Bibliografías temáticas / Wind profilers

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Literatura académica sobre el tema "Wind profilers"

Autor: Grafiati
Publicado: 25 de mayo de 2024
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Wind profilers"

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Hartten, Leslie M., Paul E. Johnston, Valerie M. Rodríguez Castro, and Paola S. Esteban Pérez. "Postdeployment Calibration of a Tropical UHF Profiling Radar via Surface- and Satellite-Based Methods." Journal of Atmospheric and Oceanic Technology 36, no. 9 (2019): 1729–51. http://dx.doi.org/10.1175/jtech-d-18-0020.1.

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Wind profiling radars are usually not calibrated with respect to reflectivity because such calibrations are both unnecessary for good wind measurements and costly. However, reflectivity from calibrated profilers can reveal many atmospheric attributes beyond winds. Establishing ways to calibrate these radars even after they have been taken out of service would expand the utility of archived profiler data. We have calibrated one operating mode of a 915-MHz profiler deployed at Manus, Papua New Guinea (1992–2001), using two methods. The first method adjusts a radar parameter until the profiler’s
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Monna, W. A. A. "On the use of wind profilers in meteorology." Annales Geophysicae 12, no. 6 (1994): 482–86. http://dx.doi.org/10.1007/s00585-994-0482-9.

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Abstract. As an introduction to this special issue of Annales Geophysicae a review is given of the applicability and performance of wind profilers. In meteorology, wind profilers play an increasingly important role. They can provide upper-wind measurements with an accuracy comparable to radiosonde data, but with a significantly higher temporal resolution. Height coverage and vertical resolution depend on the operating frequency, which, depending on the application, is usually chosen to be around 50, 400 or 1000 MHz. Measurements from stand-alone profilers in sparse data areas as well as data f
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Barth, M. F., R. B. Chadwick, and D. W. van de Kamp. "Data processing algorithms used by NOAA's wind profiler demonstration network." Annales Geophysicae 12, no. 6 (1994): 518–28. http://dx.doi.org/10.1007/s00585-994-0518-1.

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Abstract. The National Oceanic and Atmospheric Administration's (NOAA) Wind Profiler Demonstration Network consists of 32 wind profiling radars, based primarily in the central United States. The network is being used to determine the operational feasibility and characteristics of a possible future nationwide profiler network. Data processing is performed both at the individual profiler sites and at a central hub processing system. This paper documents the algorithms used at the profilers to produce profiles of the moments of the velocity spectrum every 6 minutes, as well as those used on the h
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Chen, Zhao-Yu, Yen-Hsyang Chu, and Ching-Lun Su. "Intercomparisons of Tropospheric Wind Velocities Measured by Multi-Frequency Wind Profilers and Rawinsonde." Atmosphere 12, no. 10 (2021): 1284. http://dx.doi.org/10.3390/atmos12101284.

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Concurrent measurements of three-dimensional wind velocities made with three co-located wind profilers operated at frequencies of 52 MHz, 449 MHz, and 1.29 GHz for the period 12–16 September 2017 are compared for the first time in this study. The velocity–azimuth display (VAD) method is employed to estimate the wind velocities. The result shows that, in the absence of precipitation, the root mean square difference (RMSD) in the horizontal wind speed velocities U and wind directions D between different pairs of wind profilers are, respectively, in the range of 0.94–0.99 ms−1 and 7.7–8.3°, and t
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Schafer, Robert, Susan K. Avery, Kenneth S. Gage, and George N. Kiladis. "Wind Profiler Observations over the Central Equatorial Pacific: Optimizing Processing to Improve Quality and Height Coverage." Journal of Atmospheric and Oceanic Technology 24, no. 10 (2007): 1710–25. http://dx.doi.org/10.1175/jtech2072.1.

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Abstract UHF (boundary layer) and VHF (troposphere–stratosphere) wind profilers have operated at Christmas Island (2°N, 157°W) in the central equatorial Pacific from 1986 to 2002. Observed profiles of winds are sparse over the tropical oceans, but these are critical for understanding convective organization and the interaction of convection and waves. While the zonal winds below about 10 km have previously shown good agreement with the National Centers for Environmental Prediction–National Center for Atmospheric Research (NCEP–NCAR) reanalysis (RI), significant differences were found above a h
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Wang, Cheng, Min Chen, and Yaodeng Chen. "Impact of Combined Assimilation of Wind Profiler and Doppler Radar Data on a Convective-Scale Cycling Forecasting System." Monthly Weather Review 150, no. 2 (2022): 431–50. http://dx.doi.org/10.1175/mwr-d-20-0383.1.

