REVIEW 3 major objections 4 minor 63 references
Set-up and Characterisation of Atmospheric Boundary Layers in the 10'x5' Wind Tunnel
T0 review · 3 major / 4 minor · reviewed 2026-08-11 · deepseek-v4-flash
Pith's one-line read This paper claims that Irwin spires alone, with no floor roughness, can generate marine atmospheric boundary layers matching target velocity and turbulence profiles, and that a multi-hole probe measures the flow nearly as accurately as a…
desk verdict Solid incremental wind-tunnel study; the 'reliable marine ABL' claim needs the missing spectral/length-scale evidence before it lands. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The load-bearing object is the Irwin spire: a set of triangular plates mounted at the wind tunnel inlet whose blockage produces a shear layer and turbulence that develop into a boundary layer downstream. The paper combines two diagnostics: Laser Doppler Anemometry (LDA) as the reference measurement and a multi-hole probe (MHP) as the practical, cheaper instrument. The target profiles themselves—normalised mean velocity and turbulence intensity curves from international standards and from English Channel and North Sea inflow conditions—serve as the validation yardstick; agreement with them, plus spanwise uniformity and spectra, is what qualifies the spires as sufficient. No floor roughness is used, so the argument rests on the spires doing all the boundary layer generation.
What would settle it
Measure the same spire-generated flow with an independent technique, such as a hot-wire anemometer or a second LDA system, at the same test conditions; if the streamwise mean velocity differs from the MHP by more than 1 percent or any turbulent component's standard deviation differs by more than 5 percent, the validation claim fails.
Extended reading notes
Core claim
The central claim is that Irwin spires alone—triangular spires placed at the tunnel inlet to generate large-scale shear—can produce credible marine ABLs without floor roughness elements. Two target profiles were defined: Profile 1 as a commonality framework across international wind-engineering standards, and Profile 2 as a model of wind farm inflow over the English Channel and North Sea. The study reports that the measured normalised velocity and turbulence intensity match these targets, that MHP streamwise velocity differs from LDA by under 1 percent, and that standard deviations in all three velocity components differ by under 5 percent. Spanwise uniformity and spectral checks across different inflow speeds are used to argue that the simulated ABLs are robust. The conclusion is that this spire-only configuration is a cost-effective and reliable way to simulate marine ABLs for offshore wind applications.
Load-bearing premise
The demonstration depends on the target profiles being accurate stand-ins for real marine atmospheric boundary layers; if those targets misrepresent the true offshore wind environment, a good match to them would not prove the tunnel reproduces the real inflow.
Editorial extensions
If this is right
- A wind tunnel can reproduce marine ABL inflow using spires alone, eliminating the cost and complexity of floor roughness elements.
- The multi-hole probe can replace laser Doppler anemometry for this kind of characterization to within 1 percent in mean streamwise velocity and 5 percent in turbulence standard deviation, shortening measurement campaigns.
- The two profiles give future studies ready-made target curves: one that spans international wind-loading standards and one that represents English Channel and North Sea inflow.
- Because spanwise uniformity and spectra were stable across inflow velocities, the setup can be reused for parametric studies of offshore wind turbine loads.
- The Profile 1 commonality framework gives wind engineering a potential reference for comparing how different national standards specify ABL inflow.
Reading between the lines
- The spire-only configuration should transfer to other smooth-terrain boundary layers, such as coastal or ice-covered offshore sites, so long as the target roughness remains low; this is a natural next test.
- The reported MHP-versus-LDA agreement suggests the probe could be trusted for two-component turbulence statistics, but the claim is stated for standard deviation, not for full spectra or higher moments, which would need separate validation.
- The commonality profile could serve as a benchmark for reconciling national wind-load standards, but the paper only demonstrates the tunnel reproduces one such curve; testing against more standards is needed.
