Wildfire Intensity and Fire Emissions in Siberia

An analysis of fire characteristics in the boreal forests of Siberia (50–75° N, 60–140° E) was performed for the period 2002–2022. We found a positive trend in the proportion of high-intensity fires in dominant forest stands of Siberia based on long-term series of variations in the Fire Radiative Po...

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Published in:Fire
Main Authors: Evgenii I. Ponomarev, Andrey N. Zabrodin, Eugene G. Shvetsov, Tatiana V. Ponomareva
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/fire6070246
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spelling ftmdpi:oai:mdpi.com:/2571-6255/6/7/246/ 2023-08-20T04:04:49+02:00 Wildfire Intensity and Fire Emissions in Siberia Evgenii I. Ponomarev Andrey N. Zabrodin Eugene G. Shvetsov Tatiana V. Ponomareva agris 2023-06-22 application/pdf https://doi.org/10.3390/fire6070246 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/fire6070246 https://creativecommons.org/licenses/by/4.0/ Fire; Volume 6; Issue 7; Pages: 246 wildfires Siberia normalized burn ratio fire severity fire radiative power fire emissions Text 2023 ftmdpi https://doi.org/10.3390/fire6070246 2023-08-01T10:34:47Z An analysis of fire characteristics in the boreal forests of Siberia (50–75° N, 60–140° E) was performed for the period 2002–2022. We found a positive trend in the proportion of high-intensity fires in dominant forest stands of Siberia based on long-term series of variations in the Fire Radiative Power (FRP) measurements from the Moderate Resolution Imaging Spectroradiometer (MODIS). Our results showed that there was an increase in the proportion of areas of high-intensity fires over the past decade on about ~30% of the boreal forests of Siberia, including the Arctic zone. For the sample group of fires, the level of correlation (R2 = 0.80–0.94) between the fire impact, classified according to the NBR/dNBR technology, and the integral FRP values was revealed. The intensity of combustion in terms of FRP is associated with the volume of burned biomass and determines the dynamics of specific emissions values per unit area. The results suggest that further increase in fire emissions in Siberia will be determined not only by an increase of burned areas, but also by a redistribution of low- and high-intensity burning and an increase in specific emission values. Finally, we estimated that Siberian fires are responsible for about 5–20% of the total volume of greenhouse gas emissions in the Russian Federation, depending on the fire season scenario. The recurrence of extremely high emissions (296–350 Tg C/year) will make it possible to consider part of Siberian forests as a source of carbon in the nearest future. Text Arctic Siberia MDPI Open Access Publishing Arctic Fire 6 7 246
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic wildfires
Siberia
normalized burn ratio
fire severity
fire radiative power
fire emissions
spellingShingle wildfires
Siberia
normalized burn ratio
fire severity
fire radiative power
fire emissions
Evgenii I. Ponomarev
Andrey N. Zabrodin
Eugene G. Shvetsov
Tatiana V. Ponomareva
Wildfire Intensity and Fire Emissions in Siberia
topic_facet wildfires
Siberia
normalized burn ratio
fire severity
fire radiative power
fire emissions
description An analysis of fire characteristics in the boreal forests of Siberia (50–75° N, 60–140° E) was performed for the period 2002–2022. We found a positive trend in the proportion of high-intensity fires in dominant forest stands of Siberia based on long-term series of variations in the Fire Radiative Power (FRP) measurements from the Moderate Resolution Imaging Spectroradiometer (MODIS). Our results showed that there was an increase in the proportion of areas of high-intensity fires over the past decade on about ~30% of the boreal forests of Siberia, including the Arctic zone. For the sample group of fires, the level of correlation (R2 = 0.80–0.94) between the fire impact, classified according to the NBR/dNBR technology, and the integral FRP values was revealed. The intensity of combustion in terms of FRP is associated with the volume of burned biomass and determines the dynamics of specific emissions values per unit area. The results suggest that further increase in fire emissions in Siberia will be determined not only by an increase of burned areas, but also by a redistribution of low- and high-intensity burning and an increase in specific emission values. Finally, we estimated that Siberian fires are responsible for about 5–20% of the total volume of greenhouse gas emissions in the Russian Federation, depending on the fire season scenario. The recurrence of extremely high emissions (296–350 Tg C/year) will make it possible to consider part of Siberian forests as a source of carbon in the nearest future.
format Text
author Evgenii I. Ponomarev
Andrey N. Zabrodin
Eugene G. Shvetsov
Tatiana V. Ponomareva
author_facet Evgenii I. Ponomarev
Andrey N. Zabrodin
Eugene G. Shvetsov
Tatiana V. Ponomareva
author_sort Evgenii I. Ponomarev
title Wildfire Intensity and Fire Emissions in Siberia
title_short Wildfire Intensity and Fire Emissions in Siberia
title_full Wildfire Intensity and Fire Emissions in Siberia
title_fullStr Wildfire Intensity and Fire Emissions in Siberia
title_full_unstemmed Wildfire Intensity and Fire Emissions in Siberia
title_sort wildfire intensity and fire emissions in siberia
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/fire6070246
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Siberia
genre_facet Arctic
Siberia
op_source Fire; Volume 6; Issue 7; Pages: 246
op_relation https://dx.doi.org/10.3390/fire6070246
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/fire6070246
container_title Fire
container_volume 6
container_issue 7
container_start_page 246
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