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Abstract The two types of wind observations, profiler and radar radial velocity, have been successfully assimilated into numerical weather prediction (NWP) systems. However, the added value of profiler data, especially from a densely deployed profiler network, is unknown when assimilated together with Doppler radar radial velocity. In this article, two combined assimilation strategies of profilers along with radar radial winds are compared within a convective-scale data assimilation (DA) framework. In strategy I, the profiler data are assimilated with conventional observations to generate an i
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Adachi, Ahoro, Takahisa Kobayashi, Kenneth S. Gage, et al. "Evaluation of Three-Beam and Four-Beam Profiler Wind Measurement Techniques Using a Five-Beam Wind Profiler and Collocated Meteorological Tower." Journal of Atmospheric and Oceanic Technology 22, no. 8 (2005): 1167–80. http://dx.doi.org/10.1175/jtech1777.1.

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Abstract In this paper a five-beam wind profiler and a collocated meteorological tower are used to estimate the accuracy of four-beam and three-beam wind profiler techniques in measuring horizontal components of the wind. In the traditional three-beam technique, the horizontal components of wind are derived from two orthogonal oblique beams and the vertical beam. In the less used four-beam method, the horizontal winds are found from the radial velocities measured with two orthogonal sets of opposing coplanar beams. In this paper the observations derived from the two wind profiler techniques ar
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St-James, Judy S., and Stéphane Laroche. "Assimilation of Wind Profiler Data in the Canadian Meteorological Centre’s Analysis Systems." Journal of Atmospheric and Oceanic Technology 22, no. 8 (2005): 1181–94. http://dx.doi.org/10.1175/jtech1765.1.

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Abstract Real-time horizontal wind observations from the National Oceanic and Atmospheric Administration’s (NOAA’s) Profiler Network (NPN) are assessed in preparation for their assimilation in the Canadian Meteorological Centre (CMC) analysis systems. As a first step, radiosonde winds from 20 stations were compared to the central U.S. profiler stations over the 2001/02 winter season. It was found that profilers are at least as good as conventional radiosonde data. The 2001/02 winter season data were also used to examine the vertical correlation structure of the observation error for profilers.
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Goodrich, Robert K., Corrinne S. Morse, Larry B. Cornman, and Stephen A. Cohn. "A Horizontal Wind and Wind Confidence Algorithm for Doppler Wind Profilers." Journal of Atmospheric and Oceanic Technology 19, no. 3 (2002): 257–73. http://dx.doi.org/10.1175/1520-0426-19.3.257.

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Abstract Boundary layer wind profilers are increasingly being used in applications that require high-quality, rapidly updated winds. An example of this type of application is an airport wind hazard warning system. Wind shear can be a hazard to flight operations and is also associated with the production of turbulence. A method for calculating wind and wind shear using a linear wind field assumption is presented. This method, applied to four- or five-beam profilers, allows for the explicit accounting of the measurable shear terms. An error analysis demonstrates why some shears are more readily
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Baray, Jean-Luc, Yves Pointin, Joël Van Baelen, et al. "Case Study and Climatological Analysis of Upper-Tropospheric Jet Stream and Stratosphere–Troposphere Exchanges Using VHF Profilers and Radionuclide Measurements in France." Journal of Applied Meteorology and Climatology 56, no. 11 (2017): 3081–97. http://dx.doi.org/10.1175/jamc-d-16-0353.1.

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AbstractThe authors present a climatological analysis of tropospheric horizontal wind profiles and jet stream events using long series of wind profiles from two VHF profilers located in France: Lannemezan (2001–14) and Opme (1999–2014). A case study of jet stream and stratospheric intrusion of air into the troposphere that occurred in January 2013 is first described and demonstrates the capability of the VHF profilers to detect jet stream events. The climatology study over the two sites reveals the strongest values of seasonal wind during winter (21.4 m s−1 at 8.7-km height at Opme; 25.1 m s−1
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Tesis sobre el tema "Wind profilers"

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Lee, Christopher Francis. "Use of wind profilers to quantify atmospheric turbulence." Thesis, University of Manchester, 2011. https://www.research.manchester.ac.uk/portal/en/theses/use-of-wind-profilers-to-quantify-atmospheric-turbulence(d6a12ed2-533a-4dae-9f0d-747bc0b4c725).html.

