Lahar flow simulations using LAHARZ program: Application for the Popocatépetl volcano, Mexico

Munoz-Salinas, E., Castillo-Rodríguez, M., Manea, V., Manea, M. and Palacios, D. (2009) Lahar flow simulations using LAHARZ program: Application for the Popocatépetl volcano, Mexico. Journal of Volcanology and Geothermal Research, 182(1-2), pp. 13-22. (doi: 10.1016/j.jvolgeores.2009.01.030)

Full text not currently available from Enlighten.

Publisher's URL: http://dx.doi.org/10.1016/j.jvolgeores.2009.01.030

Abstract

Lahars are a type of catastrophic event that is generated in volcanic environments. Due to the recent technological advances computer simulated models have become widely used by the scientific community to predict the distribution of catastrophic events, such as floods, debris avalanches, earth landslides or lahars, and to mitigate possible damage to populations located in a risk area. Our study risk area is located in the Popocatépetl volcano, a large and active stratovolcano in the Trans Mexican Volcanic Belt. Here, lahars have been occurring during the last century, and some of them have seriously affected nearby towns. Since one of the main input parameters into a lahar simulation is the Digital Elevation Model (DEM), this paper focuses on studying lahar simulations on Popocatépetl using DEMs obtained from various sources with the aid of a popular package known as LAHARZ. The first simulations were performed using a 1:50,000 topographic map with 20-m contours interval. The second set of tests used an enhanced DEM with profiles measured during fieldwork in the lahar channel. In the last set of tests, we added lateral artificial barriers to the channel profiles used in the previous enhanced DEM. Our results show that the use of high resolution and detailed DEMs does not necessarily guarantee a realistic lahar simulation as was previously thought, and a detailed explanation as to why the LAHARZ code computation creates ragged edges is offered. Our results also offer useful information on the level of detail necessary for an input DEM into LAHARZ in order to obtain lahar simulations closer to real lahars. The minimum resolution for the DEM used in simulations must be less than the width of the narrowest cross-section of the channel to realistically reproduce the lahars. For DEMs with lower resolution, sometimes the modeled lahars are shorter in length, and therefore underestimate real hazards to populations. Also, the results show that lateral barriers are sometimes needed to obtain more realistic inundation areas.

Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Munoz-Salinas, Dr Esperanza
Authors: Munoz-Salinas, E., Castillo-Rodríguez, M., Manea, V., Manea, M., and Palacios, D.
Subjects:Q Science > QE Geology
College/School:College of Science and Engineering > School of Geographical and Earth Sciences
Journal Name:Journal of Volcanology and Geothermal Research
ISSN:0377-0273
ISSN (Online):1872-6097
Published Online:15 February 2009

University Staff: Request a correction | Enlighten Editors: Update this record