Using Spaceborne Synthetic Aperture Radar to Improve Marine Surface Analyses

Abstract The ever-changing weather and lack of in situ data in the Bering Sea warrants experimentation with new meteorological observing systems for this region. Spaceborne synthetic aperture radar (SAR) is well suited for observing the sea surface footprints of marine meteorological phenomena because its radiation is sensitive to centimeter-scale sea surface roughness, regardless of the time of day or cloud conditions. The near-surface wind field generates this sea surface roughness. Therefore, the sea surface footprints of meteorological phenomena are often revealed by SAR imagery when the main modulator of sea surface roughness is the wind. These attributes, in addition to the relatively high resolution of SAR products, make this instrument an excellent candidate for filling the meteorological observing needs over the Bering Sea. This study demonstrates the potential usefulness of SAR for observing Bering Sea meteorology by focusing on its ability to image the sea surface footprints of polar mesoscale ...

[1]  I. Orlanski A rational subdivision of scales for atmospheric processes , 1975 .

[2]  John P. Monteverdi The Single Air Mass Disturbance and Precipitation Characteristics at San Francisco , 1976 .

[3]  P. Hobbs,et al.  Mesoscale Structures of Vortices in Polar Air Streams , 1982 .

[4]  S. Businger The synoptic climatology of polar low outbreaks , 1985 .

[5]  K. Davidson,et al.  Polar and Arctic Lows , 1989 .

[6]  N. Bond,et al.  Polar lows over the Gulf of Alaska in conditions of reverse shear , 1991 .

[7]  George S. Young,et al.  Use of Spaceborne Synthetic Aperture Radar Imagery of the Sea Surface in Detecting the Presence and Structure of the Convective Marine Atmospheric Boundary Layer , 1995 .

[8]  Michael W. Douglas,et al.  Research Aircraft Observations of a Polar Low at the East Greenland Ice Edge , 1995 .

[9]  R. J. Reed,et al.  Origin and structure of a numerically simulated polar low over Hudson Bay , 1995 .

[10]  N. G. Kvamstø,et al.  Numerical simulations of the synoptic conditions and development of Arctic outbreak polar lows , 1995 .

[11]  J. Mailhot,et al.  A numerical case study of a polar low in the Labrador Sea , 1996 .

[12]  G. Heinemann,et al.  Report of a Workshop on Theoretical and Observational Studies of Polar Lows'' of the European Geophysical Society Polar Lows Working Group , 1997 .

[13]  D. Bromwich,et al.  Mesoscale cyclone activity over Antarctica during 1991: 1. Marie Byrd Land , 1997 .

[14]  A. Carleton,et al.  Synoptic climatology, and intrahemispheric associations, of cold air mesocyclones in the Australasian sector , 1997 .

[15]  Todd D. Sikora,et al.  Synthetic Aperture Radar as a Tool for Investigating Polar Mesoscale Cyclones , 2000 .

[16]  Frank Monaldo The Alaska SAR demonstration and near-real-time synthetic aperture radar winds , 2000 .

[17]  Pablo Clemente-Colón,et al.  NOAA CoastWatch SAR Applications and Demonstration , 2000 .