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Doppler radar wind profilers are already widely used to measure atmospheric winds throughout the free troposphere and stratosphere. Several methods have been developed to quantify atmospheric turbulence with such radars, but to date they have remained largely un-tested; this thesis presents the first comprehensive validation of one such method. Conventional in-situ measurements of turbulence have been concentrated in the surface layer, with some aircraft and balloon platforms measuring at higher altitudes on a case study basis. Radars offer the opportunity to measure turbulence near continuous
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Adachi, Ahoro. "An observational study of mesoscale phenomena with UHF wind profilers." 京都大学 (Kyoto University), 2007. http://hdl.handle.net/2433/136957.

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Renggono, Findy. "Study on precipitating clouds over Kototabang, west Sumatra observed by wind profilers." 京都大学 (Kyoto University), 2006. http://hdl.handle.net/2433/144127.

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Leblanc, Sylvain G. "Studies of turbulence with a wind profiler." Thesis, McGill University, 1994. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=22755.

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In Doppler radar analysis of the atmosphere the spectrum width is rarely used but it contains information about turbulence. Turbulence is not the only effect that contributes to the broadening of the spectrum. Another effect is the cross-beam wind, which can be dominant in broad-beam radars such as wind profilers. Once this effect is removed, the so-called residual width then serves as an indication of turbulence. A large snowstorm is used in this study for the computation of the residual width. Strong wind and wind shear were observed during the storm. The time-height pattern of residual widt
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Domps, Baptiste. "Identification et détection de phénomènes transitoires contenus dans des mesures radar à faible rapport signal à bruit : Applications conjointes aux problématiques océanographique et atmosphérique." Electronic Thesis or Diss., Toulon, 2021. http://www.theses.fr/2021TOUL0001.

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L'observation de la dynamique de l'atmosphère et de la surface de l'océan peut être réalisée par télédétection radar. L'approche habituelle consiste, dans les deux cas, à calculer numériquement le spectre Doppler des échos temporels reçus à l'aide d'une transformée de Fourier discrète. Bien que satisfaisante pour la plupart des applications, cette méthode ne convient pas pour l'observation de phénomènes transitoires, plus courts que le temps d'intégration nécessaire à l'observation radar. Nous utilisons une technique alternative, basée sur une représentation autorégressive des séries temporell
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Soler-Bientz, Rolando. "Evaluation of the wind patterns over the Yucatán Peninsula in México." Thesis, Loughborough University, 2010. https://dspace.lboro.ac.uk/2134/5988.

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Wind power is seen as one of the most effective means available to combat the twin crises of global climate change and energy security. The annual market growth has established wind power as the leading renewable energy technology. Due to the availability of sparsely populated and flat open terrain, the Yucatán Peninsula located in eastern México is a promising region from the perspective of wind energy development but no comprehensive assessment of wind resource has been previously published. A basic requirement when developing wind power projects is to study the main characteristic parameter
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Ritlop, Robert. "Toward the aerodynamic shape optimization of wind turbine profiles." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=66672.

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This research presents automatic aerodynamic shape optimization results for the NREL S809 wind turbine profile. The objective of this re-design was to improve the total lift to drag ratio for steady low-Mach number flows. This research sets the groundwork for the development of a multidisciplinary optimization framework for complete wind turbine rotors. To develop the aerodynamic design framework for the wind turbine applications, low-Mach preconditioning and Menter's k-omega SST turbulence model have been implemented into the flow solver. A preconditioned discrete viscous ad
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Ignace, Richard, R. Bessey, and C. Price. "Modeling Forbidden Line Emission Profiles from Colliding Wind Binaries." Digital Commons @ East Tennessee State University, 2009. https://dc.etsu.edu/etsu-works/6266.

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This paper presents calculations for forbidden emission-line profile shapes arising from colliding wind binaries. The main application is for systems involving a Wolf–Rayet (WR) star and an OB star companion. The WR wind is assumed to dominate the forbidden line emission. The colliding wind interaction is treated as an Archimedean spiral with an inner boundary. Under the assumptions of the model, the major findings are as follows. (i) The redistribution of the WR wind as a result of the wind collision is not flux conservative but typically produces an excess of line emission; however, this exc
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Stec, Jeffrey D. "Wind profiler study of the central California sea/land breeze /\." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1996. http://handle.dtic.mil/100.2/ADA317994.

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Thesis (M.S. in Meteorology and Physical Oceanography) Naval Postgraduate School, September. 1996.<br>Thesis advisor(s): Carlyle H. Wash. "September 1996." Includes bibliographical references (p. 97-100). Also available online.
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Low, David J. "Studies of the lower atmosphere with a VHF wind profiler /." Title page, abstract and contents only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09phl9121.pdf.

