Sensing the wind profile

    Research output: Book/ReportPh.D. thesisResearch

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    Abstract

    This thesis consists of two parts. The first is a synopsis of the theoretical progress of the study that is based on a number of journal papers. The papers, which constitute the second part of the report, aim to analyze, measure, and model the wind prole in and beyond the surface layer by combining observations from cup anemometers with lidars. The lidar is necessary to extend the measurements on masts at the Horns Rev offshore wind farm and over at land at Høvsøre, Denmark. Both sensing techniques show a high degree of agreement for wind speed measurements performed at either sites. The wind speed measurements are averaged for several stability conditions and compare well with the surface-layer wind profile. At Høvsøre, it is sufficient to scale the wind speed with the surface friction velocity, whereas at Horns Rev a new scaling is added, due to the variant roughness length. This new scaling is coupled to wind prole models derived for flow over the sea and tested against the wind proles up to 160 m at Horns Rev. The models, which account for the boundary-layer height in stable conditions, show better agreement with the measurements than compared to the traditional theory. Mixing-length parameterizations for the neutral wind prole compare well with length-scale measurements up to 300 m at Høvsøre and 950 m at Leipzig. The mixing-length-derived wind proles strongly deviate from the logarithmic wind prole, but agree better with the wind speed measurements. The length-scale measurements are compared to the length scale derived from a spectral analysis performed up to 160 m at Høvsøre showing high agreement. Mixing-length parameterizations are corrected to account for stability and used to derive wind prole models. These compared better to wind speed measurements up to 300 m at Høvsøre than the surface-layer wind prole. The boundary-layer height is derived in nearneutral and stable conditions based on turbulent momentum uxes only and in unstable conditions based on profiles of aerosol backscatter from ceilometer measurements. The lidar measuring technique is used to estimate momentum flux, showing high agreement compared to measurements at Høvsøre and Horns Rev when the filtering effects of the lidar are taken into account.
    Original languageEnglish
    Place of PublicationRoskilde, Denmark
    PublisherRisø National Laboratory
    Number of pages80
    ISBN (Print)978-87-550-3709-0
    Publication statusPublished - 2009
    SeriesRisø-PhD
    Number45(EN)

    Bibliographical note

    Risø-PhD-45(EN)

    Keywords

    • Wind energy
    • Meteorology
    • Risø-PhD-45(EN)
    • Risø-PhD-45
    • Risø-PhD-0045

    Cite this

    Pena Diaz, A. (2009). Sensing the wind profile. Roskilde, Denmark: Risø National Laboratory. Risø-PhD, No. 45(EN)
    Pena Diaz, Alfredo. / Sensing the wind profile. Roskilde, Denmark : Risø National Laboratory, 2009. 80 p. (Risø-PhD; No. 45(EN)).
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    abstract = "This thesis consists of two parts. The first is a synopsis of the theoretical progress of the study that is based on a number of journal papers. The papers, which constitute the second part of the report, aim to analyze, measure, and model the wind prole in and beyond the surface layer by combining observations from cup anemometers with lidars. The lidar is necessary to extend the measurements on masts at the Horns Rev offshore wind farm and over at land at H{\o}vs{\o}re, Denmark. Both sensing techniques show a high degree of agreement for wind speed measurements performed at either sites. The wind speed measurements are averaged for several stability conditions and compare well with the surface-layer wind profile. At H{\o}vs{\o}re, it is sufficient to scale the wind speed with the surface friction velocity, whereas at Horns Rev a new scaling is added, due to the variant roughness length. This new scaling is coupled to wind prole models derived for flow over the sea and tested against the wind proles up to 160 m at Horns Rev. The models, which account for the boundary-layer height in stable conditions, show better agreement with the measurements than compared to the traditional theory. Mixing-length parameterizations for the neutral wind prole compare well with length-scale measurements up to 300 m at H{\o}vs{\o}re and 950 m at Leipzig. The mixing-length-derived wind proles strongly deviate from the logarithmic wind prole, but agree better with the wind speed measurements. The length-scale measurements are compared to the length scale derived from a spectral analysis performed up to 160 m at H{\o}vs{\o}re showing high agreement. Mixing-length parameterizations are corrected to account for stability and used to derive wind prole models. These compared better to wind speed measurements up to 300 m at H{\o}vs{\o}re than the surface-layer wind prole. The boundary-layer height is derived in nearneutral and stable conditions based on turbulent momentum uxes only and in unstable conditions based on profiles of aerosol backscatter from ceilometer measurements. The lidar measuring technique is used to estimate momentum flux, showing high agreement compared to measurements at H{\o}vs{\o}re and Horns Rev when the filtering effects of the lidar are taken into account.",
    keywords = "Wind energy, Meteorology, Ris{\o}-PhD-45(EN), Ris{\o}-PhD-45, Ris{\o}-PhD-0045, Meteorologi, Vindenergi",
    author = "{Pena Diaz}, Alfredo",
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    Pena Diaz, A 2009, Sensing the wind profile. Risø-PhD, no. 45(EN), Risø National Laboratory, Roskilde, Denmark.

