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Governance struggles and policy processes: A comparison of earthquake risk
reduction in Nepal and Bihar, India
9 December, Monday 1pm-2pm
Institute of Hazard, Risk and Resilience, Durham University
In this presentation we share some preliminary findings on the national level governance landscape of earthquake risk reduction in Nepal and Bihar State in India. Located along the Himalayan Arc, Nepal and Bihar are both highly susceptible to earthquake hazard and were both affected by the 1934 earthquake. Despite the shared earthquake hazard, and some similarities in terms of ethnic and caste based inequalities and conflict, they have very different political and economic histories. Nepal is emerging from a recent conflict and receives relatively high levels of development aid while Bihar has a strong state system and is now making rapid economic progress after decades of stalled development due to weak governance. They therefore make for an interesting comparison in earthquake risk governance. In-depth interviews with over 40 stakeholders were conducted and focus groups were held to map out stakeholder relationships, interests and challenges of earthquake risk governance. Read the rest of this entry »
Durham postgraduate researcher Hanna Ruszczyk has been awarded a PhD fellowship for her research on community resilience and earthquakes.
Hanna’s postgraduate award has been made possible thanks to a generous gift from a Durham alumnus. Hanna’s research, will investigate the role of resilience in disaster risk reduction. She will study how resilience strategies can be operationalised within urban communities vulnerable to seismic hazards in Nepal and Bihar, India. Her PhD programme is based in the Department of Geography, linked to IHRR and is supervised by Dr Katie Oven and Dr Colin MacFarlane.
For her PhD, Ruszczyk is making a comparative analysis between Nepal and Bihar, which will investigate how to build individual and community level capacity for resilience. Both have their own particular strengths and weaknesses when it comes to adapting and building resilience to natural hazards. ‘I’m looking at how they can learn from each other’, said Ruszczyk. ‘There is a clear social element of resilience, but what are the most important components of resilience to be aware of?’, she asks. Read the rest of this entry »
Regular readers will know that the lack of attention that is paid to potential and actual landslide impacts during earthquakes in upland areas is a real hobby-horse of mine. Time and again we see the situation in which there is a lack of preparedness for landslides, causing huge disruption to the response and recovery operations, even though the threat was entirely forseeable. It is pleasing to see increased interest in the science of this issue in recent years, with a succession of good papers exploring both the mechanics of the landslide process (which is a very complex problem) and the likely occurrence of landslides.
This week, a paper has been electronically released on the BSSA website, to appear in a forthcoming edition of the journal, which examines the likely impact of landslides in the event of a Mw=7.0 earthquake of a “Seattle earthquake” – i.e. a quake on the Seattle Fault in Seattle, Washington. The paper, Allstadt et al. (2013) uses synthetic broadband seismograms to model shallow landslides in the area likely toi be affected by such an earthquake. Such an analysis is complex and computationally extremely intensive. I should also note that the technique uses the so-called Newmark method to model the slope behaviour. Newmark is basically the best technique that we have at our disposal at present, and so the team were right to do this, but in my view it is somewhat deficient in terms of the ways in which it models slope behaviour. We need a better technique; the trouble is that at the moment we do not have one. Read the rest of this entry »
Wednesday of next week will mark the 50th anniversary of the Vajont disaster, which occurred on 9th October 1963. This was of course the worst landslide disaster in European history. In addition it marked a watershed in a number of areas, not least landslide management and the development of large dams. On Thursday Michele and I will set off from the UK to attend the conference to mark the anniversary – the organisers were kind enough to invite me to give one of the keynote addresses, which will be on the topic of fatal landslides and large dams over the last decade. I will make it available online in due course.
In the meantime, I thought it would be useful to provide a list of some of the key resources that are available on the dam and the landslide disaster: Read the rest of this entry »
4th October 2013, 14:00 to 15:00, Seminar Room 010, Dept of Geography, Dr Md. Nadiruzzaman, United Nations University (MRF-UNU) Project
Population movements following an environmental stress can be a huge development challenge if we do not know where people are going and at what number. Without knowledge of the locations of affected people, relief assistance is compromised. No rapid and accurate method exists to track population movements after disasters. This research learns lessons from Haiti and plans to use CDR (call data record) from the Grameen Phone, the largest cellphone operator in Bangladesh, to estimate the magnitude and trends of population movements following the Cyclone Mohasen, which swept across Bangladesh on the 20th May 2013.
Geographic positions of SIM cards were determined by the location of the mobile phone tower through which each SIM card connects when calling. We will follow daily positions of SIM cards for Barisal and Chittagang Division from 01 April to 30 June of 2013. To exclude inactivated SIM cards, we will include SIM cards that made at least one call during the time of our study. Results from the Haiti study suggest that estimates of population movements during disasters and outbreaks can be delivered rapidly and with potentially high validity in areas with high mobile phone use. This research would offer new ways to understand population movements and climate change threshold.