Počet záznamů: 1  

Precipitation variability in the czech land since ad 1500. How strong is the signal contained within documentary sources?

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    0423465 - ÚVGZ 2014 RIV CZ eng C - Konferenční příspěvek (zahraniční konf.)
    Dobrovolný, Petr - Brázdil, Rudolf - Trnka, Miroslav - Kotyza, O. - Valášek, H.
    Precipitation variability in the czech land since ad 1500. How strong is the signal contained within documentary sources?
    Global Change and Resilience: From Impacts to Responses : Proceedings of the 3rd annual Global Change and Resilience Conference. Brno: Global change research centre, Academy of Sciences of the Czech Republic, v. v. i, 2013 - (Stojanov, R.; Žalud, Z.; Cudlín, P.; Farda, A.; Urban, O.; Trnka, M.), s. 95-99. ISBN 978-80-904351-8-6.
    [Global Change and Resilience. Brno (CZ), 22.05.2013-24.05.2013]
    Institucionální podpora: RVO:67179843
    Klíčová slova: documentary evidence * precipitation * reconstruction * Czech Lands
    Kód oboru RIV: EH - Ekologie - společenstva

    Past climate may be reconstructed from a number of proxies. Some of them are “natural archives”, such as tree rings, ice cores and boreholes, most of which are sensitive to air temperature. Other valuable information can be also found in “man-made archives”. Various sources of documentary data very oft en refer not only to temperature but also to other aspects of past weather and climate, such as dry and wet periods. We use the long and homogeneous precipitation series from the recent instrumental period to calibrate precipitation indices derived from older documentary sources. Th e primary objective of this contribution is to provide a quantitative reconstruction of precipitation in the Czech Lands for the last 500 years. Calibration and verifi cation statistics are used to evaluate the strength of the signal. Reconstructed precipitation series are compared with similar Central European documentary-based reconstructions, as well as with reconstructions based on a range of natural proxies.
    Trvalý link: http://hdl.handle.net/11104/0229748

     
     
Počet záznamů: 1  

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