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  • 1
    Monograph available for loan
    Monograph available for loan
    Darmstadt : Primus
    Call number: M 10.0218 ; 12/2010.19 ; AWI A3-18-13656
    Description / Table of Contents: Sind die Unwetter und Katastrophen der letzten Jahre Ausdruck einer Klimaveränderung oder gab es sie schon immer? Diese 1000 Jahre umfassende Klimadarstellung, die auf den unterschiedlichsten Quellen basiert, ist einmalig für Mitteleuropa. Sie belegt die nachhaltigen Veränderungen des Klimas in den vergangenen Jahrhunderten, die Auswirkungen auf die Gesellschaft und macht deutlich, bis zu welchem Grad der Mensch in jüngerer Zeit Einfluss genommen hat.
    Type of Medium: Monograph available for loan
    Pages: VIII, 264 S. , Ill., Kt.
    Edition: 2., aktualisierte und erw. Aufl.
    ISBN: 9783896786043
    Classification:
    Meteorology and Climatology
    Language: German
    Note: Inhalt: Vorwort. - Vorwort zur 2.Auflage. - TEIL I GRUNDLAGEN DER HISTORISCHEN KLIMAFORSCHUNG. - Klima in Perspektive: Eine Einführung. - Begründung und Forschungsansätze. - Forschungssituation in Mitteleuropa. - Auf Spurensuche: Quellen, Daten und Zitate. - Chroniken und Annalen: Die ersten Spuren von Wetter, Witterung und Klima. - Quelleninformation - Quellenbezug - Quellenkompilation: Die Dhein-Chronik. - Als das Wetter zum täglichen Ereignis wurde: Wetterjournale. - Vom Wetter auf See: Schiffsjournale. - Vom Wetter unterwegs: Itinerare. - Wetter nach Maß: Die Anfänge der Instrumentenmessung. - Gemalt, gepinselt und gehämmert: Bildhafte und plastische Informationen zum historischen Klima. - Klima auf Umwegen: Proxydaten. - Methoden zur Klimarekonstruktion. - "Hat man mir wahrhafftiglich versicheret": Die quellenkritische Interpretation von schriftlichen Quellenhinweisen. - Klima-, Witterungs- und Wettervorstellungen: Ein Beitrag zur Quellenkritik. - Quelle - Index - Klimawert: Die Transformation schriftlicher Klimahinweise. - Tägliche Wetteraufzeichnungen: Rückblicke der besonderen Art. - Historische Instrumentenmessdaten: Ein Brückenschlag zur Moderne. - Proxydaten: Ihre klimatische Interpretation. - Methoden: Eine Nachbetrachtung. - HISKLID: Aufbau und Struktur der Historischen Klimadatenbank. - TEIL II HITZE, FLUTEN, EIS UND STURM IM SPIEGELBILD DER QUELLEN. - Vom Optimum der Römerzeit über das Pessimum der Völkerwanderung ins Mittelalterliche Wärmeoptimum. - Prolog zum Mittelalterlichen Wärmeoptimum. - Das Klima von 1000 bis 1500. - Warme Zeiten - kalte Zeiten: Die Sommerverhältnisse von 1000 und 1500. - Aus der Kältekammer ins Treibhausklima: Die Winterverhältnisse von 1000 bis 1500. - Im Märzen der Bauer? Die Frühlingsverhältnisse von 1000 bis 1500. - Altweibersommer oder Herbststürme? Die Herbstverhältnisse von 1000 bis 1500. - Das Klima von 1500 bis 2000. - Der jährliche Witterungsgang von 1500 bis 1750. - Zur Kleinen Eiszeit - ein Epilog. - Aus der Kleinen Eiszeit ins Treibhausklima: Die Verhältnisse ab 