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  • 1
    Online-Ressource
    Online-Ressource
    Schweizerbart ; 2007
    In:  Meteorologische Zeitschrift Vol. 16, No. 4 ( 2007-08-30), p. 367-373
    In: Meteorologische Zeitschrift, Schweizerbart, Vol. 16, No. 4 ( 2007-08-30), p. 367-373
    Materialart: Online-Ressource
    ISSN: 0941-2948
    Originaltitel: The vertical structure of turbulent momentum flux in the lower part of the atmospheric boundary layer
    RVK:
    Sprache: Englisch , Englisch
    Verlag: Schweizerbart
    Publikationsdatum: 2007
    ZDB Id: 511391-X
    ZDB Id: 2045168-4
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2013
    In:  Journal of Atmospheric and Oceanic Technology Vol. 30, No. 9 ( 2013-09-01), p. 1970-1977
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 30, No. 9 ( 2013-09-01), p. 1970-1977
    Kurzfassung: Continuous sodar measurements of wind profiles have been carried out at the Zvenigorod Scientific Station of the Obukhov Institute of Atmospheric Physics since 2008. The station is located in a slightly inhomogeneous rural area about 45 km west of Moscow, Russia. The data were used to determine the parameters of wind and turbulence within low-level jets in the stable atmospheric boundary layer (ABL). Along with the mean velocity profiles, the profiles of variances of wind speed components from the sodar and the profiles of temperature from a microwave radiometer have been used to quantify turbulence and thermal stratification. Data from two sonic anemometers were used to get the near-surface parameters. The typical standard deviation of the vertical wind component σw within the low-level jet is about 5% of the maximum wind speed in the jet. No noticeable vertical variation of σw across the jets was detected in several earlier sodar campaigns, and it was not found in the present study. An increase in horizontal variances was detected in zones of substantial wind shear, which agrees with earlier published lidar data. Quasi-periodic structures in the sodar return signal, which appear in sodar echograms as braid-shaped patterns, were found to emerge preferably when a substantial increase of wind shear occurs at the top of the stable ABL. The braid patterns in the sodar echograms were not accompanied by any noticeable increase of observed σw, which disagrees with earlier data and indicates that such patterns may originate from various phenomena.
    Materialart: Online-Ressource
    ISSN: 0739-0572 , 1520-0426
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2013
    ZDB Id: 2021720-1
    ZDB Id: 48441-6
    Standort Signatur Einschränkungen Verfügbarkeit
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