B. Anselme, SEA-ICE FIELDS AND ATMOSPHERIC PHENOMENA IN EURASIATIC ARCTIC SEAS ASSEEN FROM THE NOAA-12 SATELLITE, International journal of remote sensing, 19(2), 1998, pp. 307-316
The image presented in this study is a mosaic showing the Barents and
Kara seas area. It was processed from 1.1 km resolution NOAA-12 AVHRR
data, acquired in the near-infrared band, on 17 June, 1994, 8h30 GMT a
nd 19 June, 1994, 8h10 GMT. With the exception of the western and sout
hern part of the Barents sea, all the area is cloud-free. Such an even
t is relatively seldom and enables us to observe diverse surface ocean
ic features, such as the sea ice distribution, the location of polynya
s and the influence of warm waters, remnants of the North Atlantic Dri
ft, on the ice held. The two days lag between the scenes allows us to
observe the drifting of ice hoes, influenced by winds and currents, es
pecially in the southern part of Franz Josef Land archipelago. Atmosph
eric lee-waves are observed at Hopen Island and westward of Bear Islan
d.