Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption

In this paper we analyzed the 2011-2012 eruption of Nyamulagira volcano using MODIS Data. Eruptions have been occurring every 3–4 years throughout the last century. Satellite infrared data, collected by MODIS sensor to estimate pixels thermal anomaly of hot spots were analized, the radiance emitted...

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Main Authors: Bagalwa Montfort, Karume Katcho
Format: Article
Language:English
Published: Sciendo 2015-01-01
Series:Journal of Landscape Ecology
Subjects:
Online Access:https://doi.org/10.1515/jlecol-2015-0006
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spelling doaj-23ce0ff9a8484d448cc63a6cc67f2c302021-09-06T19:40:40ZengSciendoJournal of Landscape Ecology1805-41962015-01-018152110.1515/jlecol-2015-0006jlecol-2015-0006Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruptionBagalwa Montfort0Karume Katcho1Department of Geodesy, Goma Volcano Observatory, Goma, North Kivu, D.R.CongoDepartment of Geodesy, Goma Volcano Observatory, Goma, North Kivu, D.R.CongoIn this paper we analyzed the 2011-2012 eruption of Nyamulagira volcano using MODIS Data. Eruptions have been occurring every 3–4 years throughout the last century. Satellite infrared data, collected by MODIS sensor to estimate pixels thermal anomaly of hot spots were analized, the radiance emitted at 3,959 and 12.02μm for each pixel and the thermal emissions at Nyamulagira feall into three distinct radiating regimes released during the 2011–2012 eruption. Initial activity was detected on 6 November, at 19:55 UTC, with a large thermal anomaly with 28 pixels approximately on the north flank of the volcano. The anomaly was limited to the north flank. The anomaly reached a maximum size of 1188 pixels in January 2012. The size and intensity of the anomaly rapidly diminished to first April 2012 were no more than 2 piixels indicate the end of eruption.https://doi.org/10.1515/jlecol-2015-0006nyamuragira volcano modis, thermal anomalies pixel, hot spot volcanic radiative power thermal regimeseffusive trends
collection DOAJ
language English
format Article
sources DOAJ
author Bagalwa Montfort
Karume Katcho
spellingShingle Bagalwa Montfort
Karume Katcho
Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
Journal of Landscape Ecology
nyamuragira volcano
modis, thermal anomalies
pixel, hot spot
volcanic radiative power
thermal regimes
effusive trends
author_facet Bagalwa Montfort
Karume Katcho
author_sort Bagalwa Montfort
title Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
title_short Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
title_full Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
title_fullStr Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
title_full_unstemmed Monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
title_sort monitoring and analysis of nyamulagira volcano activity using modis data: case of the 2011-2012 eruption
publisher Sciendo
series Journal of Landscape Ecology
issn 1805-4196
publishDate 2015-01-01
description In this paper we analyzed the 2011-2012 eruption of Nyamulagira volcano using MODIS Data. Eruptions have been occurring every 3–4 years throughout the last century. Satellite infrared data, collected by MODIS sensor to estimate pixels thermal anomaly of hot spots were analized, the radiance emitted at 3,959 and 12.02μm for each pixel and the thermal emissions at Nyamulagira feall into three distinct radiating regimes released during the 2011–2012 eruption. Initial activity was detected on 6 November, at 19:55 UTC, with a large thermal anomaly with 28 pixels approximately on the north flank of the volcano. The anomaly was limited to the north flank. The anomaly reached a maximum size of 1188 pixels in January 2012. The size and intensity of the anomaly rapidly diminished to first April 2012 were no more than 2 piixels indicate the end of eruption.
topic nyamuragira volcano
modis, thermal anomalies
pixel, hot spot
volcanic radiative power
thermal regimes
effusive trends
url https://doi.org/10.1515/jlecol-2015-0006
work_keys_str_mv AT bagalwamontfort monitoringandanalysisofnyamulagiravolcanoactivityusingmodisdatacaseofthe20112012eruption
AT karumekatcho monitoringandanalysisofnyamulagiravolcanoactivityusingmodisdatacaseofthe20112012eruption
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