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  • 1990-1994  (4)
  • 1
    Keywords: Klima
    Type of Medium: Book
    Pages: 128 S. , graph. Darst., Kt. , 18 cm
    ISBN: 3411103914
    Series Statement: Meyers Forum 23
    RVK:
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    Language: German
    Note: Literaturverz. S. 123 - 124
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  • 2
    Keywords: climatology ; Klimaänderung ; Klimaänderung
    Description / Table of Contents: Taschenbuchausgabe der im BA 7/92 vorgestellten Hardcover-Ausgabe. Inhaltlich wurden laut Vorwort vom Rezensenten nicht feststellbare - "umgangreiche" Aktualisierungen eingearbeitet. Der Umfang der Aktualisierungen macht die Anschaffung der Neuauflage nicht zwingend erforderlich. Anschaffung des seinerzeit von K. Bock besonders empfohlenen Buches ist jetzt auch jenen möglich, die sich die gebundene Ausgabe nicht leisten konnten oder wollten. (2 S) (LK/SB: Prawitt)
    Type of Medium: Book
    Pages: 254 S. , Ill., graph. Darst., Kt. , 19 cm
    Edition: Taschenbuchausg., vollst. überarb. und aktualisiert, Stand: November 1993, Lizenz[ausg.]
    ISBN: 3499195550
    Series Statement: rororo 9555
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    Language: German
    Note: Lizenz der Dt. Verl.-Anst., Stuttgart. - Literaturverz. S. 234 - 236 , Literaturverz. S. 234 - 236
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  • 3
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Based on univariate correlation and coherence analyses and considering the physical basis of the relationships, a simple multiforced (multiple) statistical concept is used which correlates observational climatic time series simultaneously with volcanic, solar, ENSO, and the anthropogenic greenhouse gases forcing. This is appropriate to remove some natural climate noise in the observed data and to evaluate the components (signals) possibly due to the anthropogenic greenhouse gas forcing (CO2, or “equivalent” CO2 implying additional gases) during industrial time. In this paper, we apply this technique to 100 global “box” data time series 1890–1985, of the surface air temperature, using observed data from Hansen and Lebedeff. The results are presented in terms of latitudinal-seasonal and regional trends, where the observed trend patterns are compared with the hypothetical signals (statistical assessments) possibly due to anthropogenic greenhouse forcing. These latter signals can be amplified to enable a comparison with corresponding results from general circulation model (GCM) CO2 doubling experiments. These observed-statistical assessments lead to results which are, at least qualitatively and in respect to the zonal mean temperatures, very similar to some GCM experiments indicating the maximum CO2 doubling signals (statistical assessment 〉 12 K) in the arctic winter. However, these signals are moderate in the tropics and in the Southern Hemisphere (global average 2.8–4.4 K). As far as the “industrial” signals are concerned (observed period) these signals are somewhat larger (maximum 7 K, global average 0.5–0.9 K) than the observed trends (maximum 5 K, global average 0.5 K). Phase shifts of cause and effect may amplify these signals but are very uncertain.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 27 (1994), S. 259-281 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Based on the physical background that varying solar activity should lead to variations of the ‘solar constant’ and that the climate system may respond sensitively even to small solar variations, a correlation analysis is performed where hemispheric and global averages of the annual mean surface air temperature are compared with the variations of a variety of solar forcing parameters: sunspots, related hypotheses including variations of the quasi-eleven-year solar cycle length, solar diameter variations and gravitational effects. This analysis is based on the 1881–1988 period, for the northern hemisphere including proxy data 1671–1988. Cross correlations and correlations moving in time reveal some instability effects which are hard to interpret. The temperature variance components which may be hypothetically explained by solar forcing are small. Similarly, a seasonal and regional signal and signal-to-noise analysis based on a gridded temperature time series 1890–1985 reveals small signals which do not exceed roughly 1.5 K in the arctic winter (maximum) or 0.2-0.3 K on a global average.
    Type of Medium: Electronic Resource
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