- A direct field comparison, using lidar or mast measurements at an English Channel or North Sea site, would check whether the tunnel targets themselves are faithful to real offshore conditions.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript (presented as an abstract) reports a wind-tunnel study in which two marine atmospheric boundary layer (ABL) profiles are generated using Irwin spires without floor roughness elements. Profile 1 targets a commonality framework across international wind engineering standards, and Profile 2 targets inflow conditions for wind farms in the English Channel and North Sea. The flow is measured with Laser Doppler Anemometry (LDA) and a multi-hole probe (MHP). The authors report that MHP agrees with LDA to within 1% in streamwise velocity and within 5% standard deviation in all three velocity components, that the profiles agree with target normalised velocity and turbulence intensity, and that spanwise uniformity and spectral analysis confirm robustness. The central conclusion is that Irwin spires provide a cost-effective and reliable method for simulating marine ABLs, with relevance to offshore wind energy systems.
Significance. If the claims are substantiated, this work would provide a low-cost experimental method for generating marine ABL inflow conditions, which is valuable for wind tunnel testing of offshore wind turbines and for comparing measurement techniques (MHP vs. LDA). The use of external benchmarks (wind engineering standards, LDA as an independent reference) avoids circularity and is a strength. However, the abstract alone does not provide the quantitative evidence needed to assess whether the simulated flow reliably reproduces a marine ABL, particularly regarding turbulence spectra and length scales.
major comments (3)
- [Abstract] The abstract states that "spectral analysis confirmed the robustness of the simulation," but no quantitative spectral or turbulence length-scale comparison is reported. For a marine ABL relevant to offshore wind turbine loads, the integral length scale and spectral shape (e.g., Kaimal or von Kármán with appropriate parameters) are as important as mean velocity and turbulence intensity. Without showing that the generated turbulence has marine-like spectra and length scales, the claim that Irwin spires alone "reliably" simulate marine ABLs is not fully supported. Please provide quantitative comparisons of the measured spectra and integral length scales against target marine spectra for both profiles.
- [Abstract] The MHP/LDA agreement is reported as "less than 1% deviation in the streamwise velocity" and "under 5% standard deviation in the streamwise, spanwise, and wall-normal velocity components." It is unclear what statistical quantity "deviation" refers to (bias, root-mean-square difference, uncertainty?) and how the standard deviation was computed (over spatial locations? repeated runs?). No measurement uncertainty, sample size, or convergence criterion is given. Without this information, the reader cannot assess the reliability of the 1% and 5% claims. Please specify the definitions, report uncertainties, and state the number of measurement points and samples.
- [Abstract] The profiles "achieved good agreement with target metrics such as normalised velocity and turbulence intensity," but the abstract gives no quantitative measure of agreement, such as maximum deviation, root-mean-square error, or relative error, and does not specify the exact target profiles or their sources for Profile 1 and Profile 2. Since the central conclusion depends on these profile matches, please report quantitative fit metrics and reference the standard or dataset used for each target profile.
minor comments (4)
- [Title/Abstract] The tunnel dimensions "10'x5'" should be written with proper unit notation (e.g., 10 ft × 5 ft) to avoid ambiguity.
- [Abstract] The phrase "MHP showed a reasonably high accuracy" is informal; the quantitative statement that follows is stronger and should replace it or be integrated.
- [Abstract] Please clarify whether the "standard deviation" in the MHP/LDA comparison refers to the standard deviation of the measurement error or to the variability of the flow fluctuations themselves.
- [Abstract] The abstract mentions "varying inflow velocities" but does not state the range of wind speeds tested; please add this information for completeness.