    Sensing the wind profile. / Pena Diaz, Alfredo.

    Roskilde, Denmark : Risø National Laboratory, 2009. 80 p. (Risø-PhD; No. 45(EN)).

    Research output: Book/ReportPh.D. thesisResearch

    TY - BOOK

    T1 - Sensing the wind profile

    AU - Pena Diaz, Alfredo

    N1 - Risø-PhD-45(EN)

    PY - 2009

    Y1 - 2009

    N2 - This thesis consists of two parts. The first is a synopsis of the theoretical progress of the study that is based on a number of journal papers. The papers, which constitute the second part of the report, aim to analyze, measure, and model the wind prole in and beyond the surface layer by combining observations from cup anemometers with lidars. The lidar is necessary to extend the measurements on masts at the Horns Rev offshore wind farm and over at land at Høvsøre, Denmark. Both sensing techniques show a high degree of agreement for wind speed measurements performed at either sites. The wind speed measurements are averaged for several stability conditions and compare well with the surface-layer wind profile. At Høvsøre, it is sufficient to scale the wind speed with the surface friction velocity, whereas at Horns Rev a new scaling is added, due to the variant roughness length. This new scaling is coupled to wind prole models derived for flow over the sea and tested against the wind proles up to 160 m at Horns Rev. The models, which account for the boundary-layer height in stable conditions, show better agreement with the measurements than compared to the traditional theory. Mixing-length parameterizations for the neutral wind prole compare well with length-scale measurements up to 300 m at Høvsøre and 950 m at Leipzig. The mixing-length-derived wind proles strongly deviate from the logarithmic wind prole, but agree better with the wind speed measurements. The length-scale measurements are compared to the length scale derived from a spectral analysis performed up to 160 m at Høvsøre showing high agreement. Mixing-length parameterizations are corrected to account for stability and used to derive wind prole models. These compared better to wind speed measurements up to 300 m at Høvsøre than the surface-layer wind prole. The boundary-layer height is derived in nearneutral and stable conditions based on turbulent momentum uxes only and in unstable conditions based on profiles of aerosol backscatter from ceilometer measurements. The lidar measuring technique is used to estimate momentum flux, showing high agreement compared to measurements at Høvsøre and Horns Rev when the filtering effects of the lidar are taken into account.

    AB - This thesis consists of two parts. The first is a synopsis of the theoretical progress of the study that is based on a number of journal papers. The papers, which constitute the second part of the report, aim to analyze, measure, and model the wind prole in and beyond the surface layer by combining observations from cup anemometers with lidars. The lidar is necessary to extend the measurements on masts at the Horns Rev offshore wind farm and over at land at Høvsøre, Denmark. Both sensing techniques show a high degree of agreement for wind speed measurements performed at either sites. The wind speed measurements are averaged for several stability conditions and compare well with the surface-layer wind profile. At Høvsøre, it is sufficient to scale the wind speed with the surface friction velocity, whereas at Horns Rev a new scaling is added, due to the variant roughness length. This new scaling is coupled to wind prole models derived for flow over the sea and tested against the wind proles up to 160 m at Horns Rev. The models, which account for the boundary-layer height in stable conditions, show better agreement with the measurements than compared to the traditional theory. Mixing-length parameterizations for the neutral wind prole compare well with length-scale measurements up to 300 m at Høvsøre and 950 m at Leipzig. The mixing-length-derived wind proles strongly deviate from the logarithmic wind prole, but agree better with the wind speed measurements. The length-scale measurements are compared to the length scale derived from a spectral analysis performed up to 160 m at Høvsøre showing high agreement. Mixing-length parameterizations are corrected to account for stability and used to derive wind prole models. These compared better to wind speed measurements up to 300 m at Høvsøre than the surface-layer wind prole. The boundary-layer height is derived in nearneutral and stable conditions based on turbulent momentum uxes only and in unstable conditions based on profiles of aerosol backscatter from ceilometer measurements. The lidar measuring technique is used to estimate momentum flux, showing high agreement compared to measurements at Høvsøre and Horns Rev when the filtering effects of the lidar are taken into account.

    KW - Wind energy

    KW - Meteorology

    KW - Risø-PhD-45(EN)

    KW - Risø-PhD-45

    KW - Risø-PhD-0045

    KW - Meteorologi

    KW - Vindenergi

    M3 - Ph.D. thesis

    SN - 978-87-550-3709-0

    BT - Sensing the wind profile

    PB - Risø National Laboratory

    CY - Roskilde, Denmark

    ER -

    Pena Diaz A. Sensing the wind profile. Roskilde, Denmark: Risø National Laboratory, 2009. 80 p. (Risø-PhD; No. 45(EN)).