登入選單
返回Google圖書搜尋
A Satellite Imagery Study of Eastern Parry Channel
註釋NOAA and Landsat satellite imagery have been used to study the patterns of ice movement in the eastern half of Parry Channel, extending from Lascaster Sound to the western end of Barrow Strait. Relatively little year-to-year variation (one or two weeks) was noted in the timings of major steps in the break-up of the winter ice, provided that similar positions obtained for the stable cross-channel edge of winter landfast ice. Some correlations were noted between the positioning of this edge and the average winter ice velocities of the mobile ice in the eeastern portion of the Channel.