Circularity Check
No circularity: validation is against external standards and LDA reference, not the paper's own outputs.
full rationale
The abstract's derivation chain is self-contained. The target ABL profiles are fixed by external criteria (international wind engineering standards and English Channel/North Sea inflow conditions), and the measured LDA/MHP quantities are compared against those fixed targets. Nothing described as a prediction is constructed from the measured data: the 1% streamwise and 5% standard-deviation MHP-vs-LDA comparison is a metrological cross-check against an independent instrumentation principle, not a fitted parameter renamed as validation. The spire generation of the boundary layer is set by standard Irwin-spire design considerations, and the paper reports agreement with target normalised velocity and turbulence-intensity profiles as an outcome, not as a constraint used to define the target. No self-citation is invoked, and no uniqueness theorem or imported ansatz is used to forbid alternatives. The absence of full text prevents checking spectral or length-scale details, but the reader's concern about missing spectral validation is a completeness or validity issue, not circularity: the claim would be premature if spectra are unmatched, but that would not make the derivation circular. Under hard rule 3, self-contained comparison against external benchmarks merits score 0-2; here the comparison is explicitly external (standards, LDA), so the honest finding is no significant circularity.
Assumptions & free parameters
free parameters (2)
- Irwin spire geometric parameters for Profile 1 =
not reported in abstract
- Irwin spire geometric parameters for Profile 2 =
not reported in abstract
assumptions (3)
- domain assumption The target ABL profiles from international standards and from the English Channel/North Sea are representative of real marine boundary layers.
- domain assumption Laser Doppler Anemometry provides an accurate reference velocity measurement.
- domain assumption The wind tunnel flow is stationary and statistically converged during measurements.
Cite this review
Pith. "Pith review of Set-up and Characterisation of Atmospheric Boundary Layers in the 10'x5' Wind Tunnel." pith.science (2026). https://pith.science/paper/M7J2UVZG
@misc{pith2026260807764,
author = {Pith},
title = {Pith review of: Set-up and Characterisation of Atmospheric Boundary Layers in the 10'x5' Wind Tunnel},
year = {2026},
howpublished = {\url{https://pith.science/paper/M7J2UVZG}},
note = {Machine review of arXiv:2608.07764}
}
read the original abstract
The Atmospheric Boundary Layer (ABL) plays a critical role in influencing objects exposed to atmospheric conditions, making its study crucial. Due to the high cost of real-world testing, this thesis focuses on replicating marine ABLs in a wind tunnel environment. Two profiles were developed: one that served as a framework for establishing commonality among the various international wind engineering standards ('Profile 1'), and a second profile, which is more suitable for modelling the inflow to wind farms in the English Channel and the North Sea ('Profile 2'). The ABLs were generated using Irwin spires without floor roughness elements, and the flow characteristics were measured using Laser Doppler Anemometry (LDA) and a multi-hole probe (MHP). MHP showed a reasonably high accuracy when compared to LDA, with less than 1% deviation in the streamwise velocity and under 5% standard deviation in the streamwise, spanwise, and wall-normal velocity components. The profiles achieved good agreement with target metrics such as normalised velocity and turbulence intensity. Spanwise uniformity and spectral analysis confirmed the robustness of the simulation across varying inflow velocities. Overall, Irwin spires proved to be a cost-effective and reliable method for simulating marine ABLs, offering valuable insights for optimising offshore wind energy systems.
