scholarly journals How Venice and Miami are adapting to sea-level rise

2018 ◽  
Author(s):  
OCTO

The authors describe governance approaches to sea-level rise (SLR) adopted by the large, coastal cities of Venice, Italy, and Miami, Florida, USA -- offering advice on how each city could learn from the other. The authors, who work in these cities on the issue of SLR, were able to bring their own observations into this analysis alongside archival research and interviews with government officials, NGOs, and scientists.

2018 ◽  
Author(s):  
Emanuela Molinaroli ◽  
Stefano Guerzoni ◽  
Daniel Suman

Both Venice and Miami are highly vulnerable to sea level rise and climate change. We examine the two cities´ biophysical environments, their socioeconomic bases, the legal and administrative structures, and their vulnerabilities and responses to sea level rise and flooding. Based on this information we critically compare the different adaptive responses of Venice and Miami and suggest what each city may learn from the other, as well as offer lessons for other vulnerable coastal cities.


Water ◽  
2020 ◽  
Vol 12 (7) ◽  
pp. 1934
Author(s):  
Adrienne Fung ◽  
Roger Babcock

Collection systems in coastal cities are often below the groundwater table, leading to groundwater infiltration (GWI) through defects such as cracks and poor lateral connections. Climate-change-induced sea level rise (SLR) will raise groundwater levels, increasing the head and thus the inflow. A method has been developed to predict GWI when groundwater levels change using calibration with sewershed flow monitoring data. The calibration results in a parameter that characterizes the porosity of the collection system. A case study is presented for a coastal city with reliable flow monitoring data for eight days that resulted in a large range of effective defect sizes (minimum 0.0044 to maximum 0.338 radians), however, the range of predicted future GWI in currently submerged pipes varied by only 12% from the mean. The mean effective defect predicts 70 to 200% increases in GWI due to SLR of 0.3 to 0.9 m (1 to 3 ft), respectively, for currently submerged pipes. Predicted additional GWI for pipes that will become submerged due to SLR will increase GWI to values that approach or exceed the current average dry weather flow. This methodology can be used for planning of infrastructure improvements to enhance resiliency in coastal communities.


2020 ◽  
Vol 12 (1) ◽  
pp. 113-131 ◽  
Author(s):  
Patrick D. Nunn

Abstract As concern about sea level rise grows and optimal solutions are sought to address its causes and effects, little attention has been given to past analogs. This article argues that valuable insights into contemporary discussions about future sea level rise can be gained from understanding those of the past, specifically the ways in which coastal peoples and societies reacted during the period of postglacial sea level rise. For much of the Holocene, most continental people eschewed coastal living in favor of inland areas. In many places large coastal settlements appeared only after the development of polities and associated crosswater networks. Postglacial sea level rise affected coastal living in ways about which we remain largely ignorant. Yet, millennia-old stories from Australia and northwest Europe show how people responded, from which we can plausibly infer their motivations. Stories from Australia say the people have succeeded in halting sea level rise, whereas those from northwest Europe indicate that people have failed, leading to the drowning of coastal cities such as Ys (Brittany) and Cantre’r Gwaelod (Wales). This distinction is explained by the contrasting duration of postglacial sea level rise in these regions; around Australia, sea level stopped rising 7,000 years ago, while along many coasts of northwest Europe it has risen unceasingly since the last ice age ended. The nature of past human and societal responses to postglacial sea level rise holds important insights for the future.


2019 ◽  
Vol 64 (4) ◽  
pp. 391-415 ◽  
Author(s):  
Emanuela Molinaroli ◽  
Stefano Guerzoni ◽  
Daniel Suman

2016 ◽  
Vol 60 (2) ◽  
pp. 249-265 ◽  
Author(s):  
Xinyu Fu ◽  
Mohammed Gomaa ◽  
Yujun Deng ◽  
Zhong-Ren Peng

2021 ◽  
Vol 41 (4) ◽  
Author(s):  
Patrick Boyden ◽  
Elisa Casella ◽  
Christopher Daly ◽  
Alessio Rovere

