On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer

Kinetic energy spectra of the horisontal wind vector were estimated from time series measured along the Risø 123 m meteorological tower throughout ten years. Also measurements from other localities (Station Nord, Greenland, and Karlstrup, Zealand) were uaed. Spectra and methods are presented and dis...

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Bibliographic Details
Main Author: Lundtang Petersen, Erik
Format: Book
Language:English
Published: Risø National Laboratory 1975
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/4851c4cc-8cec-4c8d-b104-999b93ce4fd7
https://backend.orbit.dtu.dk/ws/files/53636507/ris_285.pdf
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spelling ftdtupubl:oai:pure.atira.dk:publications/4851c4cc-8cec-4c8d-b104-999b93ce4fd7 2023-05-15T16:29:18+02:00 On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer Lundtang Petersen, Erik 1975 application/pdf https://orbit.dtu.dk/en/publications/4851c4cc-8cec-4c8d-b104-999b93ce4fd7 https://backend.orbit.dtu.dk/ws/files/53636507/ris_285.pdf eng eng Risø National Laboratory info:eu-repo/semantics/openAccess Lundtang Petersen , E 1975 , On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer . Denmark. Forskningscenter Risoe. Risoe-R , no. 285 , Risø National Laboratory , Roskilde, Denmark . Risø-R-285 Risø-285 Risø report 285 book 1975 ftdtupubl 2022-08-14T08:10:26Z Kinetic energy spectra of the horisontal wind vector were estimated from time series measured along the Risø 123 m meteorological tower throughout ten years. Also measurements from other localities (Station Nord, Greenland, and Karlstrup, Zealand) were uaed. Spectra and methods are presented and discussed. Emphasis is laid on the gain in information which is achieved when the components of the wind vector are considered rather than just the wind speed. Spectral equations in the frequency domain are derived from the equations of motion. B is shown how a ratio including the Coriolia parameter, the quadrature spectrum of the components, the energy spectrum, and the frequency can be used to determine the explicit effect of the rotating of the earth on the kinetic energy spectrum. The wind structure in thsSoundary layer, as measured at the Risø site, audits relation to the diurnal cycle and horisontal inhomogenslttss of surface temperature are Investigated. The date reveal an exceptionally large turning of the wind with the height above the ground. It is shown that this feature can be given a phenomsnologlcal description by making an analogy to the thermal wind effect. Book Greenland Technical University of Denmark: DTU Orbit Greenland Station Nord ENVELOPE(-16.663,-16.663,81.599,81.599)
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
topic Risø-R-285
Risø-285
Risø report 285
spellingShingle Risø-R-285
Risø-285
Risø report 285
Lundtang Petersen, Erik
On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
topic_facet Risø-R-285
Risø-285
Risø report 285
description Kinetic energy spectra of the horisontal wind vector were estimated from time series measured along the Risø 123 m meteorological tower throughout ten years. Also measurements from other localities (Station Nord, Greenland, and Karlstrup, Zealand) were uaed. Spectra and methods are presented and discussed. Emphasis is laid on the gain in information which is achieved when the components of the wind vector are considered rather than just the wind speed. Spectral equations in the frequency domain are derived from the equations of motion. B is shown how a ratio including the Coriolia parameter, the quadrature spectrum of the components, the energy spectrum, and the frequency can be used to determine the explicit effect of the rotating of the earth on the kinetic energy spectrum. The wind structure in thsSoundary layer, as measured at the Risø site, audits relation to the diurnal cycle and horisontal inhomogenslttss of surface temperature are Investigated. The date reveal an exceptionally large turning of the wind with the height above the ground. It is shown that this feature can be given a phenomsnologlcal description by making an analogy to the thermal wind effect.
format Book
author Lundtang Petersen, Erik
author_facet Lundtang Petersen, Erik
author_sort Lundtang Petersen, Erik
title On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
title_short On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
title_full On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
title_fullStr On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
title_full_unstemmed On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
title_sort on the kinetic energy spectrum of atmospheric motions in the planetary boundary layer
publisher Risø National Laboratory
publishDate 1975
url https://orbit.dtu.dk/en/publications/4851c4cc-8cec-4c8d-b104-999b93ce4fd7
https://backend.orbit.dtu.dk/ws/files/53636507/ris_285.pdf
long_lat ENVELOPE(-16.663,-16.663,81.599,81.599)
geographic Greenland
Station Nord
geographic_facet Greenland
Station Nord
genre Greenland
genre_facet Greenland
op_source Lundtang Petersen , E 1975 , On the kinetic energy spectrum of atmospheric motions in the planetary boundary layer . Denmark. Forskningscenter Risoe. Risoe-R , no. 285 , Risø National Laboratory , Roskilde, Denmark .
op_rights info:eu-repo/semantics/openAccess
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