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Works this paper leans on
-
[1]
The atmospheric boundary layer; 2025
Office M. The atmospheric boundary layer; 2025. Accessed 2025-04-10. Available from:https: //www.metoffice.gov.uk/research/foundation/parametrizations/boundary-layer
work page 2025
-
[2]
Eurocode 1: Actions on structures - Parts 1-4: General actions - Wind actions
British-Standard-Institution. Eurocode 1: Actions on structures - Parts 1-4: General actions - Wind actions. Eurocodes. 2005:1-16
work page 2005
-
[3]
NA to BS EN 1991-1-4:2005+A1:2010
British-Standard-Institution. NA to BS EN 1991-1-4:2005+A1:2010. UK National Annex Eurocode I - Actions on structures, Part1-4: General actions - wind actions, British Standards. 2010:1-16
work page 1991
-
[4]
International Standard for Standardization
ISO 19901-1:2015, Petroleum and natural gas industries - Specific requirements for offshore structures - Part 1: Metocean design and operating considerations. International Standard for Standardization. 2015
work page 2015
- [5]
-
[6]
Part II: single pointdataforstrongwinds(neutralatmosphere)
ESDU85020 Characteristics of atmospheric turbulence near the ground. Part II: single pointdataforstrongwinds(neutralatmosphere). EngineeringSciences Data Unit 85020
-
[7]
Australian/ New Zealand Standard, Structural design actions, Part 2: Wind actions. AS/NZS 11702:2021. 2021
work page 2021
-
[8]
The application of the boundary layer wind tunnel to the prediction of wind loading
Davenport AG, Isyumov N. The application of the boundary layer wind tunnel to the prediction of wind loading. In: Proceedings of the International Research Seminar: Wind Effects on Buildings and Structures. Ottawa, Canada. September; 1967. p. 11-5. Available from:https://www.aivc. org/sites/default/files/members_area/medias/pdf/Airbase/airbase_00393.pdf
work page 1967
Show all 63 references
-
[9]
Guidelines for converting between various wind averaging periods in tropical cyclone conditions
Harper B, Kepert J, Ginger J. Guidelines for converting between various wind averaging periods in tropical cyclone conditions. Citeseer; 2010
2010
-
[10]
Wind actions to BS EN 1991-1-4
Hughes A. Wind actions to BS EN 1991-1-4. Steel Construction Institute; 2014
1991
-
[11]
Converging profile relationships for offshore wind speed and turbulence intensity
Jeans G. Converging profile relationships for offshore wind speed and turbulence intensity. Wind Energy Science. 2024;9(10):2001-15
2024
-
[12]
Evaluation of marine wind profiles in the North Sea and Norwegian Sea based on measurements and satellite-derived wind products
Olsen AM, Øiestad M, Berge E, Køltzow MØ, Valkonen T. Evaluation of marine wind profiles in the North Sea and Norwegian Sea based on measurements and satellite-derived wind products. Tellus A: Dynamic Meteorology and Oceanography. 2022;74(1)
2022
-
[13]
A mathematical model of the structure of strong winds
Deaves D. A mathematical model of the structure of strong winds. CIRIA Report 76, Const Ind Research and Inf Assoc. 1978. Available from:https://cir.nii.ac.jp/crid/ 1570009749310590336
1978
-
[14]
ESDU spreadsheet
01008 E. ESDU spreadsheet;. [14/10/2024]]. Available from:https: //imperiallondon-my.sharepoint.com/:x:/g/personal/smn21_ic_ac_uk/ ESDt2bm2ATpGushPp_gkGTQBWmin6ml9TyjNUB4O_EPmCQ?e=UaMCI1
2024
-
[15]
What’s the gust wind speed?; 2013
Ginger JHJ, Harper B. What’s the gust wind speed?; 2013
2013
-
[16]
Simplified elements for wind-tunnel measurements with type-III-terrain atmospheric boundary layer
De Paepe W, Pindado S, Bram S, Contino F. Simplified elements for wind-tunnel measurements with type-III-terrain atmospheric boundary layer. Measurement. 2016;91:590-600. Available from:https://www.sciencedirect. com/science/article/pii/S0263224116302457?casa_token=I5Xsi0xLOOo...
2016
-
[17]
A wind tunnel study of wind loads on a model wind turbine in atmospheric boundary layer winds
Tian W, Ozbay A, Hu H. A wind tunnel study of wind loads on a model wind turbine in atmospheric boundary layer winds. Journal of Fluids and Structures. 2019;85:17-26. Available from:https://www.sciencedirect.com/science/ article/pii/S0889974618301543?casa_token=OdhMqbDAOv0AAAA...
