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Roger I C Hansell

Biographic Data

ID5689221
NAMERoger I C Hansell
GIVEN NAMESRoger I C
FAMILY NAMEHansell
SIGNATUREHANSELL R I C
AFFILIATIONSUniversity of Toronto
VERIFIEDNo
TOTAL WORKS4
TOTAL CITATIONS0
AUTHOR COUNT4
EDITOR COUNT0
FIRST PUBLICATION YEAR1971
LATEST PUBLICATION YEAR2002
H-INDEX0
  • Development of White Spruce Tree Islands in the Shrub Zone of the Forest-tundra

    Open Access•Peter A Scott, Peter Scott et al.•ARTICLE•ARCTIC•2002

    The growth of four white spruce (Picea glauca) clonal islands ranging in age from ca. 98 years to more than 400 years was investigated in the shrub zone of the forest-tundra east of Churchill, Manitoba, Canada. The elongation of 20 similar-aged stems in each of the three youngest islands was monitored during 1988 and 1989, along with ground and air temperatures. Stems in the younger islands showed a more flexible response to both daily and annual…

  • Influences of Wind and Snow on Northern Tree-Line Environments at Churchill, Manitoba, Canada

    Open Access•Peter A Scott, Peter Scott et al.•ARTICLE•ARCTIC•1993

    The influences of wind and snow distribution at the tree line near Churchill, Manitoba, were studied. Wind profiles above the snow surface, snow crystal size and quantity were examined during abrasion experiments with white spruce branchlets. For white spruce, the abrasion zone was evidently within 80 cm above the snow surface, and needle removal by abrasion was strongly influenced by branch age. Removal by abrasion of similar-aged needles was hi…

  • Permafrost Development in the Intertidal Zone at Churchill, Manitoba

    Open Access•Roger I C Hansell, Peter A Scott et al.•ARTICLE•ARCTIC•1983

    Boreholes drilled in the Beech Bay area during July to November 1929 indicated that a sill of permafrost had extended below the high-water line, tapering in depth towards low water. The boreholes revealed thick layers of fine sediments on top of deep underlain bedrock. Recent borings determined the upper limits of permafrost in 1981. Examination of the data shows that there has been a permafrost expansion into the emerging tidal zone. These obser…

  • Changes in the Northern Limit of Spruce at Dubawnt Lake, Northwest Territories

    Open Access•Roger I C Hansell, D A Chant et al.•ARTICLE•ARCTIC•1971

    Larsen described the treeline west of Hudson Bay and particularly at Ennadi, Yathkyed and Dubawnt Lakes, as clumps of spruce, relict from a former more northerly distribution. ... Evidence collected by us in 1966 on the Dubawnt River system on the Mackenzie-Keewatin border, indicates that the spruce trees are re-establishing themselves and have moved northward and closer to Dubawnt Lake during the past one hundred years. ... Larsen's view that sp…

No prominent works on this page.

  • Changes in the Northern Limit of Spruce at Dubawnt Lake, Northwest Territories

    Open Access•Roger I C Hansell, D A Chant et al.•ARTICLE•ARCTIC•1971

    Larsen described the treeline west of Hudson Bay and particularly at Ennadi, Yathkyed and Dubawnt Lakes, as clumps of spruce, relict from a former more northerly distribution. ... Evidence collected by us in 1966 on the Dubawnt River system on the Mackenzie-Keewatin border, indicates that the spruce trees are re-establishing themselves and have moved northward and closer to Dubawnt Lake during the past one hundred years. ... Larsen's view that sp…

  • Permafrost Development in the Intertidal Zone at Churchill, Manitoba

    Open Access•Roger I C Hansell, Peter A Scott et al.•ARTICLE•ARCTIC•1983

    Boreholes drilled in the Beech Bay area during July to November 1929 indicated that a sill of permafrost had extended below the high-water line, tapering in depth towards low water. The boreholes revealed thick layers of fine sediments on top of deep underlain bedrock. Recent borings determined the upper limits of permafrost in 1981. Examination of the data shows that there has been a permafrost expansion into the emerging tidal zone. These obser…

  • Influences of Wind and Snow on Northern Tree-Line Environments at Churchill, Manitoba, Canada

    Open Access•Peter A Scott, Peter Scott et al.•ARTICLE•ARCTIC•1993

    The influences of wind and snow distribution at the tree line near Churchill, Manitoba, were studied. Wind profiles above the snow surface, snow crystal size and quantity were examined during abrasion experiments with white spruce branchlets. For white spruce, the abrasion zone was evidently within 80 cm above the snow surface, and needle removal by abrasion was strongly influenced by branch age. Removal by abrasion of similar-aged needles was hi…

  • Development of White Spruce Tree Islands in the Shrub Zone of the Forest-tundra

    Open Access•Peter A Scott, Peter Scott et al.•ARTICLE•ARCTIC•2002

    The growth of four white spruce (Picea glauca) clonal islands ranging in age from ca. 98 years to more than 400 years was investigated in the shrub zone of the forest-tundra east of Churchill, Manitoba, Canada. The elongation of 20 similar-aged stems in each of the three youngest islands was monitored during 1988 and 1989, along with ground and air temperatures. Stems in the younger islands showed a more flexible response to both daily and annual…

Climate change and permafrost (3 works) · Geography (3 works) · Geology (3 works) · Geology (3 works) · Tree-ring climate responses (3 works) · Arctic (2 works) · Bay (2 works) · Biology (2 works) · Ecology (2 works) · Ecology (2 works)

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