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      Was there a ?medieval warm period?, and if so, where and when?

      Author(s): ,
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      Journal: Climatic Change
      Publisher: Springer Nature

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          Lanczos Filtering in One and Two Dimensions

          Claude E. Duchon (1979)
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            The early medieval warm epoch and its sequel

            H.H. Lamb (1965)
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              Paleoclimatic Inferences from Long Tree-Ring Records: Intersite comparison shows climatic anomalies that may be linked to features of the general circulation.

              C Lamarche (1974)
              Tree-ring data contribute to a better understanding of the nature of past climatic variations. Annual ring records several thousand years long can be constructed for a few areas, but interpretation of them requires the development of new approaches. For example, a single record of average ring width in the upper tree line environment provides a guide to past temperature fluctuations. However, comparison of this record with another, that of the arid lower forest border, from the same area permits characterization of associated precipitation and temperature anomalies that may, in turn, be linked to features of the general circulation. Other approaches that promise to be very fruitful include study of the variation of ring-width statistics through time, investigation of the physical and chemical properties of wood, and combined multivariate analysis of data for a variety of paleoclimatic indicators.
              Article 0 comments Cited 128 times – based on 0 reviews     Review now
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                Author and article information

                Journal
                Title: Climatic Change
                Abbreviated Title: Climatic Change
                Publisher: Springer Nature
                ISSN (Print): 0165-0009
                ISSN (Electronic): 1573-1480
                Publication date Created: March 1994
                Publication date (Print): March 1994
                Volume: 26
                Issue: 2-3
                Pages: 109-142
                Article
                DOI: 10.1007/BF01092410
                SO-VID: a392e795-07fb-4ff7-9d1d-bc245ad0465a
                Copyright © © 1994
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