2019
-
[18]
Experiments on integral length scale control in atmospheric boundary layer wind tunnel
Varshney K, Poddar K. Experiments on integral length scale control in atmospheric boundary layer wind tunnel. Theoretical and applied climatology. 2011;106:127-37. Available from:https: //link.springer.com/article/10.1007/s00704-011-0415-y
2011 doi
-
[19]
Wind-tunnel simulation of the wake of a large wind turbine in a stable boundary layer
Hancock PE, Pascheke F. Wind-tunnel simulation of the wake of a large wind turbine in a stable boundary layer. Part 1: the boundary-layer simulation. Boundary-layer meteorology. 2014;151(1):3-21. Available from:https://link.springer.com/article/10. 1007/s10546-013-9886-y
2014
-
[20]
Wind-tunnel simulation of weakly and moderately stable atmospheric boundary layers
Hancock PE, Hayden P. Wind-tunnel simulation of weakly and moderately stable atmospheric boundary layers. Boundary-layer meteorology. 2018;168:29-57. Available from:https://link. springer.com/article/10.1007/s10546-018-0337-7
2018 doi
-
[21]
Wind-tunnel simulation of approximately horizontally homogeneous stable atmospheric boundary layers
Hancock PE, Hayden P. Wind-tunnel simulation of approximately horizontally homogeneous stable atmospheric boundary layers. Boundary-layer meteorology. 2021;180(1):5-26. Available from:https://link.springer.com/article/10.1007/s10546-021-00611-7
2021 doi
-
[24]
Part-depth wind tunnel simulations of the atmospheric boundary layer
De Bortoli M, Natalini B, Paluch M, Natalini M. Part-depth wind tunnel simulations of the atmospheric boundary layer. Journal of Wind Engineering and Industrial Aerodynamics. 2002;90(4-5):281-91. Available from:https://www.sciencedirect.com/science/article/ pii/S01676105010020...
2002
-
[26]
Generating an artificially thickened boundary layer to simulate the neutral atmospheric boundary layer
Hohman TC, Van Buren T, Martinelli L, Smits A. Generating an artificially thickened boundary layer to simulate the neutral atmospheric boundary layer. Journal of Wind Engineering and Industrial Aerodynamics. 2015;145:1-16. Available from:https://www.sciencedirect.com/ science/...
2015
-
[27]
The development and structure of simulated neutrally stable atmospheric boundary layers; 1979
Robins A. The development and structure of simulated neutrally stable atmospheric boundary layers; 1979
1979
-
[28]
The design of spires for wind simulation
Irwin H. The design of spires for wind simulation. Journal of wind engineering and industrial aerodynamics. 1981;7(3):361-6. Available from:https://www.aivc.org/sites/ default/files/members_area/medias/pdf/Airbase/airbase_00778.pdf
1981
-
[30]
Progress Report II on Simulation of Earth’s Surface Winds by Artificially Thickened Wind Tunnel Boundary Layers
Campbell GS, Standen N. Progress Report II on Simulation of Earth’s Surface Winds by Artificially Thickened Wind Tunnel Boundary Layers. National Research Council of Canada, National Aeronautical Establishment; 1969
1969
-
[31]
Time-resolved PIV measurements of a ship airwake in a simulated atmospheric boundary layer
Seth D, Zhang Z, Gnanamanickam EP, Leishman JG. Time-resolved PIV measurements of a ship airwake in a simulated atmospheric boundary layer. In: AIAA Aviation 2020 Forum; 2020. p
2020
-
[32]
Establishing a database for flight in the wakes of structures
Healey JV. Establishing a database for flight in the wakes of structures. Journal of Aircraft. 1992;29(4):559-64. Available from:https://arc.aiaa.org/doi/pdf/10.2514/3.46202? casa_token=Fg40vLkosPEAAAAA:HZzCSgWsEOofsTz6cs6bisWW3yd9AUGnw6fOK7w7JnWMoblzw_ vGoQ0UeB7WYFPe-Tg8WzWwyA
1992 doi
-
[33]
Potential wind: The effect of obstacles on wind measurements needs to be filtered out
