COOKIES: By using this website you agree that we can place Google Analytics Cookies on your device for performance monitoring. |
University of Cambridge > Talks.cam > Institute for Energy and Environmental Flows (IEEF) > The 2010 Eruption of Eyjafjallajökull: Interaction between volcanic plumes and the wind and consequences for modelling airborne ash hazard to aviation
The 2010 Eruption of Eyjafjallajökull: Interaction between volcanic plumes and the wind and consequences for modelling airborne ash hazard to aviationAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact Catherine Pearson. The 2010 eruption of Eyjafjallajökull caused a paradigm shift in the importance of small volcanic eruptions to commercial aviation and societal infrastructure. The atmospheric wind dispersed fine volcanic ash at low levels over Northern Europe, resulting in closure of airspace for six days and estimated direct losses in excess of 1 Billion €. In this talk I will summarise the consequences of volcanic ash injection into the atmosphere for aviation, the role of Volcanic Ash Advisory Centres (VAAC) in forecasting ash hazard, and the inputs required for their dispersion modelling. I will then present a predictive model of volcanic plumes that describes the bending over of the plume trajectory in a cross-wind and show that model predictions are in accord with a dataset of historic eruptions if the profile of atmospheric wind shear is described. The wind restricts the rise height of volcanic plumes, such that an order of magnitude increase in source mass flux is required to match the rise height of a plume in a quiescent environment. This effect can lead to significant under-prediction of the mass of volcanic ash input into VAAC dispersion modelling. The model can account for the variations in plume height observed during the first explosive phase of the 2010 Eyjafjallajökull eruption using independently measured wind speeds, and this suggests that changes in the observed plume height are better explained by changing meteorology than abrupt changes in the source mass flux. This talk is part of the Institute for Energy and Environmental Flows (IEEF) series. This talk is included in these lists:
Note that ex-directory lists are not shown. |
Other listsExploring modern South Asian history with visual research methods: theories and practices euroscicon Language Technology Lab Seminars cambridge advanced imaging Pragmatics reading group Clinical Ethics ForumOther talksAnimal Migration Leveraging the imaging power of the Beacon platform Regulators of Muscle Stem Cell Fate and Function Diagnosing diseases of childhood: a bioarchaeological and palaeopathological perspective The homelands of the plague: Soviet disease ecology in Central Asia, 1920s–1950s Computational Neuroscience Journal Club Atiyah Floer conjecture Statistical Methods in Pre- and Clinical Drug Development: Tumour Growth-Inhibition Model Example Computing High Resolution Health(care) A transmissible RNA pathway in honeybees Thermodynamics de-mystified? /Thermodynamics without Ansätze? CANCELLED Jennifer Luff: Secrets, Lies, and the 'Special Relationship' in the Early Cold War |