Synergetic Use of Radar and Optical Satellite Images to Support Severe Storm Prediction for Offshore Wind Farming

In this paper, we show how satellite images taken by space-borne radar sensors can be used to determine mesoscale high-resolution wind fields in synergy with cloud parameters from optical data and, thus, help in the task of maintenance and planning offshore wind farms. The aim of this paper is to use synthetic aperture radar (SAR) and medium resolution imaging spectrometer (MERIS) onboard the environmental satellite (ENVISAT) in synergy to analyze severe weather systems, in particular, to describe the spatial evolution of the atmospheric boundary layer processes involved in cold air outbreaks. We investigated the fine-scale structure of a severe weather case on November 1, 2006 over the North Sea using satellite data. The satellite data are compared with numerical model results of the German Weather Service ldquoLokal Modellrdquo (LM) and the high-resolution limited area model (HIRLAM). LM and HIRLAM show differences in mesoscale turbulent behavior and coastal shadowing. Maximum wind speeds of up to 25 m/s are measured by SAR and are confirmed by the models. Significant differences are observed in the location of the maxima. High-resolution ENVISAT ASAR measurements provide very detailed information on small-scale atmospheric features, which seem to not be captured well by the analyzed numerical models, in particular, in coastal areas. Meteosat second generation (MSG) is used to determine the movement of cloud patterns. Cloud patterns seen in the optical data and radar cross-section modulation give a consistent dynamical picture of the atmospheric processes. The relevance for offshore wind farming is discussed.

[1]  John S. Kain,et al.  Convective parameterization for mesoscale models : The Kain-Fritsch Scheme , 1993 .

[2]  Roger M. Wakimoto,et al.  Convectively Driven High Wind Events , 2001 .

[3]  G. Mellor,et al.  A Hierarchy of Turbulence Closure Models for Planetary Boundary Layers. , 1974 .

[4]  M. Tiedtke A Comprehensive Mass Flux Scheme for Cumulus Parameterization in Large-Scale Models , 1989 .

[5]  Ad Stoffelen,et al.  The Improved C-Band Geophysical Model Function CMOD5 , 2005 .

[6]  David Atlas,et al.  Footprints of storms on the sea: A view from spaceborne synthetic aperture radar , 1994 .

[7]  R. Barthelmie,et al.  Observations and simulations of diurnal cycles of near-surface wind speeds over land and sea , 1996 .

[8]  R. Barthelmie,et al.  Statistical analysis of flow characteristics in the coastal zone , 2002 .

[9]  Johannes Schulz-Stellenfleth,et al.  ON THE DIVERGENCE AND VORTICITY OF SAR DERIVED WIND FIELDS , 2007 .

[10]  S. Lehner,et al.  Mesoscale wind measurements using recalibrated ERS SAR images , 1998 .

[11]  Marina I. Mityagina,et al.  Detection of convective instability in atmospheric boundary layer over the ocean by airborne Ku-band real aperture radar , 1996, IGARSS '96. 1996 International Geoscience and Remote Sensing Symposium.

[12]  Thomas Nauss,et al.  Discriminating raining from non-raining clouds at mid-latitudes using multispectral satellite data , 2006 .

[13]  L. R. Koenig,et al.  A Short Course in Cloud Physics , 1979 .

[14]  Rebecca J. Barthelmie,et al.  Comparison of potential power production at on‐ and offshore sites , 2001 .

[15]  J. Fischer,et al.  Cloud top pressure retrieval from measurements within the O/sub 2/-A band with the satellite imaging sensor MERIS , 1999, IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293).

[16]  Tammy M. Weckwerth,et al.  Horizontal Convective Rolls: Determining the Environmental Conditions Supporting their Existence and Characteristics , 1997 .

[17]  Jochen Horstmann,et al.  Global wind speed retrieval from SAR , 2003, IEEE Trans. Geosci. Remote. Sens..

[18]  Jochen Horstmann,et al.  Comparison of offshore wind park sites using SAR wind measurement techniques , 2005 .

[19]  Joseph B. Klemp,et al.  Characteristics of Isolated Convective Storms , 1986 .