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  • 1
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1998
    In:  Journal of Geophysical Research: Atmospheres Vol. 103, No. D8 ( 1998-04-27), p. 8935-8946
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 103, No. D8 ( 1998-04-27), p. 8935-8946
    Kurzfassung: Within the Paleoclimate Modeling Intercomparison Project, we have performed simulations of the present‐day, mid‐Holocene (MH), and Last Glacial Maximum (LGM) climates with two versions of the LMD (Laboratoire de Météorologie Dynamique, CNRS, Paris) atmospheric general circulation model which differ in their horizontal resolution and some parameterizations of the surface processes. This work focuses on the winter simulated climatic changes in northern midlatitudes, and we use energy budget analyses to diagnose the impact of the parameterizations on the climatic sensitivity. The dependency of the surface transfer coefficients on the air stability is shown to play a key role for the climatic sensitivity over regions of stable conditions: the northern Atlantic which is sea‐ice covered at LGM, and the midlatitude continents during MH. For the MH we use a simple mathematical projection method to extract the climatic change signal from its interannual variability.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1998
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1993
    In:  Journal of Geophysical Research: Atmospheres Vol. 98, No. D2 ( 1993-02-20), p. 2807-2830
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 98, No. D2 ( 1993-02-20), p. 2807-2830
    Kurzfassung: The linear relationship observed between the water isotopic contents of precipitation and surface air temperatures leads to the use of the water isotopes, H 2 18 O and HDO, in paleoclimatology. Applied to the measurements of the isotopic content of paleowaters, like groundwaters and deep ice cores, this relationship is used to infer paleotemperatures. However, this interpretation of paleo‐isotopic contents is only valid if the isotope‐temperature relationship is not affected by climate change. To address this problem, we have developed a water isotope modeling inside an atmospheric general circulation model (AGCM) and performed simulations of both the present‐day and Last Glacial Maximum (LGM) climatic conditions. AGCMs are indeed the only appropriate tools able to account the whole complexity of the atmospheric circulation. For the present‐day climate, preliminary results for January were presented by Joussaume et al. (1984) and are complemented by new simulations performed for both February and August climatic conditions with a higher‐resolution version of the model. Model results are well corroborated by observations. They also exhibit some effects of the atmospheric circulation on the isotopic fields. For the simulated LGM climate, the model results compare well with paleoclimatic data of water isotopic contents, except for a higher than observed spatial variability. The overall patterns of the simulated δ 18 O‐temperature relationship for the LGM climate are practically unchanged, which tends to comfort the use of water isotopes in paleoclimatology. However, concerning the deuterium excess, i.e., the relationship between oxygen 18 and deuterium, the model results are not sufficiently valid to allow a discussion of the use of deuterium excess in paleoclimatology.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1993
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1996
    In:  Geophysical Research Letters Vol. 23, No. 22 ( 1996-11-01), p. 3191-3194
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 23, No. 22 ( 1996-11-01), p. 3191-3194
    Materialart: Online-Ressource
    ISSN: 0094-8276
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1996
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    OpenEdition ; 2013
    In:  Histoire de la recherche contemporaine , No. Tome II - N°1 ( 2013-06-15), p. 38-49
    In: Histoire de la recherche contemporaine, OpenEdition, , No. Tome II - N°1 ( 2013-06-15), p. 38-49
    Materialart: Online-Ressource
    ISSN: 2260-3875 , 2265-786X
    URL: Issue
    Sprache: Unbekannt
    Verlag: OpenEdition
    Publikationsdatum: 2013
    ZDB Id: 2724035-6
    SSG: 19,2
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Online-Ressource
    Online-Ressource
    International Glaciological Society ; 1997
    In:  Annals of Glaciology Vol. 25 ( 1997), p. 145-152
    In: Annals of Glaciology, International Glaciological Society, Vol. 25 ( 1997), p. 145-152
    Kurzfassung: In the framework of the Paleoclimate Modelling Intercomparison Project (PMIP), simulations of the Last Glacial Maximum (LGM) have- been performed. More than 10 different atmospheric general circulation models (AGCMs) have been used with the same boundary conditions: sea-surface temperatures prescribed by CLIMAP (1981), ice-sheet reconstruction provided by Peltier (1994), change in insolation, and reduced CO 2 content. One of the major questions is to investigate whether the simulations of the LGM are in equilibrium with the prescribed ice-sheet reconstruction. To answer this question, we have used two different approaches. First, we analyze the results of a sel of LGM simulations performed with different versions of the Laboratoire de Meteorolo-gie Dynamique (LMD) AGCM and study the hydrologic and snow- budgets over the Laurcntide and Fennoscandian ice sheets. Second, we use the AGCM outputs to force an ice-sheet model in order to investigate its ability to maintain the ice sheets as reconstructed by CLIMAP (1981) or Peltier (1994).