KNMI. Potential wind: The effect of obstacles on wind measurements needs to be filtered out
-
[34]
Simula¸ c˜ ao da camada limite atmosf´ erica em t´ unel de vento
Loredo-Souza AM, Schettini EBC, Paluch MJ. Simula¸ c˜ ao da camada limite atmosf´ erica em t´ unel de vento. Turbulˆ encia Rio de Janeiro: Associa¸ c˜ ao Brasileira de Engenharia e Ciˆ encias Mecˆ anicas-ABCM. 2004;4:137-63
2004
-
[35]
Atmospheric boundary layer flows: their structure and measurement
Kaimal JC, Finnigan JJ. Atmospheric boundary layer flows: their structure and measurement. Oxford university press; 1994
1994
-
[37]
Wind tunnel simulation of the atmospheric boundary layer for studying the wind pattern at centro de lan¸ camento de alcˆ antara
Avelar AC, Brasileiro FLC, Marto AG, Marciotto ER, Fisch G, Faria AF. Wind tunnel simulation of the atmospheric boundary layer for studying the wind pattern at centro de lan¸ camento de alcˆ antara. Journal of Aerospace Technology and Management. 2012;4(4):463-73. Available fr...
2012
-
[38]
Numerical modelling of velocity profile parameters of the atmospheric boundary layer simulated in wind tunnels
Abubaker A, Kosti´ c I, Kosti´ c O. Numerical modelling of velocity profile parameters of the atmospheric boundary layer simulated in wind tunnels. In: IOP Conference Series: Materials Science and Engineering. vol. 393. IOP Publishing; 2018. p. 012025. Available from:https: //...
2018 doi
-
[39]
Determining the power-law wind-profile exponent under near-neutral stability conditions at sea
Hsu S, Meindl EA, Gilhousen DB. Determining the power-law wind-profile exponent under near-neutral stability conditions at sea. Journal of Applied Meteorology (1988-2005). 1994:757-65. Available from:https://www.jstor.org/stable/26186719?casa_token=ksl0Gn9F5xMAAAAA% 3AM3XArnP7...
1988
-
[40]
Wind tunnel simulation of atmospheric boundary layer flows
Barbosa P, Cataldi M, Freire APS. Wind tunnel simulation of atmospheric boundary layer flows. Journal of the Brazilian Society of Mechanical Sciences. 2002;24(3):177-85. Available from: https://www.scielo.br/j/jbsms/a/DLMQYyR3wML8pDypZtGRWzR/?lang=en
2002
-
[41]
Simula¸ c˜ ao da estrutura do vento natural em um t´ unel de vento aerodinˆ amico
Blessmann J. Simula¸ c˜ ao da estrutura do vento natural em um t´ unel de vento aerodinˆ amico. S˜ ao Jbs´ e dos Campos. 1973
1973
-
[42]
Truncated vortex generators for part-depth wind-tunnel simulations of the atmospheric boundary layer flow
Kozmar H. Truncated vortex generators for part-depth wind-tunnel simulations of the atmospheric boundary layer flow. Journal of Wind Engineering and Industrial Aerodynamics. 2011;99(2-3):130-6. Available from:https://www.sciencedirect.com/science/article/pii/ S0167610510001194
2011
-
[43]
Scale effects in wind tunnel modeling of an urban atmospheric boundary layer
Kozmar H. Scale effects in wind tunnel modeling of an urban atmospheric boundary layer. Theoretical and Applied Climatology. 2010;100:153-62. Available from:https://link. springer.com/article/10.1007/s00704-009-0156-3
2010 doi
-
[44]
On simulating the lower third of the urban adiabatic boundary layer in a wind tunnel
Cook N. On simulating the lower third of the urban adiabatic boundary layer in a wind tunnel. Atmospheric Environment (1967). 1973;7(7):691-705. Available from:https://www. sciencedirect.com/science/article/abs/pii/0004698173901510
1967
-
[45]
Wind-tunnel simulation of the adiabatic atmospheric boundary layer by roughness, barrier and mixing-device methods
Cook N. Wind-tunnel simulation of the adiabatic atmospheric boundary layer by roughness, barrier and mixing-device methods. Journal of Wind Engineering and Industrial Aerodynamics. 1978;3(2-3):157-76. Available from:https://www.sciencedirect.com/science/article/abs/ pii/016761...
