Skip to main content

The Relevance of Surface Roughness Data Qualities in Diagnostic Modeling of Wind Velocity in Complex Terrain: A Case Study from the Śnieżnik Massif (SW Poland)

  • Chapter
  • First Online:
Geoinformatics and Atmospheric Science

Part of the book series: Pageoph Topical Volumes ((PTV))

  • 938 Accesses

Abstract

Numerical modeling of wind velocity above complex terrain has become a subject of numerous contemporary studies. Regardless of the methodical approach (dynamic or diagnostic), it can be observed that information about surface roughness is indispensable to achieve realistic results. In this context, the current state of GIS and remote sensing development allows access to a number of datasets providing information about various properties of land coverage in a broad spectrum of spatial resolution. Hence, the quality of roughness information may vary depending on the properties of primary land coverage data. As a consequence, the results of the wind velocity modeling are affected by the accuracy and spatial resolution of roughness data. This paper describes further attempts to model wind velocity using the following sources of roughness information: LiDAR data (Digital Surface Model and Digital Terrain Model), database of topographical objects (BDOT10k) and both raster and vector versions of Corine Land Cover 2006 (CLC). The modeling was conducted in WindStation 4.0.2 software which is based on the computational fluid dynamics (CFD) diagnostic solver Canyon. Presented experiment concerns three episodes of relatively strong and constant synoptic forcing: 26 November 2011, 25 May 2012 and 26 May 2012. The modeling was performed in the spatial resolution of 50 and 100 m. Input anemological data were collected during field measurements while the atmosphere boundary layer parameters were derived from the meteorological stations closest to the study area. The model’s performance was verified using leave-one-out cross-validation and calculation of error indices such as bias error, root mean square error and index of wind speed. Thus, it was possible to compare results of using roughness datasets of different type and resolution. The study demonstrates that the use of LiDAR-based roughness data may result in an improvement of the model’s performance in 100 and 50 m resolution, comparing to CLC and BDOT10k. Furthermore, a slight improvement of these results can be accomplished if the LiDAR-based roughness calculation process includes the variable of prevailing wind direction. Qualities of both CLC and BDOT10k raw datasets (imposed land coverage classes, necessity of the roughness classes assignment) induce relatively high values of the modeled velocity error indices. Hence, these and other similar datasets need to be carefully analyzed (e.g. compared with aerial or satellite imagery) before they are used in the process of roughness length parameterization.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 79.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 99.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Abbes, M., Belhadj, J. (2012), Wind resource estimation and wind park design in El-Kef region, Tunisia, Energy 40, 348–357.

    Google Scholar 

  • Cho, J., Miyazaki, S., Yeh, P.J.-F., Kim, W., Kanae, S., Oki T. (2012), Testing the hypothesis on the relationship between aerodynamic roughness length and albedo using vegetation structure parameters, International Journal of Biometeorology 56, 411–418.

    Google Scholar 

  • Colin, J., Faivre, R. (2010), Aerodynamic roughness length estimation from very high-resolution imaging LIDAR observations over the Heihe basin in China, Hydrology and Earth System Sciences 14, 2661–2669.

    Google Scholar 

  • Corine Land Cover 2006 raster dataset (version 15) (2011); http://www.eea.europa.eu/data-and-maps/data/corine-land-cover-2006-raster-1. Accessed date 13 Mar 2012.

  • Corine Land Cover 2006 vector dataset (version 17) (2013); http://www.eea.europa.eu/data-and-maps/data/clc-2006-vector-data-version-3. Access date 20 Mar 2014.

  • Database of Topographical Objects (BDOT10k)—vector database; http://www.codgik.gov.pl/index.php/zasob/baza-danych-obiektow-topograficznych.html. Accessed date 30 May 2015.

  • Davenport, A.G. (1960), Rationale for determining design wind velocities, Journal of Structural Division 86, 39–68.

    Google Scholar 

  • De Meij, A., Vinuesa, J.F. (2014), Impact of SRTM and Corine Land Cover data on meteorological parameters using WRF, Atmospheric Research 143, 351–370.

    Google Scholar 

  • Dong, Z., Gao, S., Fryrear, D.W. (2001), Drag coefficients, roughness length and zero-plane displacement height as disturbed by artificial standing vegetation, Journal of Arid Environments 49, 485–505.