    Materialart: Online-Ressource
    ISSN: 0260-3055 , 1727-5644
    Sprache: Englisch
    Verlag: International Glaciological Society
    Publikationsdatum: 1997
    ZDB Id: 2122400-6
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Online-Ressource
    Online-Ressource
    International Glaciological Society ; 1985
    In:  Annals of Glaciology Vol. 7 ( 1985), p. 131-137
    In: Annals of Glaciology, International Glaciological Society, Vol. 7 ( 1985), p. 131-137
    Kurzfassung: Atmospheric general circulation models are believed to be appropriate tools for studying airborne impurity cycles in order to supplement observations and to improve our knowledge of gaseous and particulate pollutant cycles in the atmosphere. The main aspects of the modelling of tracer cycles are reviewed and illustrated by two particular examples: desert dust particles in the 1 μm range and water isotope species HDO and H 2 18 O. Some results from a first simulation including desert dust and water isotope cycles using the model developed at the Laboratoire de Météorologie Dynamique (LMD) are presented and compared to observations, with particular emphasis on ice-sheet data. The relatively good agreement with observations obtained so far is encouraging and should stimulate further applications to other types of tracers.
    Materialart: Online-Ressource
    ISSN: 0260-3055 , 1727-5644
    Sprache: Englisch
    Verlag: International Glaciological Society
    Publikationsdatum: 1985
    ZDB Id: 2122400-6
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Online-Ressource
    Online-Ressource
    Springer Science and Business Media LLC ; 1997
    In:  Nature Vol. 386, No. 6627 ( 1997-4), p. 788-795
    In: Nature, Springer Science and Business Media LLC, Vol. 386, No. 6627 ( 1997-4), p. 788-795
    Materialart: Online-Ressource
    ISSN: 0028-0836 , 1476-4687
    RVK:
    RVK:
    RVK:
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 1997
    ZDB Id: 120714-3
    ZDB Id: 1413423-8
    SSG: 11
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Online-Ressource
    Online-Ressource
    Springer Science and Business Media LLC ; 2020
    In:  Climatic Change Vol. 162, No. 2 ( 2020-09), p. 527-544
    In: Climatic Change, Springer Science and Business Media LLC, Vol. 162, No. 2 ( 2020-09), p. 527-544
    Kurzfassung: Global warming is projected to intensify during the twenty-first century. Yet, only few studies investigate how global warming could be perceived by future populations. Here, we propose an assessment of how climate change could be perceived by combining climatological indicators. We analyse extremes of temperature ( T 99 ) and simplified Wet-Bulb Globe Temperature (WBGT 99 ), a heat stress index assessing the combined effect of elevated temperature and humidity on the human body. The speed of change is defined for each year as the difference between the previous 20 years and the twenty upcoming years (i.e. with a moving baseline), and we assess how these speeds emerge from each last 20-year interannual variability. Using a set of 12 CMIP5 models, speeds of change of T 99 and WBGT 99 in 2080 are both twice as fast compared with current speeds in mid-latitudes, and by up to four times faster in the tropics under the RCP8.5 scenario. Warming accelerations are thus similar for T 99 and WBGT 99 . However, these speeds in tropical regions in 2080 are projected to be 2.3 times larger than the last 20-year interannual variability for WBGT 99 , and only 1.5 to 1.8 times larger for T 99 . According to the models, the WBGT 99 intensification will be more emergent from the recent year-to-year variability than the T 99 warming. This analysis suggests that the accelerated warming of heat extremes will be felt more strongly by populations than current changes for RCP8.5, and that this evolution will be more perceived in heat stress than in temperature, particularly within the tropics.
    Materialart: Online-Ressource
    ISSN: 0165-0009 , 1573-1480
    RVK:
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 2020
    ZDB Id: 751086-X
    ZDB Id: 1477652-2
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    In: VertigO, OpenEdition, , No. Hors-série 12 ( 2012-05-15)
    Materialart: Online-Ressource
    ISSN: 1492-8442
    URL: Issue
    Sprache: Französisch
    Verlag: OpenEdition
    Publikationsdatum: 2012
    ZDB Id: 2160750-3
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Online-Ressource
    Online-Ressource
    PERSEE Program ; 1994
    In:  Bulletin de la Société préhistorique française Vol. 91, No. 1 ( 1994), p. 64-76
    In: Bulletin de la Société préhistorique française, PERSEE Program, Vol. 91, No. 1 ( 1994), p. 64-76
    Kurzfassung: RÉSUMÉ Placé à quelques mètres en avant de la "Ciste des Cous", monument à chambre circulaire et couloir d'accès dans un cairn circulaire à double parement, le dolmen des Pierres-Folles est de type angevin. Sa chambre présente une longueur intérieure de 5 m pour 2,60 m de large. Son tumulus étroit à façade rectiligne, ou légèrement rentrante, rappelle fortement celui du dolmen angevin de la Bajou- lière à Saint-Rémy-la-Varenne dans le Maine-et-Loire. Les éléments archéologiques recueillis dans ce dolmen très perturbé ne permettent pas d'en dater la construction.
    Materialart: Online-Ressource
    ISSN: 0249-7638
    Sprache: Französisch
    Verlag: PERSEE Program
    Publikationsdatum: 1994
    ZDB Id: 2506497-6
    SSG: 6,12
    SSG: 6,11
    Standort Signatur Einschränkungen Verfügbarkeit
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