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2015, Mitigation and Adaptation Strategies for Global Change
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8 pages
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Climate change significantly exacerbates flood risks due to increased extreme weather events and sea level rise, impacting millions globally, especially in flood-prone regions. The importance of both mitigation and adaptation strategies is highlighted, as effective global climate change mitigation remains elusive while adaptation to climate variability presents its own challenges. The paper aims to inspire diverse approaches to developing context-specific flood risk management strategies across varying socio-economic and geo-ecological settings.
Article 15a of the Dutch Law on authorship, sections of this publication may be quoted on the understanding that a clear reference is made to this publication. Liability The National Research Programme Knowledge for Climate and the authors of this publication have exercised due caution in preparing this publication. However, it can not be excluded that this publication may contain errors or is incomplete. Any use of the content of this publication is for the own responsibility of the user. The Foundation Knowledge for Climate (Stichting Kennis voor Klimaat), its organisation members, the authors of this publication and their organisations may not be held liable for any damages resulting from the use of this publication. Towards climate-change proof flood risk management Exploration of innovative measures for the Netherlands' adaptation policy inspired by experiences from abroad Interim report, full text Theme 1 Knowledge for Climate research programme
Hydrological Sciences Journal, 2013
A holistic perspective on changing rainfall-driven flood risk is provided for the late 20th and early 21st centuries. Economic losses from floods have greatly increased, principally driven by the expanding exposure of assets at risk. It has not been possible to attribute rain-generated peak streamflow trends to anthropogenic climate change over the past several decades. Projected increases in the frequency and intensity of heavy rainfall, based on climate models, should contribute to increases in precipitation-generated local flooding (e.g. flash flooding and urban flooding). This article assesses the literature included in the IPCC SREX report and new literature published since, and includes an assessment of changes in flood risk in seven of the regions considered in the
Unit for Social and Environmental Research, …, 2005
Flood estimation and flood management have traditionally been the domain of hydrologists, water resources engineers and statisticians, and disciplinary approaches have abound. Dominant views have been shaped; one example is the catchment perspective: floods are formed and influenced by the interaction of local, catchment-specific 5 characteristics, such as meteorology, topography and geology. These traditional views have been beneficial, but they have a narrow framing. In this paper we contrast traditional views with broader perspectives that are emerging from an improved understanding of the climatic context of floods. We conclude: (1) extending the traditional system boundaries (local catchment, recent decades, hydrological/hydraulic processes) opens 10 up exciting possibilities for better understanding and improved tools for flood risk assessment and management.
Despite continuing global debates over both the effects of greenhouse gases and mitigation of their effects, the risk is high that climate change will occur despite any response. Consequently, solutions will require both mitigating future damage and adapting to inevitable changes. Climate adaptation--finding ways to live with the consequences of global warming--will become increasingly important. Warmer average temperatures mean more energy in the atmospheric system, leading to more extreme and frequent weather events, increased effects of natural disasters, and changes to rainy seasons. Societies in both the developed and the developing world are not yet prepared to respond to these changes and have much to learn from each other.
Nature Climate Change, 2015
Understanding global future river flood risk is a prerequisite for the quantification of climate change impacts and planning e ective adaptation strategies 1. Existing global flood risk projections fail to integrate the combined dynamics of expected socioeconomic development and climate change. We present the first global future river flood risk projections that separate the impacts of climate change and socioeconomic development. The projections are based on an ensemble of climate model outputs 2 , socioeconomic scenarios 3 , and a state-of-the-art hydrologic river flood model combined with socioeconomic impact models 4,5. Globally, absolute damage may increase by up to a factor of 20 by the end of the century without action. Countries in Southeast Asia face a severe increase in flood risk. Although climate change contributes significantly to the increase in risk in Southeast Asia 6 , we show that it is dwarfed by the e ect of socioeconomic growth, even after normalization for gross domestic product (GDP) growth. African countries face a strong increase in risk mainly due to socioeconomic change. However, when normalized to GDP, climate change becomes by far the strongest driver. Both highand low-income countries may benefit greatly from investing in adaptation measures, for which our analysis provides a basis. Between 1980 and 2013, the global direct economic losses due to floods exceeded $1 trillion (2013 values), and more than 220,000 people lost their lives 7. Global flood damages have been increasing steeply over the past decades, so far mainly driven by steady growth in population and economic activities in flood-prone areas 8,9. Future increases in flood frequency and severity due to changes in extreme weather are expected 1,9. Such increasing trends in flood risk may have severe direct humanitarian and economic impacts and lasting long-term negative effects on economic growth 10,11. In 2015, several major international policies are being initiated or renewed that may catalyse flood risk adaptation and hence risk reduction, such as the Sustainable Development Goals, Conference of the Parties (COP) 21, and the Sendai Framework for Disaster Risk Reduction. Such efforts require global understanding of the drivers of flood risk change in the future. Past efforts to enhance this understanding have focused on the global-scale mapping of present-day flood hazard 12,13 and risk 4,5 and future changes in global flood exposure and risk 14 due to either climate change 6,15,16 or socioeconomic development 8,17. One recent study 18 combined global socioeconomic and climate change into future global flood risk projections for the first time, however, this work did not reveal regional patterns nor quantify the drivers of risk change. Furthermore, no study has so far accounted for installed and maintained flood protection standards (FPS; ref. 10).