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Libros sobre el tema "Wind profilers"

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B, Chadwick Russell, and Forecast Systems Laboratory (U.S.), eds. Coherent interference tests for wind profilers. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Forecast Systems Laboratory, 1992.

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Strauch, R. G. Radar wind profilers in the Colorado network. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Wave Propagation Laboratory, 1985.

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Gossard, Earl E. Automated editing of spectra from wind profilers. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1997.

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E, Gaines Steven, Hipskind R. Stephen, United States. National Aeronautics and Space Administration., and San Jose State University. Meteorology Dept., eds. An atlas of objectively analyzed atmospheric cross sections 1973-1980. National Aeronautics and Space Administration, 1985.

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Wuertz, David B. Editing wind profiler measurements. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Wave Propagation Laboratory, 1989.

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Wuertz, David B. Editing wind profiler measurements. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Wave Propagation Laboratory, 1989.

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Wuertz, David B. Editing wind profiler measurements. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Wave Propagation Laboratory, 1989.

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Baillie, S. W. An investigation of lateral tracking techniques, flight directors and automatic control coupling on decelerating IFR approaches for rotorcraft. National Aeronautical Establishment, 1988.

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J, Murphy Patrick, FWG Associates, and George C. Marshall Space Flight Center., eds. Analysis of wind profile measurements from an instrumented aircraft: Interim final report. FWG Associates, Inc., 1991.

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Graham, R. Electrical demand profiles at six wind monitoring sites. Scottish Agricultural College, Engineering Dept., 1999.

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Capítulos de libros sobre el tema "Wind profilers"

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Gu, Taofeng, Jiamin Wang, Feng Shen, et al. "3D Wind Field Construction with Multiple Wind Profilers." In Lecture Notes in Electrical Engineering. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-99-7505-1_47.

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Emeis, Stefan, and Matthias Turk. "Comparison of Logarithmic Wind Profiles and Power Law Wind Profiles and their Applicability for Offshore Wind Profiles." In Wind Energy. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-33866-6_11.

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Lehmann, Volker, and William Brown. "Radar Wind Profiler." In Springer Handbook of Atmospheric Measurements. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-52171-4_31.

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Tambke, J., J. A. T. Bye, Bernhard Lange, and J. O. Wolff. "Wind Speed Profiles above the North Sea." In Wind Energy. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-33866-6_5.

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Emeis, Stefan. "Vertical Profiles Over Flat Terrain." In Wind Energy Meteorology. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-72859-9_3.

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Emeis, Stefan. "Vertical Profiles Over Flat Terrain." In Wind Energy Meteorology. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30523-8_3.

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Bourguet, Rémi, Guillaume Martinat, Gilles Harran, and Marianna Braza. "Aerodynamic Multi-Criteria Shape Optimization of VAWT Blade Profile by Viscous Approach." In Wind Energy. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-33866-6_39.

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Bedka, Kristopher, John Marketon, Sammy Henderson, and Michael Kavaya. "AWP: NASA’s Aerosol Wind Profiler Coherent Doppler Wind Lidar." In Space-based Lidar Remote Sensing Techniques and Emerging Technologies. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-53618-2_3.

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Sepe, Vincenzo, Alberto M. Avossa, Fabio Rizzo, and Francesco Ricciardelli. "Can Wind Lidars Be Used to Calibrate Mean Wind Profiles?" In Lecture Notes in Civil Engineering. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-53059-3_19.

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Barreal Pernas, Jesús, and Gil Jannes. "Comparison of international tourist profiles in the Spanish wine and olive oil PDOs." In Tourism marketing in Western Europe. CABI, 2021. http://dx.doi.org/10.1079/9781789248753.0005.

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Abstract This chapter, by Jesús Barreal Pernas and Gil Jannes, deals with gastro-tourism in Spain and studies the international tourist profile in the Spanish wine and olive oil Protected Destinations of Origin (PDOs). Specifically, the study focuses on regions that have such PDOs and examines the differences and similarities among the profiles of international tourists that visit them. The study concludes with a classification of four clusters according to demographic, travel and motivational characteristics of tourists in the particular area.
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Actas de conferencias sobre el tema "Wind profilers"

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Bukrin, Ilya V., Sergey I. Kudinov, Viacheslav E. Ivanov, and Oleg V. Plokhikh. "Main Characteristics of Clear Sky Wind Profiler." In 2025 IEEE Ural-Siberian Conference on Biomedical Engineering, Radioelectronics and Information Technology (USBEREIT). IEEE, 2025. https://doi.org/10.1109/usbereit65494.2025.11054102.

