Transforming Development and Disaster Risk

Abstract: This article focuses on the complex relationship between development and disaster risk. Development and disaster risk are closely linked as the people and assets exposed to risk, as well as their vulnerability and capacity, are largely determined by development processes. Transformation is key to moving from current development patterns that increase, create or unfairly distribute risks, to forms of development that are equitable, resilient and sustainable. Based on a review of existing literature, we present three opportunities that have the potential to lead to transformation in the development-disaster risk relationship: (i) exposing development-disaster risk trade-offs in development policy and decision-making; (ii) prioritizing equity and social justice in approaches to secure resilience; and (iii) enabling transformation through adaptive governance. This research aims to contribute to breaking down existing barriers in research, policy and practice between the disaster risk reduction, climate change adaptation, and development communities by providing cross-sectoral opportunities to operationalize theoretical knowledge on transformation. It also helps to clarify the connections between different global agendas by positioning transformation as a potential bridging concept to link disconnected policy processes. This paper argues for empirical research to test the opportunities presented here and further define transformative pathways at multiple scales

Single-Turnover Variable Chlorophyll Fluorescence as a Tool for Assessing Phytoplankton Photosynthesis and Primary Productivity: Opportunities, Caveats and Recommendations

Phytoplankton photosynthetic physiology can be investigated through single-turnover variable chlorophyll fluorescence (ST-ChlF) approaches, which carry unique potential to autonomously collect data at high spatial and temporal resolution. Over the past decades, significant progress has been made in the development and application of ST-ChlF methods in aquatic ecosystems, and in the interpretation of the resulting observations. At the same time, however, an increasing number of sensor types, sampling protocols, and data processing algorithms have created confusion and uncertainty among potential users, with a growing divergence of practice among different research groups. In this review, we assist the existing and upcoming user community by providing an overview of current approaches and consensus recommendations for the use of ST-ChlF measurements to examine in-situ phytoplankton productivity and photo-physiology. We argue that a consistency of practice and adherence to basic operational and quality control standards is critical to ensuring data inter-comparability. Large datasets of inter-comparable and globally coherent ST-ChlF observations hold the potential to reveal large-scale patterns and trends in phytoplankton photo-physiology, photosynthetic rates and bottom-up controls on primary productivity. As such, they hold great potential to provide invaluable physiological observations on the scales relevant for the development and validation of ecosystem models and remote sensing algorithms

Tsunami hazard assessment of coastal South Africa based on mega-earthquakes of remote subduction zones

After the mega-earthquakes and concomitant devastating tsunamis in Sumatra (2004) and Japan (2011), we launched an investigation into the potential risk of tsunami hazard to the coastal cities of South Africa. This paper presents the analysis of the seismic hazard of seismogenic sources that could potentially generate tsunamis, as well as the analysis of the tsunami hazard to coastal areas of South Africa. The subduction zones of Makran, South Sandwich Island, Sumatra, and the Andaman Islands were identified as possible sources of mega-earthquakes and tsunamis that could affect the African coast. Numerical tsunami simulations were used to investigate the realistic and worst-case scenarios that could be generated by these subduction zones. The simulated tsunami amplitudes and run-up heights calculated for the coastal cities of Cape Town, Durban, and Port Elizabeth are relatively small and therefore pose no real risk to the South African coast. However, only distant tsunamigenic sources were considered and the results should therefore be viewed as preliminary.The Nuclear Structural Engineering (Pty) and the National Research Foundation through the Technology and Human Resources for Industry Programme project (THRIP) TP2011061400009.https://link.springer.com/journal/242019-04-01hj2018Geolog

East Anglia's crumbling coastline : are offshore breakwaters the answer?

During the storm surge of the 31 January and 1 February 1953 more than 300 people in eastern England lost their lives. At Sea Palling in Norfolk, the surge breached the sand dunes and resulted in the death of seven people. Similar events of catastrophic tidal flooding have been recorded since medieval times and numerous coastal villages have been lost to the sea. Storm surges have played an important role in the evolution of the East Anglian coastline throughout the historical period, and large-scale morphological changes can be caused by a single storm. In north Norfolk, for example, over a threeyear period more than 50 per cent of the net cliff erosion was observed to have occurred during a singlg storm surge.5 page(s

'We all knew that a cyclone was coming' : disaster preparedness and the cyclone of 1999 in Orissa, India

Imagine that a cyclone is coming, but that those living in the affected areas do nothing or too little to protect themselves. This is precisely what happened in the coastal state of Orissa, India. Individuals and communities living in regions where natural hazards are a part of daily life develop strategies to cope with and adapt to the impacts of extreme events. In October 1999, a cyclone killed 10,000 people according to government statistics, however, the unofficial death toll is much higher. This article examines why such a large loss of life occurred and looks at measures taken since then to initiate comprehensive disaster-preparedness programmes and to construct more cyclone shelters. The role of both governmental organisations and NGOs in this is critically analysed. The good news is that, based on an assessment of disaster preparedness during a small cyclone in November 2002, it can be seen that at community-level awareness was high and that many of the lessons learnt in 1999 were put into practice. Less positive, however, is the finding that at the state level collaboration continues to be problematic.15 page(s

Resilience in the context of tsunami early warning systems and community disaster preparedness in the Indian Ocean Region

17 page(s

The Role of Collective Action in Enhancing Communities’ Adaptive Capacity to Environmental Risk: An Exploration of Two Case Studies from Asia

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