Research Square (Research Square), 2021
Read Full License A Framework to Estimate Loss and Damage (L&D) to Floods in a Changing Climate, using Capital-based Approach 1. Introduction Floods are one of the frequent hydrological disasters, which have been becoming a severe menace to the mankind and environment (Wallemacq, 2018). According to (IPCC, 2012a) and EM-Dat, the International Disaster Database by Centre for Research on the Epidemiology of Disasters (CRED), flood is defined as the flow of water from a stream channel, or any other water bodies, in excess, of the normal, resulting in submerging of areas, which are dry otherwise. They are mainly caused by climate change, antecedent soil moisture, deforestation, and urbanization (Chang & Franczyk, 2008). Floods can be of various types-river (fluvial) floods, flash floods and surface water (pluvial) floods, coastal floods, urban floods, sewer floods, and glacial lake outburst floods (GLOF). With 43% of the disasters, globally, from 1998 to 2017, being floods, they have affected two billion people, and around 23% of the economic losses, worldwide , due to disasters, have been attributed to floods (Wallemacq, 2018). Floods are associated with mortality and morbidity effects like deaths due to drowning, physical trauma, electrocution, etc, and incidence of water and vector-borne diseases like diarrhoea, cholera, typhoid, dengue, malaria, etc. (Jonkman & Kelman, 2005; Doocy et al., 2013;World Health Organization, NA); mental health effects; disruption in provision of health care facilities, due to damage inflicted on physical infrastructure; and injuries during evacuation process (IPCC, 2007; World Health Organization, NA). Besides, they impact personal security through income losses; and inflict damage to their physical capital stock (H. Dewan, 2015; Tripathi, 2015; Paavola, 2017). Such flooding risks will exacerbate with the rising frequency and intensity of pluvial and river floods, in a changing climate (IPCC, 2012b; IPCC, 2021). Climate model simulations provide empirical evidences that climate change influences the frequency and intensity of floods, and is also projected to increase with increase in greenhouse warming, in future (Balica et al., 2012; Andersen & Shepherd, 2013; Cai et al., 2014). Besides, advective effects, indicated by changes in sea level pressure, due to changes in global air circulation also contribute to increased rainfall in northwestern and northeastern North America, northern Europe, northern Asia, east coast of Asia, southeastern Australia, and south-central South America (Meehl et al., 2005); and flooding risk increases especially in the mid-to-high latitudes (Trenberth, 2011). The relationship between an increase in sea surface temperature over tropical Indian Ocean and an increase in extreme rainfall events in a global warming scenario suggests an increase in flood risks in central India (Goswami et al., 2006; Rajeevan et al., 2008). A relatively greater increase in flood frequency is projected in the Indian subcontinent basins, under the low emission scenario of Representative Concentration Pathway (RCP) 2.6, as compared to RCP 8.5 (Al et al., 2019). Such increase in flood risks although, can be dealt with flood protection measures (Mishra et al., 2012), but, a shift has been suggested from flood protection to flood risk management approach (Garrote et al., 2019). However, such an approach will yet leave some residual flood losses, known as loss and damage to floods. This paper is organized as follows: Section 2 introduces the concept of loss and damage, its evolution, and its relevance in the context of floods. The existing methodologies for quantification of loss and damage, across literature, are discussed briefly in Section 3. Section 4 provides a proposed framework on estimation of residual "loss and damage (L&D)" to floods on the livelihood assets through the lens of the vulnerability context and the capital assets. 2. Loss and Damage-concept, history, and relevance in floods Climate extremes and disasters can neither be used interchangeably, nor there exist any one-to-one relationship between them (IPCC, 2012b). In other words, extreme events like floods pose serious threats to livelihoods,and alter the normal functioning of the prevailing physical, geographical and social conditions of the communities, if their occurrence is accompanied by exposure of communities to floods, and a high degree of vulnerability. It has been suggested that that even though binding mitigation actions can reduce greenhouse gases, yet, there are some residual impacts to which the world is already committed, viz. the sea level rise, frequent and intense cyclones, storm surges, etc., resulting in flooding; hence it is imperative to include adaptation along with mitigation in climate policy actions (IPCC, 2001; Stern, 2007). A host of adaptation measures aimed at reducing vulnerability play an important role in transforming climate extremes to disasters. However, there is a wide array of factors that impede implementation of
Natural Hazards and Earth System Science, 2014
Flood estimation and flood management have traditionally been the domain of hydrologists, water resources engineers and statisticians, and disciplinary approaches have abound. Dominant views have been shaped; one example is the catchment perspective: floods are formed and influenced by the interaction of local, catchment-specific 5 characteristics, such as meteorology, topography and geology. These traditional views have been beneficial, but they have a narrow framing. In this paper we contrast traditional views with broader perspectives that are emerging from an improved understanding of the climatic context of floods. We conclude: (1) extending the traditional system boundaries (local catchment, recent decades, hydrological/hydraulic processes) opens 10 up exciting possibilities for better understanding and improved tools for flood risk assessment and management.
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