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Christian Zdanowicz

Dados Biográficos

ID6570633
NOMEChristian Zdanowicz
PRENOMESChristian
SOBRENOMEZdanowicz
ASSINATURAZDANOWICZ C
AFILIAÇÕESNatural Resources Canada
ORCID0000-0002-1045-5063
VERIFICADOSim
TOTAL DE OBRAS6
TOTAL DE CITAÇÕES7
TOTAL COMO AUTOR6
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2000
ANO MAIS RECENTE DE PUBLICAÇÃO2016
ÍNDICE H1
  • Palaeoenvironmental history of the last six centuries in the Nettilling Lake area (Baffin Island, Canada)

    Open Access•Anne Beaudoin, Reinhard Pienitz et al.•ARTICLE•The Holocene•2016•Citada por: 1•Referências: 4

    The Baffin Island region in the eastern Canadian Arctic has recently experienced a rapid warming, possibly unprecedented in millennia. To investigate the response of freshwater environments to this warming and place it in a secular perspective, we analyzed a 90-cm-long sediment core from Nettilling Lake, the largest lake of the Canadian Arctic Archipelago. The core was taken from a part of the lake basin that receives meltwater and sediment input…

  • Ice Cores from the St. Elias Mountains, Yukon, Canada

    Open Access•Christian Zdanowicz, David Fisher et al.•ARTICLE•ARCTIC•2014

    A major achievement in research supported by the Kluane Lake Research Station was the recovery, in 2001 – 02, of a suite of cores from the icefields of the central St. Elias Mountains, Yukon, by teams of researchers from Canada, the United States, and Japan. This project led to the development of parallel, long (103 – 104 year) ice-core records of climate and atmospheric change over an altitudinal range of more than 2 km, from the Eclipse Icefiel…

  • The Mt Logan Holocene—late Wisconsinan isotope record

    Open Access•David Fisher, E C Osterberg et al.•ARTICLE•The Holocene•2008•Citada por: 6•Referências: 1

    The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…

  • Nature and origin of a Pleistocene-age massive ground-ice body exposed in the Chapman Lake moraine Complex, central Yukon Territory, Canada

    Open Access•Denyse Lacelle, Bernard Lauriol et al.•ARTICLE•Quaternary Research•2007

    A massive ground-ice body was found exposed in the headwall of a thaw flow developed within the Chapman Lake terminal moraine complex on the Blackstone Plateau (Ogilvie Mountains, central Yukon Territory), which is contemporaneous to the Reid glaciation. Based on visible cryostructures in the 4-m-high headwall, two units were identified: massive ground ice, overlain sharply by 2 m of icy diamicton. The nature and origin of the Chapman Lake massiv…

  • Molar gas ratios of air entrapped in ice

    Open Access•Raphaelle Cardyn, Ian D Clark et al.•ARTICLE•Quaternary Research•2007

    The molar ratios of atmospheric gases change during dissolution in water due to differences in their relative solubilities. We exploited this characteristic to develop a tool to clarify the origin of ice formations in permafrost regions. Extracted from ice, molar gas ratios can distinguish buried glacier ice from intrasedimental ground ice formed by freezing groundwaters. An extraction line was built to isolate gases from ice by melting and trapp…

  • A Holocene Record of Atmospheric Dust Deposition on the Penny Ice Cap, Baffin Island, Canada

    Open Access•Christian Zdanowicz, Christian M Zdanowicz et al.•ARTICLE•Quaternary Research•2000

    An >11,550-yr-long record of atmospheric dust deposition was developed from an ice core (P95) drilled through the Penny ice cap, Baffin Island. The P95 record documents environmental changes that affected the production and transport of dust in the eastern Canadian Arctic during the late Pleistocene and Holocene. Dust deposition on the Penny ice cap was greatest in late-glacial time when the climate was dry and windy and comparatively low in the …

  • The Mt Logan Holocene—late Wisconsinan isotope record

    Open Access•David Fisher, E C Osterberg et al.•ARTICLE•The Holocene•2008•Citada por: 6•Referências: 1

    The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…

  • Palaeoenvironmental history of the last six centuries in the Nettilling Lake area (Baffin Island, Canada)

    Open Access•Anne Beaudoin, Reinhard Pienitz et al.•ARTICLE•The Holocene•2016•Citada por: 1•Referências: 4

