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The climate-archive dune; sedimentary record of annual wind intensity

Sebastian Lindhorst and Christian Betzler
The climate-archive dune; sedimentary record of annual wind intensity
Geology (Boulder) (September 2016) 44 (9): 711-714

Abstract

Active dunes contain an unread high-resolution archive of past wind strength. Variations in the grain-size spectrum of an active dune through time are compared with historical time series of wind speed. Annually averaged, sediment-derived wind intensity and instrumental records of wind speed show a correlation as high as 0.75. The potential of eolian dunes to gain long-term data series of wind intensity in areas and for time periods lacking an instrumental record is demonstrated by reconstructing 20 (super th) century wind-intensity variations in the southern North Sea area. The approach can be used in both recent and fossil dune systems. Potential applications include the validation of climate models, the reconstruction of supraregional wind systems, and the monitoring of future shifts in the climate system.


ISSN: 0091-7613
EISSN: 1943-2682
Coden: GLGYBA
Serial Title: Geology (Boulder)
Serial Volume: 44
Serial Issue: 9
Title: The climate-archive dune; sedimentary record of annual wind intensity
Affiliation: University of Hamburg, Institute for Geology, Hamburg, Germany
Pages: 711-714
Published: 201609
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
References: 30
Accession Number: 2016-083464
Categories: Quaternary geology
Document Type: Serial
Bibliographic Level: Analytic
Annotation: GSA Data Repository item 2016230
Illustration Description: illus. incl. sketch map
N54°46'00" - N55°02'60", E08°16'60" - E08°30'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
Update Code: 201640

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