Cite
The use of Numerical Weather Prediction and a Lagrangian transport (NAME-III) and dispersion (ASHFALL) models to explain patterns of observed ash deposition and dispersion following the August 2012 Te Maari, New Zealand eruption.
MLA
Turner, Richard, et al. “The Use of Numerical Weather Prediction and a Lagrangian Transport (NAME-III) and Dispersion (ASHFALL) Models to Explain Patterns of Observed Ash Deposition and Dispersion Following the August 2012 Te Maari, New Zealand Eruption.” Journal of Volcanology & Geothermal Research, vol. 286, Oct. 2014, pp. 437–51. EBSCOhost, https://doi.org/10.1016/j.jvolgeores.2014.05.017.
APA
Turner, R., Moore, S., Pardo, N., Kereszturi, G., Uddstrom, M., Hurst, T., & Cronin, S. (2014). The use of Numerical Weather Prediction and a Lagrangian transport (NAME-III) and dispersion (ASHFALL) models to explain patterns of observed ash deposition and dispersion following the August 2012 Te Maari, New Zealand eruption. Journal of Volcanology & Geothermal Research, 286, 437–451. https://doi.org/10.1016/j.jvolgeores.2014.05.017
Chicago
Turner, Richard, Stuart Moore, Natalia Pardo, Gabor Kereszturi, Michael Uddstrom, Tony Hurst, and Shane Cronin. 2014. “The Use of Numerical Weather Prediction and a Lagrangian Transport (NAME-III) and Dispersion (ASHFALL) Models to Explain Patterns of Observed Ash Deposition and Dispersion Following the August 2012 Te Maari, New Zealand Eruption.” Journal of Volcanology & Geothermal Research 286 (October): 437–51. doi:10.1016/j.jvolgeores.2014.05.017.