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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Online Access: | https://doi.org/10.1515/jlecol-2015-0006 |
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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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1717767987920896000 |