1 00:00:00,020 --> 00:00:04,180 Interviewer: Ok, John, could you give us a sense of how 2 00:00:04,200 --> 00:00:08,370 this mission was designed, your weather thoughts coming into it, and the 3 00:00:08,390 --> 00:00:12,560 scenery coming in over the calving front. That sort of thing. 4 00:00:12,580 --> 00:00:16,750 Sonntag: Ok, sounds good. My name is John Sonntag, 5 00:00:16,770 --> 00:00:20,930 I'm a senior scientist with the ATM Team – that’s Airborne Topographic Mapper. 6 00:00:20,950 --> 00:00:25,110 Today’s mission was called the 7 00:00:25,130 --> 00:00:29,290 Recovery Offshore 01 mission, made up of six parallel lines spaced at 20 kilometers. 8 00:00:29,310 --> 00:00:33,480 It’s called that because we concentrate on the area where the Recovery glacier, 9 00:00:33,500 --> 00:00:37,660 which is a major glacier in this part of east Antarctica, drains into the Filchner Ice Shelf. 10 00:00:37,680 --> 00:00:41,860 It tends to be difficult to get measurements to help us understand the shape 11 00:00:41,880 --> 00:00:46,060 of the cavity of water, ocean water beneath an ice shelf 12 00:00:46,080 --> 00:00:50,230 such as the Filchner, especially a big one like the Filchner. 13 00:00:50,250 --> 00:00:54,380 With our gravity instruments and our radar instruments on board the DC-8 14 00:00:54,400 --> 00:00:58,520 we are able to collect measurements which allow analysts and scientists to deduce the 15 00:00:58,540 --> 00:01:02,640 shape of those underwater cavities. And that’s important because it 16 00:01:02,660 --> 00:01:06,740 by knowing the shape of those cavities, scientists can begin to get at 17 00:01:06,760 --> 00:01:10,800 the interaction of these glaciers with warm ocean waters. 18 00:01:10,820 --> 00:01:14,830 Which, it has been determined within the last decade or two by the glaciological community 19 00:01:14,850 --> 00:01:19,020 that the interaction of these large glaciers and warming ocean waters 20 00:01:19,040 --> 00:01:23,200 tend to be quite important in determining their future behavior. 21 00:01:23,220 --> 00:01:27,370 The weather today was probably not what you would call ideal; 22 00:01:27,390 --> 00:01:31,500 we knew that there would be a cloud layer at about between eight and ten thousand feet, 23 00:01:31,520 --> 00:01:35,700 And we had a lot of confidence in this particular forecast 24 00:01:35,720 --> 00:01:39,900 So our transit in this morning took us in over the southern part of the Antarctic Peninsula 25 00:01:39,920 --> 00:01:44,080 and over the extreme southern part of the Weddell, just in front of the Ronne Ice Shelf. 26 00:01:44,100 --> 00:01:48,260 And sure enough, most of it was clouded as the models predicted it would be. 27 00:01:48,280 --> 00:01:52,450 We could see bits of sea-ice surface here and there, 28 00:01:52,470 --> 00:01:56,630 But when we made our descent into the Filchner Ice Shelf area, we could see the edge 29 00:01:56,650 --> 00:02:00,790 of the ice shelf and the edge of Berkner Island. It was clear skies there, 30 00:02:00,810 --> 00:02:04,960 and when we got on site, we were very pleased 31 00:02:04,980 --> 00:02:09,120 to see that the forecast indeed held up.