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Tarmo Virtanenj

Datos Biográficos

ID11046241
NOMBRETarmo Virtanenj
NOMBRESTarmo
APELLIDOVirtanenj
FIRMAVIRTANENJ T
AFILIACIONESFinnish Forest Research Institute, Rovaniemi Research Station, Eteldranta 55, FIN-96301 Rovaniemi, Finland; Department of Biological and Environmental Sciences, P O. Box 65 FIN-00014 University of Helsinki, Finland
VERIFICADONo
TOTAL DE OBRAS1
TOTAL DE CITAS5
TOTAL COMO AUTOR1
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN2006
AÑO MÁS RECIENTE DE PUBLICACIÓN2006
ÍNDICE H1
  • Past changes in the Scots pine forest line and climate in Finnish Lapland

    Open Access•Seija Kultti, Kari Mikkola et al.•ARTICLE•The Holocene•2006•Citada por: 5•Referencias: 9

    Subfossil samples of Scots pine (Pinus sylvestris) and evidence of pine stomata and pollen accumulation rates from previously studied lakes located beyond the present pine forest line in Finnish Lapland were used to reconstruct the extent of the past forest line and the corresponding minimum shift in mean July temperatures, compared with the present. The location of the present pine forest line follows the c. + 12.2C mean July temperature isoline…

  • Past changes in the Scots pine forest line and climate in Finnish Lapland

    Open Access•Seija Kultti, Kari Mikkola et al.•ARTICLE•The Holocene•2006•Citada por: 5•Referencias: 9

    Subfossil samples of Scots pine (Pinus sylvestris) and evidence of pine stomata and pollen accumulation rates from previously studied lakes located beyond the present pine forest line in Finnish Lapland were used to reconstruct the extent of the past forest line and the corresponding minimum shift in mean July temperatures, compared with the present. The location of the present pine forest line follows the c. + 12.2C mean July temperature isoline…

  • Past changes in the Scots pine forest line and climate in Finnish Lapland

    Open Access•Seija Kultti, Kari Mikkola et al.•ARTICLE•The Holocene•2006•Citada por: 5•Referencias: 9

    Subfossil samples of Scots pine (Pinus sylvestris) and evidence of pine stomata and pollen accumulation rates from previously studied lakes located beyond the present pine forest line in Finnish Lapland were used to reconstruct the extent of the past forest line and the corresponding minimum shift in mean July temperatures, compared with the present. The location of the present pine forest line follows the c. + 12.2C mean July temperature isoline…

Botany (1 obras) · Climate change (1 obras) · Climate change and permafrost (1 obras) · Environmental Science (1 obras) · Forestry (1 obras) · Geography (1 obras) · Geology (1 obras) · Geology and Paleoclimatology Research (1 obras) · Holocene (1 obras) · Holocene climatic optimum (1 obras)

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