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Masrur_2018_Environ._Res._Lett._13_014019.pdf 1,86MB
WeightNameValue
1000 Titel
  • Circumpolar spatio-temporal patterns and contributing climatic factors of wildfire activity in the Arctic tundra from 2001–2015
1000 Autor/in
  1. Masrur, Arif |
  2. Petrov, Andrey N |
  3. DeGroote, John |
1000 Erscheinungsjahr 2018
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2018-01-17
1000 Erschienen in
1000 Quellenangabe
  • 13(1):014019
1000 Copyrightjahr
  • 2018
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1088/1748-9326/aa9a76 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • Recent years have seen an increased frequency of wildfire events in different parts of Arctic tundra ecosystems. Contemporary studies have largely attributed these wildfire events to the Arctic's rapidly changing climate and increased atmospheric disturbances (i.e. thunderstorms). However, existing research has primarily examined the wildfire–climate dynamics of individual large wildfire events. No studies have investigated wildfire activity, including climatic drivers, for the entire tundra biome across multiple years, i.e. at the planetary scale. To address this limitation, this paper provides a planetary/circumpolar scale analyses of space-time patterns of tundra wildfire occurrence and climatic association in the Arctic over a 15 year period (2001–2015). In doing so, we have leveraged and analyzed NASA Terra's MODIS active fire and MERRA climate reanalysis products at multiple temporal scales (decadal, seasonal and monthly). Our exploratory spatial data analysis found that tundra wildfire occurrence was spatially clustered and fire intensity was spatially autocorrelated across the Arctic regions. Most of the wildfire events occurred in the peak summer months (June–August). Our multi-temporal (decadal, seasonal and monthly) scale analyses provide further support to the link between climate variability and wildfire activity. Specifically, we found that warm and dry conditions in the late spring to mid-summer influenced tundra wildfire occurrence, spatio-temporal distribution, and fire intensity. Additionally, reduced average surface precipitation and soil moisture levels in the winter–spring period were associated with increased fire intensity in the following summer. These findings enrich contemporary knowledge on tundra wildfire's spatial and seasonal patterns, and shed new light on tundra wildfire–climate relationships in the circumpolar context. Furthermore, this first pan-Arctic analysis provides a strong incentive and direction for future studies which integrate multiple datasets (i.e. climate, fuels, topography, and ignition sources) to accurately estimate carbon emission from tundra burning and its global climate feedbacks in coming decades.
1000 Sacherschließung
lokal climate variability
lokal climate change
lokal tundra wildfire
lokal climate feedback
lokal circumpolar Arctic
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0001-5050-407X|https://frl.publisso.de/adhoc/uri/UGV0cm92LCBBbmRyZXkgTg==|https://frl.publisso.de/adhoc/uri/RGVHcm9vdGUsIEpvaG4g
1000 Label
1000 Förderer
  1. National Science Foundation |
1000 Fördernummer
  1. 1338850
1000 Förderprogramm
  1. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer National Science Foundation |
    1000 Förderprogramm -
    1000 Fördernummer 1338850
1000 Objektart article
1000 Beschrieben durch
1000 @id frl:6417973.rdf
1000 Erstellt am 2019-12-11T11:34:10.311+0100
1000 Erstellt von 218
1000 beschreibt frl:6417973
1000 Bearbeitet von 218
1000 Zuletzt bearbeitet Thu Jan 30 17:41:27 CET 2020
1000 Objekt bearb. Wed Dec 11 11:35:13 CET 2019
1000 Vgl. frl:6417973
1000 Oai Id
  1. oai:frl.publisso.de:frl:6417973 |
1000 Sichtbarkeit Metadaten public
1000 Sichtbarkeit Daten public
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