Number of the records: 1  

Night-time airflow in a forest canopy near a mountain crest

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    SYSNO ASEP0348522
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleNight-time airflow in a forest canopy near a mountain crest
    Author(s) Sedlák, Pavel (UFA-U) RID, ORCID
    Aubinet, M. (BE)
    Heinesch, B. (BE)
    Janouš, Dalibor (UEK-B) RID, SAI
    Pavelka, Marian (UEK-B) RID, ORCID, SAI
    Potužníková, Kateřina (UFA-U) RID, ORCID
    Yernaux, M. (BE)
    Source TitleAgricultural and Forest Meteorology. - : Elsevier - ISSN 0168-1923
    Roč. 150, č. 5 (2010), s. 736-744
    Number of pages9 s.
    Languageeng - English
    CountryNL - Netherlands
    KeywordsSpruce forest ; Canopy layer ; Slope ; Drainage flow ; Wind profile
    Subject RIVDG - Athmosphere Sciences, Meteorology
    R&D ProjectsIAA300420803 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    KJB3087301 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30420517 - UFA-U, BC-A (2005-2011)
    AV0Z60870520 - UEK-B (2005-2011)
    UT WOS000278244400010
    DOI10.1016/j.agrformet.2010.01.014
    AnnotationNight-time airflow within a deep and dense canopy near the top of a mountain ridge is investigated based on measurements at Bily Kriz, Czech Republic. A decoupled two-layer structure of canopy flow typically develops at night. While the above-canopy flow is most frequently an upslope-directed larger-scale flow over the ridge, the lower-canopy flow is downslope. However, the lower-canopy flow can be forced upslope when the wind speed above the canopy exceeds a well-defined limit. Less frequently, on the lee slope to the larger-scale flow, both the above-canopy and the lower-canopy flow are usually downslope, although a flow reversal in the lower canopy is also observed, accompanied with a large shear stress (friction velocity) above the canopy. We introduce a simple diagnostic model, which gives realistic values of the downslope or upslope direction and speed of the lower-canopy flow that agree well with the measurements.
    WorkplaceInstitute of Atmospheric Physics
    ContactKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Year of Publishing2011
Number of the records: 1  

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