    Google Scholar 

  • Emeis, S., Knoche, H.R., Applications in meteorology. In Geomorphometry: concepts, software, applications. (eds. Hengl T., Reuter H. I.) (Elsevier 2007) pp. 603–623.

    Google Scholar 

  • Emery, C., Tai, E., Yarwood, G., Enhanced meteorological modeling and performance evaluation for two Texas ozone episodes. (ENVIRON International Corporation, 2001).

    Google Scholar 

  • Garratt, J.R., The atmospheric boundary layer (Cambridge, New York, 1994).

    Google Scholar 

  • Grimmond, C.S.B., Oke, T.R. (1999), Aerodynamic properties of urban areas derived from analysis of surface form. Journal of Applied Meteorology 38, 1262–1292.

    Google Scholar 

  • Hammond, D.S., Chapman, L., Thornes, J.E. (2012), Roughness length estimation along road transects using airborne LIDAR data, Meteorological Applications 19, 420–426.

    Google Scholar 

  • Hansen, F.V., Surface roughness lengths (Army Research Laboratory, 1993).

    Google Scholar 

  • Hasager, C.B., Nielsen, N.N., Jensen, N.O., Boegh, E., Christensen, J.H., Dellwik, E., Soegaard, H. (2003), Effective roughness calculated from satellite-derived land cover maps and hedge-information used in a weather forecasting model, Boundary-Layer Meteorology 109, 227–254.

    Google Scholar 

  • Heisler, G.M., De Walle, D.R. (1988), Effects of windbreak structure on airflow, Agriculture, Ecosystems & Environment 22/23, 41–69.

    Google Scholar 

  • Jackson, P.S. (1981), On the Displacement Height in the Logarithmic Velocity Profile, Journal of Fluid Mechanics 111, 15–25.

    Google Scholar 

  • Jacobson, M.Z., Fundamentals of atmospheric modeling (University Press, Cambridge 2005).

    Google Scholar 

  • Jancewicz, K. (2014), Remote sensing data in wind velocity field modeling: a case study from the Sudetes (SW Poland), Pure and Applied Geophysics 171, 941–964.

    Google Scholar 

  • Jasinski, M.F., Crago, R.D. (1999), Estimation of vegetation aerodynamic roughness of natural regions using frontal area density determined from satellite imagery, Agricultural and Forest Meteorology 94, 65–77.

    Google Scholar 

  • Jimenez, P.A., Dudhia, J. (2012), Improving the representation of resolved and unresolved topographic effects on surface wind in the WRF model, Journal of Applied Meteorology and Climatology, 51(2), 300–316.

    Google Scholar 

  • Lopes, A.M.G. (2003), WindStation—a software for the simulation of atmospheric flows over complex topography, Environmental Modeling & Software 18, 81–96.

    Google Scholar 

  • Lopes, A.M.G. (2013), WindStation 3.1.0: User’s Manual.

    Google Scholar 

  • Morales, L., Lang, F., Mattar, C. (2012), Mesoscale wind speed simulation using CALMET model and reanalysis information: An application to wind potential, Renewable Energy 48, 57–71.

    Google Scholar 

  • Piasecki, J., Wybrane cechy klimatu Masywu Śnieżnika, In Masyw Śnieżnika. Zmiany w środowisku przyrodniczym (eds. Jahn A., Kozłowski S., Pulina M.) (PAE, Warszawa 1996) pp. 189–206.

    Google Scholar 

  • Piasecki, J., Sawiński, T., The Niedźwiedzia Cave in the climatic environment of the Kleśnica Valley (Śnieżnik Massif), In Karst of the Częstochowa Upland and of the Eastern Sudetes: palaeoenviroments and protection (eds. Stefaniak K., Tyc A., Socha P.) (University of Silesia, Sosnowiec – Wrocław 2009) pp. 423–454.

    Google Scholar 

  • Plate, E.J., Engineering meteorology (Elsevier, New York, 1982).

    Google Scholar 

  • Ramli, N.I., Idris Ali, M., Saad, M.S.H., Majid, T.A (2009), Estimation of the roughness length (zo) in malaysia using satellite image, Conference Proceedings of The Seventh Asia-Pacific Conference on Wind Engineering, http://www.iawe.org/Proceedings/7APCWE/T2D_1.pdf.

  • Schaudt, K.J., Dickinson, R.E. (2000), An approach to deriving roughness length and zero-plane displacement height from satellite data, prototyped with BOREAS data, Agricultural and Forest Meteorology 104, 143–155.

