Sensing the wind profile

Research output: Book/ReportPh.D. thesis – Annual report year: 2009Research

Standard

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. thesis – Annual report year: 2009Research

Harvard

Pena Diaz, A 2009, Sensing the wind profile. Risø-PhD, no. 45(EN), Risø National Laboratory, Roskilde, Denmark.

APA

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

CBE

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

MLA

Pena Diaz, Alfredo Sensing the wind profile Roskilde, Denmark: Risø National Laboratory. 2009. (Risø-PhD; Journal number 45(EN)).

Vancouver

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

Author

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

Bibtex

@phdthesis{6d7b9e85cd404033a0509736ba289643,
title = "Sensing the wind profile",
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",
note = "Ris{\o}-PhD-45(EN)",
year = "2009",
language = "English",
isbn = "978-87-550-3709-0",
publisher = "Ris{\o} National Laboratory",

}

RIS

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 -