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C Lorius

Datos Biográficos

ID5396171
NOMBREC Lorius
NOMBRESC
APELLIDOLorius
FIRMALORIUS C
AFILIACIONESLaboratoire de Glaciologie et Géophysique de l’Environnement
VERIFICADONo
TOTAL DE OBRAS9
TOTAL DE CITAS0
TOTAL COMO AUTOR9
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN1964
AÑO MÁS RECIENTE DE PUBLICACIÓN2000
ÍNDICE H0
  • Four climatic cycles based on ice core data from deep drilling at the Vostok station, Antarctica

    V M Kotlyakov, C Lorius•ARTICLE•Polar Geography•2000

    The results of many years of Russian‐French‐American studies of an ice core from a borehole in central Antarctica to a depth of 3310 m are presented. The data encompass four climatic cycles over the course of 420,000 years. The similarity and differences of each of the studied glacial epochs and interglacials are demonstrated with respect to a number of parameters: isotopic temperature, insolation conditions, airborne particulates, and greenhouse…

  • Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

    Open Access•Jean‐Robert Petit, J R Petit et al.•ARTICLE•Nature•1999

  • Analysis of climatic cycles from deep‐hole data from Vostok station, Antarctica

    V M Kotlyakov, C Lorius•ARTICLE•Polar Geography•1997

    The results of processing of an ice core to a depth of 2,755 m, which encompasses the last two climatic cycles, are examined. Data on deuterium content in the ice are analyzed, as are paleotemperature, content of continental dust in the ice, and change in the isotopic composition of atmospheric oxygen extracted from the ice core. The problems involved in completing hole drilling are discussed and in this connection the characteristics of a large …

  • L'Antarctique

    Open Access•C Lorius•ARTICLE•Natures Sciences Sociétés•1997

  • A Comparison of Deep Antarctic Ice Cores and Their Implications for Climate Between 65,000 and 15,000 Years Ago

    Open Access•J Jouzel, G M Raisbeck et al.•ARTICLE•Quaternary Research•1989

    Three ice cores drilled in the central part of the Antarctic continent extend back to the last glacial period: one from West Antarctica (Byrd) and two from East Antarctica (Vostok and Dome C). This period is also partly covered by a few cores from the coastal areas. In these cores, climatic information is mostly derived from the isotopic profiles (δD or δ 18 O) from which surface temperature and, more indirectly, precipitation rate can be estimat…

  • Global change over the last climatic cycle from the vostok ice core record (Antarctica)

    Open Access•J Jouzel, N I Barkov et al.•ARTICLE•Quaternary International•1989

  • Vostok ice core provides 160,000-year record of atmospheric CO2

    Open Access•J M Barnola, Jean-Marc Barnola et al.•ARTICLE•Nature•1987

  • The International Antarctic Glaciological Project Standardization document

    Open Access•C R Bentley, Callan Bentley et al.•ARTICLE•Polar Record•1972

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Isotopes in relation to polar glaciology

    Open Access•C Lorius•ARTICLE•Polar Record•1964•Referencias: 3

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

Sin obras prominentes en esta página.

  • Isotopes in relation to polar glaciology

    Open Access•C Lorius•ARTICLE•Polar Record•1964•Referencias: 3

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • The International Antarctic Glaciological Project Standardization document

    Open Access•C R Bentley, Callan Bentley et al.•ARTICLE•Polar Record•1972

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Vostok ice core provides 160,000-year record of atmospheric CO2

    Open Access•J M Barnola, Jean-Marc Barnola et al.•ARTICLE•Nature•1987

  • A Comparison of Deep Antarctic Ice Cores and Their Implications for Climate Between 65,000 and 15,000 Years Ago

    Open Access•J Jouzel, G M Raisbeck et al.•ARTICLE•Quaternary Research•1989

    Three ice cores drilled in the central part of the Antarctic continent extend back to the last glacial period: one from West Antarctica (Byrd) and two from East Antarctica (Vostok and Dome C). This period is also partly covered by a few cores from the coastal areas. In these cores, climatic information is mostly derived from the isotopic profiles (δD or δ 18 O) from which surface temperature and, more indirectly, precipitation rate can be estimat…

  • Global change over the last climatic cycle from the vostok ice core record (Antarctica)

    Open Access•J Jouzel, N I Barkov et al.•ARTICLE•Quaternary International•1989

  • Analysis of climatic cycles from deep‐hole data from Vostok station, Antarctica

    V M Kotlyakov, C Lorius•ARTICLE•Polar Geography•1997

    The results of processing of an ice core to a depth of 2,755 m, which encompasses the last two climatic cycles, are examined. Data on deuterium content in the ice are analyzed, as are paleotemperature, content of continental dust in the ice, and change in the isotopic composition of atmospheric oxygen extracted from the ice core. The problems involved in completing hole drilling are discussed and in this connection the characteristics of a large …

  • L'Antarctique

    Open Access•C Lorius•ARTICLE•Natures Sciences Sociétés•1997

  • Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

    Open Access•Jean‐Robert Petit, J R Petit et al.•ARTICLE•Nature•1999

  • Four climatic cycles based on ice core data from deep drilling at the Vostok station, Antarctica

    V M Kotlyakov, C Lorius•ARTICLE•Polar Geography•2000

    The results of many years of Russian‐French‐American studies of an ice core from a borehole in central Antarctica to a depth of 3310 m are presented. The data encompass four climatic cycles over the course of 420,000 years. The similarity and differences of each of the studied glacial epochs and interglacials are demonstrated with respect to a number of parameters: isotopic temperature, insolation conditions, airborne particulates, and greenhouse…

Cryospheric studies and observations (8 obras) · Geography (7 obras) · Geology and Paleoclimatology Research (7 obras) · Physical geography (7 obras) · Climatology (6 obras) · Ice core (6 obras) · Climate change (5 obras) · Geology (5 obras) · Glacial period (5 obras) · Paleoclimatology (5 obras)

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