    The Baffin Island region in the eastern Canadian Arctic has recently experienced a rapid warming, possibly unprecedented in millennia. To investigate the response of freshwater environments to this warming and place it in a secular perspective, we analyzed a 90-cm-long sediment core from Nettilling Lake, the largest lake of the Canadian Arctic Archipelago. The core was taken from a part of the lake basin that receives meltwater and sediment input…

  • A Holocene Record of Atmospheric Dust Deposition on the Penny Ice Cap, Baffin Island, Canada

    Open Access•Christian Zdanowicz, Christian M Zdanowicz et al.•ARTICLE•Quaternary Research•2000

    An >11,550-yr-long record of atmospheric dust deposition was developed from an ice core (P95) drilled through the Penny ice cap, Baffin Island. The P95 record documents environmental changes that affected the production and transport of dust in the eastern Canadian Arctic during the late Pleistocene and Holocene. Dust deposition on the Penny ice cap was greatest in late-glacial time when the climate was dry and windy and comparatively low in the …

  • Nature and origin of a Pleistocene-age massive ground-ice body exposed in the Chapman Lake moraine Complex, central Yukon Territory, Canada

    Open Access•Denyse Lacelle, Bernard Lauriol et al.•ARTICLE•Quaternary Research•2007

    A massive ground-ice body was found exposed in the headwall of a thaw flow developed within the Chapman Lake terminal moraine complex on the Blackstone Plateau (Ogilvie Mountains, central Yukon Territory), which is contemporaneous to the Reid glaciation. Based on visible cryostructures in the 4-m-high headwall, two units were identified: massive ground ice, overlain sharply by 2 m of icy diamicton. The nature and origin of the Chapman Lake massiv…

  • Molar gas ratios of air entrapped in ice

    Open Access•Raphaelle Cardyn, Ian D Clark et al.•ARTICLE•Quaternary Research•2007

    The molar ratios of atmospheric gases change during dissolution in water due to differences in their relative solubilities. We exploited this characteristic to develop a tool to clarify the origin of ice formations in permafrost regions. Extracted from ice, molar gas ratios can distinguish buried glacier ice from intrasedimental ground ice formed by freezing groundwaters. An extraction line was built to isolate gases from ice by melting and trapp…

  • The Mt Logan Holocene—late Wisconsinan isotope record

    Open Access•David Fisher, E C Osterberg et al.•ARTICLE•The Holocene•2008•Citada por: 6•Referências: 1

    The ice core recovered from Prospector Russell Col on Mt Logan (5.4 km a.s.l.), in the Yukon spans over 20 000 years. This unique record offers a Pacific view of the stable isotope and chemical record from the Lateglacial to the present. The timescale is based on seasonal counted years, the largest known volcanic acid signatures and the major shift in stable isotopes and chemistry at the end of the Younger Dryas. There are large and sustained cha…

  • Ice Cores from the St. Elias Mountains, Yukon, Canada

    Open Access•Christian Zdanowicz, David Fisher et al.•ARTICLE•ARCTIC•2014

    A major achievement in research supported by the Kluane Lake Research Station was the recovery, in 2001 – 02, of a suite of cores from the icefields of the central St. Elias Mountains, Yukon, by teams of researchers from Canada, the United States, and Japan. This project led to the development of parallel, long (103 – 104 year) ice-core records of climate and atmospheric change over an altitudinal range of more than 2 km, from the Eclipse Icefiel…

  • Palaeoenvironmental history of the last six centuries in the Nettilling Lake area (Baffin Island, Canada)

    Open Access•Anne Beaudoin, Reinhard Pienitz et al.•ARTICLE•The Holocene•2016•Citada por: 1•Referências: 4

    The Baffin Island region in the eastern Canadian Arctic has recently experienced a rapid warming, possibly unprecedented in millennia. To investigate the response of freshwater environments to this warming and place it in a secular perspective, we analyzed a 90-cm-long sediment core from Nettilling Lake, the largest lake of the Canadian Arctic Archipelago. The core was taken from a part of the lake basin that receives meltwater and sediment input…

Geology and Paleoclimatology Research (5 obras) · Arctic (4 obras) · Climate change and permafrost (4 obras) · Climatology (4 obras) · Cryospheric studies and observations (4 obras) · Geography (4 obras) · Geology (4 obras) · Geomorphology (4 obras) · Ice core (4 obras) · Oceanography (4 obras)

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