Tropical Cyclone Intensity Estimated From Wide-Swath SAR Images

Due to the relatively small amount of in situ data available for the open oceans, remote sensing techniques take an important role in the retrieval of geophysical information, particularly during extreme events. The work presented here aims at the improvement of prediction of cyclone intensity using synthetic aperture radar (SAR) images. A new method to measure the hurricane intensity using SAR images, in combination with a parametric Holland-type model of wind speed, is presented. The algorithm is based on a least square minimization of the difference between the parametric model results and the SAR measurement. The radius of the maximum wind speed, required as input for the minimization procedure, is estimated from the SAR image using wavelet analysis. Information on wind direction is extracted from the SAR image through analysis of image features caused by boundary layer rolls. The root-mean-square error of the suggested method has been validated to be equal to 3.9 m/s. The study is based on a data set of wide-swath SAR images of about 400 km × 400 km coverage, acquired by the European Envisat satellite, over tropical cyclones. As a case study, hurricane Katrina is investigated in detail. A total of five tropical cyclone images will be used to validate the results of the new algorithm.

[1]  H. Graber,et al.  Can synthetic aperture radars be used to estimate hurricane force winds? , 2005 .

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

[3]  James F. W. Purdom,et al.  Satellite Analysis of Tropical Cyclones Using the Advanced Microwave Sounding Unit (AMSU). , 2000 .

[4]  Maurizio Migliaccio,et al.  On the Inversion of Wind Scatterometer Data , 2001 .

[5]  R. Raney,et al.  Theory of synthetic aperture radar ocean imaging: A MARSEN view , 1985 .

[6]  M. Powell,et al.  Reduced drag coefficient for high wind speeds in tropical cyclones , 2003, Nature.

[7]  W. Alpers,et al.  Atmospheric boundary layer rolls observed by the synthetic aperture radar aboard the ERS-1 satellite , 1994 .

[8]  Paris W. Vachon,et al.  Characterization of hurricane eyes in RADARSAT-1 images with wavelet analysis , 2003 .

[9]  H. Hersbach,et al.  An improved C-band scatterometer ocean geophysical model function: CMOD5 , 2007 .

[10]  Ralph C. Foster,et al.  Why Rolls are Prevalent in the Hurricane Boundary Layer , 2005 .

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

[12]  W. Timothy Liu,et al.  QuikSCAT geophysical model function for tropical cyclones and application to Hurricane Floyd , 2001, IEEE Trans. Geosci. Remote. Sens..

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

[14]  G. Holland An Analytic Model of the Wind and Pressure Profiles in Hurricanes , 1980 .

[15]  Richard K. Moore,et al.  Radar remote sensing and surface scattering and emission theory , 1986 .

[16]  Ralph C. Foster,et al.  Boundary-Layer Similarity Under an Axisymmetric, Gradient Wind Vortex , 2009 .

[17]  Xiaofeng Li,et al.  ENVISAT ASAR APPLICATIONS DEMONSTRATIONS: ALASKA SAR DEMONSTRATION AND GULF OF MEXICO HURRICANE STUDI ES , 2007 .

[18]  Timothy L. Olander,et al.  The Advanced Dvorak Technique: Continued Development of an Objective Scheme to Estimate Tropical Cyclone Intensity Using Geostationary Infrared Satellite Imagery , 2007 .