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STRAUCH, R., D. MERRITT, K. MORAN, P. MAY, and B. WEBER. "Doppler radar wind profilers for support of flight operations." In 27th Aerospace Sciences Meeting. American Institute of Aeronautics and Astronautics, 1989. http://dx.doi.org/10.2514/6.1989-713.

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Lei Wu, Xuhui Zhou, and Furan Wang. "Primary analysis of the comparison test of wind profilers Made in China." In 2011 International Conference on Information Science and Technology (ICIST). IEEE, 2011. http://dx.doi.org/10.1109/icist.2011.5765324.

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Westwater, E. R., and B. B. Stankov. "Recent Results in Combined Ground-based and Satellite Remote Sensing." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1993. http://dx.doi.org/10.1364/orsa.1993.mc.2.

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The implementation of the Wind Profiler Demonstration Network [1] is an indication of the increased reliance of the operational community on remote sensors. The Wind Profilers themselves can measure winds to about 16 km with a spatial resolution of 300-900 m on an hourly basis; their horizontal spacings vary from about 200 to 300 km. If the same spatial and temporal coverage of temperature, water vapor and clouds could be achieved many of the needs of forecasters and researchers could be met. However, even if the ambitious goal of measuring both dynamic and thermodynamic variables from a netwo
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Flowers, Wayne, Elaine Santantonio, Glenn Hoidale, et al. "Wind measurements from Doppler radar profilers and rawinsondes - A comparison of 50-MHz and 404-MHz profilers and rawinsonde data at White Sands Missile Range." In Aerospace Sensing, edited by Anton Kohnle and Walter B. Miller. SPIE, 1992. http://dx.doi.org/10.1117/12.137899.

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Zarate, Luz, Shejun Fan, Pak Leung, et al. "Hurricane Ida Passage Over Gulf of Mexico Oil and Gas Offshore Facilities." In Offshore Technology Conference. OTC, 2022. http://dx.doi.org/10.4043/31757-ms.

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Abstract Hurricane Ida made landfall in Port Fourchon, Louisiana, as a Category 4 hurricane on August 29th, 2021, traveling over some offshore oil and gas facilities on its path. Shell Exploration and Production's offshore oil and gas installations in the Gulf of Mexico (GoM) have the most comprehensive suite of metocean instrumentation in the region, including wave and wind systems that captured the passage of hurricane Ida. This paper analyzes the wind and wave conditions measured by some Shell facilities located along the path of hurricane Ida. The number of LiDAR wind profilers and their s
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Zarate, Luz, Shejun Fan, Pak Leung, et al. "Hurricane Ida Passage Over Gulf of Mexico Oil and Gas Offshore Facilities." In Offshore Technology Conference. OTC, 2022. http://dx.doi.org/10.4043/31757-ms.

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Abstract Hurricane Ida made landfall in Port Fourchon, Louisiana, as a Category 4 hurricane on August 29th, 2021, traveling over some offshore oil and gas facilities on its path. Shell Exploration and Production's offshore oil and gas installations in the Gulf of Mexico (GoM) have the most comprehensive suite of metocean instrumentation in the region, including wave and wind systems that captured the passage of hurricane Ida. This paper analyzes the wind and wave conditions measured by some Shell facilities located along the path of hurricane Ida. The number of LiDAR wind profilers and their s
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Sinsabvarodom, Chana, Bernt J. Leira, Knut V. Høyland, et al. "Development of the Environmental Contour for Ice Drift Speed and Wind Speed." In ASME 2024 43rd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2024. http://dx.doi.org/10.1115/omae2024-122581.

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Abstract The purpose of this study is to develop environmental contours for ice drift speed and wind speed. The drift of sea ice is naturally influenced by various external forces, including wind stress at the air-ice boundary, water stress at the water-ice boundary, the Coriolis force, pressure gradients caused by sea surface tilting, and internal stress within the sea ice itself. Typically, sea ice drifts at a rate of approximately 2–3% of the wind speed (as measured at a height of 10 meters above the ocean surface) in the Arctic region. The Nansen number, which relates to the magnitude of t
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Johnson, Steven C. "Space Shuttle Wind Profiler." In Coherent Laser Radar. Optica Publishing Group, 1991. http://dx.doi.org/10.1364/clr.1991.tud3.