AbstractSea-level rise represents a severe hazard for populations living within low-elevation coastal zones and is already largely affecting coastal communities worldwide. As sea level continues to rise following unabated greenhouse gas emissions, the exposure of coastal communities to inundation and erosion will increase exponentially. These impacts will be further magnified under extreme storm conditions. In this paper, we focus on one of the most valuable coastal real estate markets globally (Palm Beach, FL). We use XBeach, an open-source hydro and morphodynamic model, to assess the impact of a major tropical cyclone (Hurricane Matthew, 2016) under three different sea-level scenarios. The first scenario (modern sea level) serves as a baseline against which other model runs are evaluated. The other two runs use different 2100 sea-level projections, localized to the study site: (i) IPCC RCP 8.5 (0.83 m by 2100) and (ii) same as (i), but including enhanced Antarctic ice loss (1.62 m by 2100). Our results show that the effective doubling of future sea level under heightened Antarctic ice loss amplifies flow velocity and wave height, leading to a 46% increase in eroded beach volume and the overtopping of coastal protection structures. This further exacerbates the vulnerability of coastal properties on the island, leading to significant increases in parcel inundation.


2021 ◽  
Vol 9 ◽  
Author(s):  
John W. Day ◽  
Joel D. Gunn ◽  
Joseph Robert Burger

The world is urbanizing most rapidly in tropical to sub-temperate areas and in coastal zones. Climate change along with other global change forcings will diminish the opportunities for sustainability of cities, especially in coastal areas in low-income countries. Climate forcings include global temperature and heatwave increases that are expanding the equatorial tropical belt, sea-level rise, an increase in the frequency of the most intense tropical cyclones, both increases and decreases in freshwater inputs to coastal zones, and increasingly severe extreme precipitation events, droughts, freshwater shortages, heat waves, and wildfires. Current climate impacts are already strongly influencing natural and human systems. Because of proximity to several key warming variables such as sea-level rise and increasing frequency and intensity of heatwaves, coastal cities are a leading indicator of what may occur worldwide. Climate change alone will diminish the sustainability and resilience of coastal cities, especially in the tropical-subtropical belt, but combined with other global changes, this suite of forcings represents an existential threat, especially for coastal cities. Urbanization has coincided with orders of magnitude increases in per capita GDP, energy use and greenhouse gas emissions, which in turn has led to unprecedented demand for natural resources and degradation of natural systems and more expensive infrastructure to sustain the flows of these resources. Most resources to fuel cities are extracted from ex-urban areas far away from their point of final use. The urban transition over the last 200 years is a hallmark of the Anthropocene coinciding with large surges in use of energy, principally fossil fuels, population, consumption and economic growth, and environmental impacts such as natural system degradation and climate change. Fossil energy enabled and underwrote Anthropocene origins and fueled the dramatic expansion of modern urban systems. It will be difficult for renewable energy and other non-fossil energy sources to ramp up fast enough to fuel further urban growth and maintenance and reverse climate change all the while minimizing further environmental degradation. Given these trajectories, the future sustainability of cities and urbanization trends, especially in threatened areas like coastal zones in low-income countries in the tropical to sub-tropical belt, will likely diminish. Adaptation to climate change may be limited and challenging to implement, especially for low-income countries.


Author(s):  
Amar Causevic ◽  
Matthew LoCastro ◽  
Dharish David ◽  
Sujeetha Selvakkumaran ◽  
Åsa Gren

Continued greenhouse gas emissions will lead to a rise in temperatures, accompanied by rising sea levels threatening low-lying coastal cities. This vulnerability is especially acute in developing countries’ cities. This study reviews whether Bangkok, Manila, and Jakarta, less prepared emerging urban centers of developing countries, are investing in adaptation projects for resilience against sea-level rise and urban flooding. Sea-level rise and urban flooding resilience projects were identified in the selected cities through secondary research methods, data on multilateral climate funds, and other aggregated funding databases such as Aid Atlas, Cities Adaptation Action, and City Risk Index. Our findings show that even though these cities do have some adaptation projects to address coastal flooding and rising sea-level threats, the funding has been disparate and dispersed due to a lack of continuous, sizeable, and diverse financing options and does not come close to the requirement, given the risks, of covering potential disaster-related losses. Our findings further highlight the need to expand financing beyond multilateral funds and bilateral funding agreements and to include financial mechanisms that incentivize potential stakeholders to invest in projects that ordinarily are considered nonrevenue generating.


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