    Google Scholar 

  • Silva, J., Ribeiro, C., Guedes, C. (2007), Roughness length classification of Corine Land Cover Classes, Conference Proceedings of European Wind Energy Conference 2007, http://www.ewea.org/ewec2007/allfiles2/545_Ewec2007fullpaper.pdf.

  • Suder, A., Szymanowski, M. (2014), Determination of ventilation channels in urban area: a case study of Wrocław (Poland), Pure and Applied Geophysics 171, 965–975.

    Google Scholar 

  • Taylor, P.A. (1987), Comments and further analysis of effective roughness lengths for use in numerical three-dimensional models, Boundary-Layer Meteorology 39, 403–418.

    Google Scholar 

  • Thom, A.S. (1971), Momentum absorption by vegetation, Quarterly Journal of Royal Meteorological Society 97, 414–428.

    Google Scholar 

  • Tian, X., Li, Z.Y, van der Tol, C., Su, Z., Li, X., He, Q.S., Bao, Y.F., Chen, E.X., Li, L.H. (2011), Estimating zero-plane displacement height and aerodynamic roughness length using synthesis of LiDAR and SPOT-5 data, Remote Sensing of Environment 115, 2330–2341.

    Google Scholar 

  • Truhetz, H., High resolution wind field modeling over complex topography: analysis and future scenarios. (Wegener Center for Climate and Global Change, Scientific Report No. 32-2010, Graz 2010).

    Google Scholar 

  • Wieringa, J. (1993), Representative roughness parameters for homogenous terrain, Boundary-Layer Meteorology 63, 323–363.

    Google Scholar 

  • Wieringa, J., Davenport, A.G., Grimmond, C.S.B., Oke, T.R. (2001) New revision of Davenport roughness classification. Proceedings of the 3rd European & African Conference on Wind Engineering.

    Google Scholar 

  • Wood, N., Brown, A.R., Hewer, F.E., (2001), Parametrizing the effects of orography on the boundary layer: An alternative to effective roughness lengths, Q. J. R. Meteorol. Soc., 127(573), 759–777.

    Google Scholar 

  • World Meteorological Organization, Guide to meteorological instruments and methods of observation, Tech. Rep. 8 (Seventh Edition). (Secretariat of World Meteorological Organization, Geneva 2008).

    Google Scholar 

  • Yamazawa, H., Kondo J. (1989), Empirical-statistical method to estimate the surface wind speed over complex terrain, Journal of Applied Meteorology and Climatology 28, 996–1001.

    Google Scholar 

Download references

Acknowledgments

The authors are grateful to: Romuald Jancewicz, Marzena Józefczyk, Aleksandra Karbowniczak, Maurycy Urbanowicz and Remigiusz Żukowski for their support during field measurements of wind velocity, Tymoteusz Sawiński for technical support and Piotr Migoń for proofreading. Kaindl Windmaster 2 anemometers were used by kind permission of the Department of Climatology and Atmosphere Protection, University of Wrocław. WindStation 4.0.2 software was developed and provided by António Manuel Gameiro Lopes (Department of Mechanical Engineering, University of Coimbra). LiDAR and BDOT10k data were provided by the Head Office of Geodesy and Cartography under the license no. DIO.DFT.DSI.7211.1619.2015_PL_N. Corine Land Cover 2006 raster and vector datasets were provided by European Environmental Agency. Meteorological data used in presented study were provided by Department of Atmospheric Science at the University of Wyoming, National Oceanic and Atmospheric Administration, The Austrian Central Institute for Meteorology and Geodynamics (ZAMG), German Weather Service and The Institute for Meteorology at the Free University of Berlin. Finally, the author greatly appreciate reviewers for their valuable comments and constructive suggestions to improve the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Kacper Jancewicz .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2018 Springer International Publishing AG

About this chapter

Cite this chapter

Jancewicz, K., Szymanowski, M. (2018). The Relevance of Surface Roughness Data Qualities in Diagnostic Modeling of Wind Velocity in Complex Terrain: A Case Study from the Śnieżnik Massif (SW Poland). In: Niedzielski, T., Migała, K. (eds) Geoinformatics and Atmospheric Science. Pageoph Topical Volumes. Birkhäuser, Cham. https://doi.org/10.1007/978-3-319-66092-9_7

Download citation

Publish with us

Policies and ethics