extent of the north americanboreal zone

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November 2008 Extent of the North American Boreal Zone Dr. James Brandt jbrandt@nrcan.gc.ca Sir William Logan Building Ottawa CANADA

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Extent of the North American Boreal Zone

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  • November 2008

    Extent of the North American Boreal Zone

    Dr. James Brandt [email protected] Sir William Logan Building Ottawa CANADA

  • Introduction

    Circumpolar boreal zone is one of the worlds largest and most important biogeoclimatic areas

  • Background

    In the literature, there is large variation in the area of forests within circumpolar boreal zone

    Maps are often low resolution little value for estimating area

    Methodologies & terminologies of researchers have varied resulting in different opinions on limits of boreal zone in various regions

    Language barriers literature written in several languages (Chinese, English, Finnish, French, Japanese, Mongolian, Norwegian, Swedish, Russian)

  • Opportunities

    Geographic information systems (GIS) have improved our ability to produce spatially accurate maps

    Technology is limited by accuracy & resolution of accessed spatial data

    Recent studies within boreal zone and other recently developed spatial data sets provide new data that can be used in combination with a GIS to develop an improved North American boreal zone map

  • Objectives

    Review North American literature pertaining to plant geography of boreal zone

    Develop revised map of North American boreal zone and hemiboreal subzone using consistent criteria & most current information

    Use GIS to compare & contrast existing maps of zone

    Provide descriptive statistics on the area of the boreal zone and the hemiboreal subzone based on the new map

  • Source Maps

    Maps of North Americas boreal zone and its forests were scanned, digitized, and converted to GIS shapefiles; several maps were available digitally

    All shapefiles converted to same projection and datum

    GIS used to view & compare boundaries of 32 maps of boreal zone

  • Vegetation Zones Defined

    Arctic zone absence of trees, occurrence of continuous permafrost, and presence of tundra vegetation dominated by low-growing shrubs, herbaceous plants, mosses, and lichens (Walker et al. 2002)

    Boreal zone the broad, circumpolar vegetation belt of high northern latitudes covered with forests and other wooded land consisting of cold-hardy trees primarily within the genera Abies, Larix, Picea, or Pinus but also Populus and Betula

    Temperate zone dominance on most sites of tree species intolerant of extremely cold winter temperatures (warmer than 45oC) (includes hemiboreal subzone)

    in continental situations, occupied primarily by grasslands, where their occurrence is dictated by moisture availability

  • North America

  • North America

    Rowe (1972)

  • North America

    Viereck & Little (1972)

    Rowe (1972)

  • Viereck & Little (1972)

    Rowe (1972)

    North AmericaBoreal zone, hemiboreal subzone, alpine areas

    Boreal zone

  • Viereck & Little (1972)

    Rowe (1972)

    North AmericaBoreal zone, hemiboreal subzone, alpine areas

    Boreal zone

    Hemiboreal subzone (Temperate zone)

  • Viereck & Little (1972)

    Rowe (1972)

    North AmericaBoreal zone, hemiboreal subzone, alpine areas

    Boreal zone

    Hemiboreal subzone (Temperate zone)

    Alpine areas (within the Boreal zone and Hemiboreal subzone

  • North AmericaBoreal zone, hemiboreal subzone, alpine areas

    Boreal zone

    Hemiboreal subzone (Temperate zone)

  • BC Ministry of Forests

    and Range, 2006

    Marschner, 1974

    Finley, 1976

    Comer et al., 1995

    Feilberg, 1984

    Archibold &

    Wilson, 1980

    Payette, 1983

    Timoney, 1988

    Rowe, 1972

    Saucier et al., 1998

    Zoltai, 1975Shantz & Zon, 1936

    Rowe, 1972

    Natural Regions

    Committee, 2006

    Viereck &

    Little, 1972

    Bird, 1961

    Oswald &

    Senyk, 1980

    North AmericaBoreal zone and hemiboreal subzone

    Boreal zone

    Hemiboreal subzone (Temperate zone)

  • North American TreelineFrom CAVM

  • Northeastern North America TreelineFrom CAVM

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Northeastern North America8 other approaches in chronological order

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Western Interior of North America10 other approaches

  • Areal Extent (in millions of ha)

    Study

    Boreal zone in

    Canada

    This paper 552

    FAO (2006) 526

    Olsen et al. (2001) 461

    ESWG (1995) 582

    EWG (1989) 556

    Tuhkanen (1984) 557

    Rowe (1972) 531

    Semenova-Tyan-Shanskaya (1964) 511

  • Conclusions

    The map of the North American boreal zone should be considered a refinement of the maps of Rowe (1972) and Viereck and Little (1972). The hemiboreal subzone, while mapped, is considered part of the temperate zone.

    These changes in the map of the boreal zone reflect an improvement in technology and data sets rather than a shift due to environmental or anthropogenic factors.

    Thus, scientists, regulators, and environmental groups can use the map and the corresponding statistics of the North American boreal zone to create a common baseline or standard against which future changes in the North American boreal zone and the success of conservation efforts can be measured.

  • Questions?

  • Acknowledgements

    C. van Eden graphic design

    J.-P. Saucier, Qubecs Ministre des Ressources naturelles et Faune GIS data of Quebecs Ecological Land Classification hierarchy

    J. Weber, R. Brett, M. Gartrell, and

    M. Newman GIS work at NoFC

    T. Scupien, USDA FS GIS data of original vegetation in Michigan,

    Minnesota, and Wisconsin

    T. Hogg, B. Meades, J. Volney, and the anonymous reviewers of Environmental Reviews for their contribution to improving the manuscript

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • North Central North America4 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Northwestern North America8 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Great Lakes Region of North America10 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches

  • Western Cordillera of North America8 other approaches