1750. - Die derzeitigen Folgen. - Der Klimagang der letzten 1000 Jahre - eine Zusammenschau. - Der methodische Weg. - Zum Klimaverlauf ab dem Jahr 1000. - Zur Frage der Steuerungsmechanismen. - Klimarekonstruktionen und -simulationen der letzten 1000 Jahre auf der Basis von naturwissenschaftlichen Daten. - Wenn sich Wetter und Klima zur Katastrophe auswachsen. - Unwetter über Mitteleuropa. - Gewitter in Mitteleuropa. - Stürme und Orkane über Deutschland. - Die Sturmfluten an der deutschen Nord- und Ostseeküste. - Hochwasserereignisse an deutschen Flüssen. - Historische Hochwasser und Atmosphärische Zirkulationsdynamik. - Jahrhundert- und Jahrtausendhochwasser. - Höhenrauch - Sommerhitze - Winterstrenge - Hochwasser: Vier Schritte in die Katastrophe. - Die Hochwasserkatastrophe von 1824 am Neckar und aktuelle planerische Konsequenzen. - Klimakatastrophen in Mitteleuropa: Eine Nachlese. - Die zukünftige Entwicklung des Klimas und die Auswirkungen des Klimawandels in Mitteleuropa. - Die ökonomischen Folgen. - Erkenntniswege zum Treibhausklima. - Die historische Entwicklung des politischen Handlungsrahmens. - 1200 Jahre Klimageschichte: Ein Resümee. - Anhang. - Abkürzungen. - Literaturverzeichnis. - Sachregister. - Ortsregister.
    Location: Upper compact magazine
    Location: Reading room
    Location: AWI Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Darmstadt : Primus-Verl.
    Call number: 12/M 01.0099 ; AWI A3-02-0073 ; PIK N 456-01-0162
    Description / Table of Contents: Sind die Unwetter und Katastrophen der letzten Jahre Ausdruck einer Klimaveränderung oder gab es sie schon immer? Erstmals wird für Mitteleuropa eine auf der Auswertung unterschiedlichster Quellen basierende, 1000 Jahre umfassende Klimadarstellung präsentiert, wobei vor allem auf Extreme wie Dürren, Stürme, Hochwasser und Kälte eingegangen wird. Das mit zahlreichen Abbildungen illustrierte Buch veranschaulicht, welche nachhaltigen Veränderungen unser Klima in den vergangenen Jahrhunderten geprägt haben, wie sie sich auf die Gesellschaft auswirkten und bis zu welchem Grad der Mensch in jüngerer Zeit Einfluss genommen hat.
    Type of Medium: Monograph available for loan
    Pages: VIII, 227 S.
    ISBN: 3896784056
    Classification:
    Meteorology and Climatology
    Language: German
    Location: Reading room
    Location: Reading room
    Location: A 18 - must be ordered
    Branch Library: GFZ Library
    Branch Library: AWI Library
    Branch Library: PIK Library
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  • 3
    Call number: ZS-270(87)
    In: Würzburger geographische Arbeiten
    Type of Medium: Series available for loan
    Pages: 594 S.
    Series Statement: Würzburger geographische Arbeiten 87
    Language: German
    Note: Zugl.: Würzburg, Univ., Diss., 1968
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Call number: ZS-270(94)
    In: Würzburger geographische Arbeiten
    Type of Medium: Series available for loan
    Pages: 139 S.
