FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045554057> ?p ?o ?g. }

• W2045554057 endingPage "846" @default.
• W2045554057 startingPage "835" @default.
• W2045554057 abstract "Predictions of the extent of forest fires under warmer and drier conditions in boreal regions require knowledge of long-term relationships between fire and climate. However, many long-term studies that utilize the remains of total charcoal in lacustrine sediments fail to demonstrate a relationship between climate change and fire activity. A new approach to reconstruct the relative-area burned based on specific types of charcoal particles (the charcoal-morphotype (CM) fire index) has shown significant correlations to recorded forest fires. Here we assess the utility of the CM derived from an analysis of charcoal morphotypes in sediment cores from Opatcho Lake (British Columbia, Canada) using two independent paleoclimate proxies over the last 400 years, and since the mid Holocene. Over the past 400 years, significant correlations between the CM fire index and independent climate reconstructions (diatom-inferred salinity, dendroclimatic reconstructions of temperature and precipitation, and reconstructions of the Pacific Decadal Oscillation) range from 0.35 to 0.42. Similarly, since the mid Holocene the correlation between the CM fire index and independent proxies of past climate (diatom-inferred salinity and temperature inferences from chironomids from the southern interior of British Columbia) range from 0.70 to 0.76. These significant correlations strongly contrast with the very low and insignificant correlations between the CM fire index and total charcoal, suggesting that this approach provides paleofire information not available from traditional techniques. The CM fire index suggests that fires were at least two- and five-fold larger than those observed during the instrumental period, over the last 400 and 6000 years, respectively." @default.
• W2045554057 created "2016-06-24" @default.
• W2045554057 creator A5011775705 @default.
• W2045554057 creator A5029601920 @default.
• W2045554057 date "2009-08-14" @default.
• W2045554057 modified "2023-10-18" @default.
• W2045554057 title "Extreme fires under warmer and drier conditions inferred from sedimentary charcoal morphotypes from Opatcho Lake, central British Columbia, Canada" @default.
• W2045554057 cites W142745411 @default.
• W2045554057 cites W1949467692 @default.
• W2045554057 cites W1963559466 @default.
• W2045554057 cites W1963700381 @default.
• W2045554057 cites W1971170865 @default.
• W2045554057 cites W1972511685 @default.
• W2045554057 cites W1985196270 @default.
• W2045554057 cites W1988614095 @default.
• W2045554057 cites W1992682599 @default.
• W2045554057 cites W1993833546 @default.
• W2045554057 cites W1994088413 @default.
• W2045554057 cites W1996691195 @default.
• W2045554057 cites W2002992535 @default.
• W2045554057 cites W2006283520 @default.
• W2045554057 cites W2011352468 @default.
• W2045554057 cites W2013989474 @default.
• W2045554057 cites W2022798212 @default.
• W2045554057 cites W2028776183 @default.
• W2045554057 cites W2030808813 @default.
• W2045554057 cites W2033386147 @default.
• W2045554057 cites W2042437643 @default.
• W2045554057 cites W2044900008 @default.
• W2045554057 cites W2045054649 @default.
• W2045554057 cites W2062650255 @default.
• W2045554057 cites W2070766630 @default.
• W2045554057 cites W2083054884 @default.
• W2045554057 cites W2087890929 @default.
• W2045554057 cites W2091860178 @default.
• W2045554057 cites W2094829689 @default.
• W2045554057 cites W2096205454 @default.
• W2045554057 cites W2096325281 @default.
• W2045554057 cites W2099765928 @default.
• W2045554057 cites W2100119227 @default.
• W2045554057 cites W2101256521 @default.
• W2045554057 cites W2102295164 @default.
• W2045554057 cites W2114562100 @default.
• W2045554057 cites W2128449886 @default.
• W2045554057 cites W2132058438 @default.
• W2045554057 cites W2136725137 @default.
• W2045554057 cites W2138336783 @default.
• W2045554057 cites W2138444770 @default.
• W2045554057 cites W2143777190 @default.
• W2045554057 cites W2149034870 @default.
• W2045554057 cites W2150426705 @default.
• W2045554057 cites W2152043757 @default.
• W2045554057 cites W2159738122 @default.
• W2045554057 cites W2159792954 @default.
• W2045554057 cites W2161973174 @default.
• W2045554057 cites W2164482362 @default.
• W2045554057 cites W2165977355 @default.
• W2045554057 cites W2166897677 @default.
• W2045554057 cites W2168666463 @default.
• W2045554057 cites W2170881592 @default.
• W2045554057 cites W2280624662 @default.
• W2045554057 cites W235579445 @default.
• W2045554057 cites W323218244 @default.
• W2045554057 doi "https://doi.org/10.1177/0959683609337357" @default.
• W2045554057 hasPublicationYear "2009" @default.
• W2045554057 type Work @default.
• W2045554057 sameAs 2045554057 @default.
• W2045554057 citedByCount "15" @default.
• W2045554057 countsByYear W20455540572012 @default.
• W2045554057 countsByYear W20455540572013 @default.
• W2045554057 countsByYear W20455540572014 @default.
• W2045554057 countsByYear W20455540572015 @default.
• W2045554057 countsByYear W20455540572018 @default.
• W2045554057 crossrefType "journal-article" @default.
• W2045554057 hasAuthorship W2045554057A5011775705 @default.
• W2045554057 hasAuthorship W2045554057A5029601920 @default.
• W2045554057 hasConcept C100537666 @default.
• W2045554057 hasConcept C100970517 @default.
• W2045554057 hasConcept C107054158 @default.
• W2045554057 hasConcept C110872660 @default.
• W2045554057 hasConcept C111368507 @default.
• W2045554057 hasConcept C117935615 @default.
• W2045554057 hasConcept C127313418 @default.
• W2045554057 hasConcept C132651083 @default.
• W2045554057 hasConcept C140345934 @default.
• W2045554057 hasConcept C151730666 @default.
• W2045554057 hasConcept C153294291 @default.
• W2045554057 hasConcept C154808844 @default.
• W2045554057 hasConcept C159985019 @default.
• W2045554057 hasConcept C18903297 @default.
• W2045554057 hasConcept C191897082 @default.
• W2045554057 hasConcept C192562407 @default.
• W2045554057 hasConcept C204323151 @default.
• W2045554057 hasConcept C205649164 @default.
• W2045554057 hasConcept C2993091396 @default.
• W2045554057 hasConcept C33683781 @default.
• W2045554057 hasConcept C39432304 @default.
• W2045554057 hasConcept C49204034 @default.

• next