1978
-
[46]
A spire array for generating thick turbulent shear layers for natural wind simulation in wind tunnels; 1972
Standen N. A spire array for generating thick turbulent shear layers for natural wind simulation in wind tunnels; 1972. Available from:https://www.aivc.org/resource/ spire-array-generating-thick-turbulent-shear-layers-natural-wind-simulation-wind-tunnels
1972
-
[47]
Development of an Atmospheric-Boundary-Layer Profile at the NASA Langley Transonic Dynamics Tunnel
Ivanco TG, Keller DF, Pinkerton JL, Disotell KJ, Collins JG, Seliquini SL. Development of an Atmospheric-Boundary-Layer Profile at the NASA Langley Transonic Dynamics Tunnel. In: 2018 AIAA Space and Astronautics Forum and Exposition; 2018. p. 5184. Available from:https: //arc....
2018 doi
-
[48]
An experimental investigation on the wake interference of multiple wind turbines in atmospheric boundary layer winds
Ozbay A, Tian W, Yang Z, Sarkar P, Hu H. An experimental investigation on the wake interference of multiple wind turbines in atmospheric boundary layer winds. In: 30th AIAA Applied Aerodynamics Conference; 2006. p. 2784. Available from:https://arc.aiaa.org/doi/ pdf/10.2514/6.2012-2784
2006 doi
-
[49]
Simulations of the atmospheric boundary layer in a wind tunnel with short test section
Pires LBM, Paula IBd, Fisch G, Gielow R, Girardi RdM. Simulations of the atmospheric boundary layer in a wind tunnel with short test section. Journal of Aerospace Technology and Management. 2013;5(3):305-14. Available from:https://www.scielo.br/j/jatm/a/ TbtV5fd6z7KCNPq3Nw7z9h...
2013
-
[50]
Atmospheric boundary layer simulation in a short wind tunnel
Shojaee S, Uzol O, Kur¸ c ¨O. Atmospheric boundary layer simulation in a short wind tunnel. International Journal of Environmental Science and Technology. 2014;11:59-68. Available from: https://link.springer.com/article/10.1007/s13762-013-0371-4
2014 doi
-
[51]
Progress in the Statistical Theory of Turbulence*
von K´ arm´ an T. Progress in the Statistical Theory of Turbulence*. Proceedings of the National Academy of Sciences. 1948;34(11):530-9. Available from:https://www.pnas.org/doi/abs/10. 1073/pnas.34.11.530
1948
-
[52]
The local structure of turbulence in incompressible viscous fluid for very large Reynolds numbers
Kolmogorov AN. The local structure of turbulence in incompressible viscous fluid for very large Reynolds numbers. Proceedings of the Royal Society of London Series A: Mathematical and Physical Sciences. 1991;434(1890):9-13. Available from:https://royalsocietypublishing. org/do...
