Annals of Glaciology · 1997 · 69 citations · 4 references
Natural SciencesEarth SciencesOceanographyCryosphere StudiesGlaciologyRemote SensingCryospheric Remote SensingIce DynamicsRemote Sensing Of IceSea Ice DriftSea Ice Remote SensingSea Ice StudiesArctic Sea Ice DriftDisplacementIce Pack DriftSatellite Remote Sensing Of Ice MotionSea Ice Drift VelocitySea Ice Motion EstimationSea Ice Motion RetrievalSea Ice Velocity
This paper describes the application of an automated cross-correlation technique to pairs of 85.5 GHz Special Sensor Microwave Imager (SSM/I) images to obtain Ice motion over the entire Arctic Basin for a contiguous two month period between December 1993 and January 1994. Although the surface ice information in the imagery is coarse and noisy, the area cross-correlation method is quite successful in picking up ice-motion information. The accuracy of 85.5 GHz SSM/I derived ice motions is evaluated by comparing results with Arctic buoy drift. Over 390 comparisons with buoy-drift estimates of ice displacement were made with an overall correlation of 0.75 and an average vector magnitude error in ice velocity of 3.5 km d −1 . The main difficulty with the automated technique is the tendency to overestimate ice displacement compared to buoy data by about 14%. Two detailed examples of ice motion are presented. The first occurred in December 1993, when a major westward shift in the ice pack took place in the Canada Basin and opened up a very large lead off Banks and Prince Patrick Islands. The second example occurred in January 1994, when an intense anticyclone over the Canada Basin produced a strong Beaufort Gyre.
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