Abstract
Through the financial support of a recent project by an international foundation, lahar monitoring was initiated in the upper Jamapa watershed, located on the northern flank of the Pico de Orizaba volcano, inside the Pico de Orizaba National Park, where historically and also recently the occurrence of this type of phenomenon took place. The implementation of this system, focused on the monitoring, study, and later also the warning of lahars, implies the acquisition of multiparametric data, among which hydrometeorological, seismic and visual data are included. As it is a system that will fulfill the warning function, the data must be available in real-time at the monitoring center of the Seismological and Volcanological Observatory of Veracruz (Xalapa) for its storage, processing, and timely evaluation. To this end, a local telemetry network has been implemented that, in the first instance, obtains the data from the instruments at the sites of interest and subsequently proceeds to concentrate all of them at a point that houses the POHV permanent seismic monitoring station of Pico de Orizaba volcano, which represents a suitable site to transmit all the information generated by this network to the city of Xalapa.
References
Capra, L., Coviello, V., Borselli, L., Márquez-Ramírez, V.H., Arámbula-Mendoza, R. (2018) Hydrological control of large hurricane-induced lahars: evidences from rainfall, seismic and video monitoring: Natural Hazards and Earth System Sciences, 18, 781–794, https://doi.org/10.5194/nhess-2017-354
Chiarle M, Iannotto S, Martara G, Deline, P (2007) Recent debris flow occurrences associated with glaciers in the Alps. Global and Planetary Change, 56, 123-136.
Emanuel K (2021) Response of Global Tropical Cyclone Activity to Increasing CO2: Results from downscaling CMIP6 Models. Am Meteor Soc. DOI: 10.1175/JCLI-D-20-0367.1
Lauer, W., Klaus, D. (1975). Geoecological investigations on the timberline of Pico de Orizaba Mexico. Arctic and Alpine Research, pp. 315-330.Lavigne, F., Thouret, J.C. (2000). Les lahars: depots, origins et dynamique. Bull Soc geol France 171 545-557.
Lorenzo JL (1964) Los Glaciares de Mexico, UNAM, Instituto de Geofisica, 114.
Marta, S.; Azzoni, R.S.; Fugazza, D.; Tielidze, L.; Chand, P.; Sieron, K.; Almond, P.; Ambrosini, R.; Anthelme, F.; Alviz Gazitúa, P.; Bhambri, R.; Bonin, A.; Caccianiga, M.; Cauvy-Fraunié, S.; Ceballos Lievano, J.L.; Clague, J.; Cochachín Rapre, J.A.; Dangles, O.; Deline, P.; Eger, A.; Cruz Encarnación, R.; Erokhin, S.; Franzetti, A.; Gielly, L.; Gili, F.; Gobbi, M.; Guerrieri, A.; Hågvar, S.; Khedim, N.; Kinyanjui, R.; Messager, E.; Morales-Martínez, M.A.; Peyre, G.; Pittino, F.; Poulenard, J.; Seppi, R.; Chand Sharma, M.; Urseitova, N.; Weissling, B.; Yang, Y.; Zaginaev, V.; Zimmer, A.; Diolaiuti, G.A.; Rabatel, A.; Ficetola, G.F. The Retreat of Mountain Glaciers since the Little Ice Age: A Spatially Explicit Database. Data 2021, 6, 107. https://doi.org/10.3390/data6100107
Morales-Martínez, M.A., Welsh Rodríguez, C.M., Ruelas Monjardín, L.C., Weissling, B., Sieron, K, Ochoa Martínez, C.A, (2016). Afectaciones por posible asociación de eventos hidrometeorológicos y geológicos en los municipios de Calcahualco y Coscomatepec, Veracruz. Teoría y Praxis, octubre, pp. 31-49, Universidad de Quintana Roo Cozumel, México.
Naranjo, J.L., Sigurdsson, H., Carey, S.N., Fritz, W. (1986). Eruption of the Nevado del Ruiz volcano, Colombia, on 13 November 1985: tephra fall and lahars. Science, 233(4767), 961-963.
Newhall, C.G., Punongbayan, R.S. (eds) (1997). Fire and Mud: eruptions and Lahars of Mount Pinatubo, Philippines. Univ Washington Pr, 1126.
Palacios, D., y Vázquez-Selem, L. (1996). Geomorphic Effects of the Retreat of Jamapa Glacier, Pico de Orizaba Volcano (Mexico). Geografiska Annaler. Series A, Physical Geography, 78(1), 19-34.
Palacios, D., Parrilla, G., y Zamorano, J.J. (1999). Paraglacial and postglacial debris flows on a Little Ice Age terminal moraine: Jamapa Glacier, Pico de Orizaba (Mexico). Geomorphology, 28(1-2), 95-118.
Rodolfo, K. S. (1989). Origin and early evolution of lahar channel at Mabinit, Mayon Volcano, Philippines. Geological Society of America Bulletin, 101(3), 414-426.
Rodríguez, E.S., Mora-González I, Murrieta-Hernández JL (2006) Flujos de baja concentración asociados con lluvias de intensidad extraordinaria en el flanco sur del volcán Pico de Orizaba (Citlaltépetl), México. Boletín de la Sociedad Geológica Mexicana, LVIII(2), 223-236. Sociedad Geológica Mexicana, A.C.
Smith, G.A., Lowe, D.R. (1991). Lahars: volcano-hydrologic events and deposition in the debris flow-hyperconcentrated flow continuum. Sedimentation in Volcanic Settings Soc Sed Geol Spec Pub (SEPM) 45, DOI: 10.2110/pec.91.45.0059
Smith, G.A., Fritz, W.J. (1989). Volcanic influences on terrestrial sedimentation. Geology, 17(4), 375-376.
Sieron, K., Weissling, B., Morales-Martínez, M.A., Terán S. (2021). Reconstruction of the upper slope conditions of an extraordinary hydro-meteorological event along the Jamapa glacier drainage system, Citlaltépetl (Pico de Orizaba) volcano, Mexico. Frontiers in Earth Sciences, doi: 10.3389/feart.2021.668266
Thouret, J.C. y Lavigne, F. (2000). Lahars: occurrence, deposits and behaviour of volcano-hydrologic flows. Volcaniclastic rocks from magma to sediments. Gordon and Breach Science Publishers, 151-174.
Vallance, J. W., & Iverson, R. M. (2015). Lahars and their deposits. In The encyclopedia of volcanoes (pp. 649-664). Academic Press.
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
Copyright (c) 2022 Dra. Katrin Sieron , Francisco Córdoba Montiel, José Daniel Hernández Ventura , Marco Aurelio Morales Martínez , Juan Carlos Salinas Santillán , Luis Enrique Córdoba Soriano , Marian Victoria Hernández Ramírez , Osvaldo Gutiérrez López , Blake Weissling , Edwin Ulices Monfil León