. Explicit flood attribution will have to grapple with uncertainties from lack of observations and compounding from the many processes involved. Further, it requires collaboration between climatologists and hydrologists, and promises to better address the needs of flood risk management.

Abstract Image

河流洪水事件归因方面的挑战
极端事件归因领域取得的进展有助于估算全球人为变暖如何影响个别气候灾害(如河流洪水)的发生几率。极端事件归因通常使用降水量来代表洪水。然而,水文过程和先决条件使得降水和洪水之间的关系高度非线性。此外,水文学认为,土地覆盖的变化和人类对水文系统的其他干预(如灌溉和修建水坝)也会对洪水的变化产生强烈的推动作用。这些驱动因素可以放大、抑制或抵消气候变化对当地洪水发生的影响。忽视这些过程和驱动因素会导致错误的洪水归因。将洪水明确包括在内,即使用能够代表相关水文过程的水文和流体力学数据和模型,将导致更可靠的事件归因,并将考虑气候变化以外的其他驱动因素的作用。现有的尝试并不全面。我们认为,现有的极端事件归因概率框架可以扩展到明确包括近自然情况下的洪水,在这种情况下,洪水的发生不太可能受到土地覆盖变化和人类水文干预的影响。然而,在许多情况下,这一假设是不成立的,因此需要建立一个多驱动因素的条件事件归因框架。明确的洪水归因必须解决因缺乏观测数据而产生的不确定性,以及因涉及众多过程而产生的复杂性。此外,它还需要气候学家和水文学家之间的合作,并有望更好地满足洪水风险管理的需要。
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