1991
-
[53]
Experiments on the wind tunnel simulation of atmospheric boundary layers
Farell C, Iyengar AK. Experiments on the wind tunnel simulation of atmospheric boundary layers. Journal of wind engineering and industrial aerodynamics. 1999;79(1-2):11-35. Available from:https://www.sciencedirect.com/science/article/pii/S0167610598001172
1999
-
[54]
Experimental investigation of the influence of Reynolds number and buoyancy on the flow development of a plane jet in the transitional regime
Suresh P, Sundararajan T, Srinivasan K, Das SK. Experimental investigation of the influence of Reynolds number and buoyancy on the flow development of a plane jet in the transitional regime. Journal of Turbulence. 2021;22(1):26-47
2021
-
[55]
Autocorrelation functions and the determination of integral length with reference to experimental and numerical data
O’Neill PL, Nicolaides D, Honnery D, Soria J, et al. Autocorrelation functions and the determination of integral length with reference to experimental and numerical data. In: 15th Australasian fluid mechanics conference. vol. 1. University of Sydney, Sydney, NSW, Australia
-
[56]
Turbulent flows
Pope SB. Turbulent flows. Measurement Science and Technology. 2001;12(11):2020-1
2001
-
[57]
Comparison of turbulence integral length scale determination methods
TRUSH 1 A, POSP ´IˇSIL1 S, Kozmar H. Comparison of turbulence integral length scale determination methods. Advances in Fluid Mechanics XIII. 2020;128:113
2020
-
[58]
Physical fluid dynamics
Tritton DJ. Physical fluid dynamics. Springer Science & Business Media; 2012
2012
-
[59]
Wind-tunnel simulations of the suburban ABL and comparison with international standards
Kozmar H. Wind-tunnel simulations of the suburban ABL and comparison with international standards. Wind and Structures, An International Journal. 2011;14(1):15-34
2011
-
[60]
Wind structure in the atmospheric boundary layer
Pasquill F. Wind structure in the atmospheric boundary layer. Philosophical Transactions of the Royal Society of London Series A, Mathematical and Physical Sciences. 1971;269(1199):439-56. Available from:https://royalsocietypublishing.org/doi/abs/10.1098/rsta.1971.0043
1971
-
[61]
Probing PIV: multi-hole pressure and PIV measurements upstream and downstream of an instrumented model turbine
Craig Thompson MG Kevin Gouder. Probing PIV: multi-hole pressure and PIV measurements upstream and downstream of an instrumented model turbine. Wind Energy Science Conference, France. June 2025
2025
-
[62]
Laser Doppler anemometry measurements of steady flow through two bi-leaflet prosthetic heart valves
Bazan O, Ortiz JP, Vieira Junior FU, Vieira R W, Antunes N, Tabacow FBD, et al. Laser Doppler anemometry measurements of steady flow through two bi-leaflet prosthetic heart valves. Brazilian Journal of Cardiovascular Surgery. 2013;28:462-9
2013
-
[63]
Cross Line Red Laser; 2025
DEW ALT. Cross Line Red Laser; 2025. Accessed 2025-05-25. Available from:https://www. dewalt.co.uk/product/dw088k-xj/cross-line-red-laser
2025
-
[64]
Quality Assurance Manual: Wind Engineering Studies of Buildings
A WES Q. Quality Assurance Manual: Wind Engineering Studies of Buildings. Australasian Wind Engineering Society. 2019. Appendix A Simulation of the Urban Profile A.1 Profiles from the Standards Figure 61.NormalisedUprofile for the urban standards, wrt 95 m Figure 62.Turbulence...
2019
-
[67]
MHP and static holder Figure 73.CAD of the holder for MHP and static
-
[68]
Aluminium truss structure Figure 74.CAD of the Aluminium truss structure for the traverse v D Wind Tunnel Set-up D.1 Green mesh roughness - Lower TS Figure 75.Green mesh roughness with 2 spire ‘set 1’ - lower TS D.2 2, 3 spires - Lower TS Figure 76.2 spires installed in the lo...
-
[2025]
Available from:https://www.knmi.nl/kennis-en-datacentrum/ project/potential-wind
Accessed 2025-05-20. Available from:https://www.knmi.nl/kennis-en-datacentrum/ project/potential-wind
2025
-
[2701]
Available from:https://arc.aiaa.org/doi/abs/10.2514/6.2020-2701
2020 doi
Reviewed August 11, 2026 · model on record in the stance chip above.
Discussion (0). Continue with ORCID to comment.