    Series Statement: Würzburger geographische Arbeiten 94
    Classification:
    Geography and Geomorphology
    Language: German
    Note: Zugl.: Würzburg, Univ., Diss., 1968
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 81 (1994), S. 97-107 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 81 (1994), S. 97-107 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Notes: Abstract. The paper is concerned with various aspects of climatic history. Emphasis is on the spectrum of data and methods used in historical climatology. The following section is devoted to an outline of the short- and long-range climatic changes since 1500 A.D. that show how much the climate has varied in space and time. It is pointed out that climatic extremes have been an ever-recurrent phenomenon throughout history.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The severity and frequency of sixteenth-century floods of the Rhine, the Main, the middle and upper Elbe with its tributaries, rivers of northern and central Italy, the Garonne and rivers in Catalonia and Andalusia are analyzed using documentary evidence. The basic topographical and hydrological characteristics of the rivers investigated as well as the synoptic causes of their flooding during the instrumental period are presented. Different examples of modifications of the run-off process due to anthropogenic activity are discussed. Prevalence in flood occurrence during the second half of the sixteenth century in comparison to the first half is typical for central European and Andalusian rivers (mainly in the 1560s and 1590s) and agrees with the evolution of precipitation patterns. On the other hand, Italian and Catalonian rivers, in part, had a higher occurrence of floods during the first half of the century. Changes in the flooding seasons in both halves of the century are not unambiguous. Results of an analysis on a broader European scale show floods to be a random natural phenomena with limited areal extent defined by the spatial influence of forcing meteorological factors (continuous heavy rains, sudden melting of thick snow cover, etc.). Despite some limitations of documentary evidence, series of reconstructed historical floods are valuable sources of proxy data which can be utilized for the study of the flooding fluctuations in the pre-instrumental period.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 31 (1995), S. 79-98 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This reconstruction of the ice winter severity in the Western Baltic is based for the period 1878-1993 on the accumulated areal ice volume along the German Baltic coast with observations from 13 coastal stations; for the period 1701-1877 it is based on the accumulated areal ice volume divided into 7 classes (ice winter severity types). The various types of data consulted in the latter case provided ice data of good spatial and temporal resolution. Speerschneider's compilation of data relating to ice conditions in Danish Baltic waters was found to be a valuable source of information. Using a classification table for the periods 1907-1943 and 1947-1992, five of the seven ice winter types have been derived with certainty as they are characterized by typical stages of maximum ice cover throughout the Western Baltic. The Gaussian lowpass-filtered time series of the ice winter index numerals with a 20 year cutoff period shows four periods of varying ice winter severity over a secular range: 1701-1720: slightly increased ice winter severity with regard to the mean of the 1701-1993 time series; this period can be assigned to the end of a cooling phase during ‘Little Ice Age’ which in central Europe peaked in the second half of the 17th c. 1721-1760: ice winter severity is clearly reduced in this period. 1761-1860: ice winter severity is clearly increased (maximum occurs around 1800) towards the end of the ‘Little Ice Age’, associated with increased variability of ice production. 1861-1993: the present-day ice winter regime when three short intervals with increased ice winter severity (the 1890s, 1940s and 1980s) and a period of greatly reduced ice winter severity (between 1900 and the mid-1920s) stand out.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Thirty-two weather diaries written in astronomical calendars in central Europe in the late fifteenth and sixteenth centuries are presented and discussed. Systematic weather observations were promoted by the rise of planetary astronomy and its application in astro-meteorology. The practice of keeping weather diaries spread from Cracow (Poland) to Ingolstadt (Germany) and from there to other universities. The data obtained from these sources provided the backbone for setting up series of precipitation indices for Poland, Germany and Switzerland. Monthly statistics of days with precipitation, snowfall and frost were computed by counting the relevant entries in the most important diaries. The results were compared with either those obtained from instrumental measurements in the same place or with those from modern instrumental measurements in a neighbouring place. The final results show that autumn was considerably colder in the early sixteenth century. April was considerably drier and July was wetter during the period 1508-1531 than during 1901-1960. In order to highlight the impact of weather patterns on grain prices in a year of crisis, the timing of wet and dry spells in southern Poland and southern Germany is compared for the year 1529. Winters became 1.7°C colder from 1564 to 1576 and the month of July tended to be wetter than in 1901-1960. Details noted in the diaries kept between 1585 and 1600 by the astronomers Brahe (near Copenhagen) and Fabricius (in the Ostfriesland region of northwestern Germany) closely agree. It rained more often in June and July and temperatures dropped. The winter months were more frequently dominated by winds from easterly directions, the frequency of snowfall was higher and a deficit occurred in precipitation. This points to a higher frequency of high pressure in the Fennoscandian area with cold air advection from the east or northeast.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 43 (1999), S. 3-4 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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