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Knowledge of winds is required to reduce aerodynamic loads on the Space Shuttle during launch. Knowledge of winds is also required to safely land the unpowered orbiter. Balloons are currently used in both instances to produce the necessary wind profiles. The balloons require an hour to rise through the altitude range, sometimes drifting far from the area where the wind measurement is desired. As a result, the correlation between the actual winds encountered by the vehicle and those measured is reduced. NASA is investigating the potential of alternate wind sensors to produce more local wind mea
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Sinsabvarodom, Chana, Bernt J. Leira, Knut V. Høyland, Wei Chai, Arvid Naess, and Gowtham Radhakrishnan. "On the Relationship Between Spectral Models of Ice Drift and Wind Turbulence." In ASME 2023 42nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2023. http://dx.doi.org/10.1115/omae2023-104751.

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Abstract At present, there is quite limited research activity related to mathematical models of the ice drift spectrum. The intention of this work is to propose a novel mathematical model of a generalized ice drift speed spectrum to describe the ice drift behavior in the frequency domain. The drift of sea ice is naturally influenced by external forces such as wind stress at the air-ice interface, water stress at the water-ice interface, the Coriolis force, pressure gradients due to sea surface tilting, and internal stress within the sea ice itself. Typically, wind dominates the ice drift at hi
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Informes sobre el tema "Wind profilers"

1

Williams, Christopher. Advanced Precipitation and Boundary Layer Data Products Derived from ARM Radar Wind Profilers. Office of Scientific and Technical Information (OSTI), 2024. https://doi.org/10.2172/2477697.

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Coulter, R. L., B. M. Lesht, M. L. Wesely, D. R. Cook, D. J. Holdridge, and T. J. Martin. Performance of radar wind profilers, radiosondes, and surface flux stations at the SGP CART site. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/81006.

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Boss, Emmanuel. Shelf-Slope Physical/Biological Response to Monsoonal Wind Forcing and Riverine Inflow - 4D Sampling with Towed Profilers and Autonomous Gliders Off Vietnam. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada572165.

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Jones, Burton H. Shelf-Slope Physical/Biological Response to Monsoonal Wind Forcing and Riverine Inflo - 4D Sampling with Towed Profilers and Autonomous Gliders Off Vietnam. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada572175.

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Boss, Emmanuel. Shelf-Slope Physical/Biological Response to Monsoonal Wind Forcing and Riverine Inflow - 4D Sampling with Towed Profilers and Autonomous Gliders Off Vietnam. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada601171.

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Boss, Emmanuel, and Burton H. Jones. Shelf-Slope Physical/Biological Response to Monsoonal Wind Forcing and Riverine Inflow - 4D Sampling with Towed Profilers and Autonomous Gliders off Vietnam. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada601223.

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Petersen, Guðrún. Alviðruhamrar – Meteorological conditions. Icelandic Meteorological Office, 2025. https://doi.org/10.33112/damc5680.

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This report is written for EP Power Minerals ehf. that is planning activities in in SoutheastIceland. Themeteorological conditions inMýrdalssandur and Alviðruhamrar in SoutheastIceland are analysed using observations from two automatic long-term weather stations and reanalysis data from the CARRA reanalysis project. The emphasis is on the wind conditions. The climate of the region is mild and wet. There are three main wind directions, northerly, easterly and southwesterly. Winds from the north are in general dry and winds form the east wet. However, depending on the general weather conditions
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Ziegler, Nancy, Nicholas Webb, Adrian Chappell, and Sandra LeGrand. Scale invariance of albedo-based wind friction velocity. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/40499.

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Obtaining reliable estimates of aerodynamic roughness is necessary to interpret and accurately predict aeolian sediment transport dynamics. However, inherent uncertainties in field measurements and models of surface aerodynamic properties continue to undermine aeolian research, monitoring, and dust modeling. A new relation between aerodynamic shelter and land surface shadow has been established at the wind tunnel scale, enabling the potential for estimates of wind erosion and dust emission to be obtained across scales from albedo data. Here, we compare estimates of wind friction velocity (u*)
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Helmus, Jonathan, and Virendra P. Ghate. Improved Estimates of Moments and Winds from Radar Wind Profiler. Office of Scientific and Technical Information (OSTI), 2017. http://dx.doi.org/10.2172/1343609.

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Law, Daniel, Frank Sanders, Gary Patrick, and Michael Richmond. Measurements of Wind Profiler EMC Characteristics. Institute for Telecommunication Sciences, 1994. https://doi.org/10.70220/gpcnld43.

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