91![rafted debris in the shallower core is evident from the radiographs. Because the supply of ice-rafted debris to the seabed should be independent of bottom topography, the variation in abundance of ice-rafted debris betwe rafted debris in the shallower core is evident from the radiographs. Because the supply of ice-rafted debris to the seabed should be independent of bottom topography, the variation in abundance of ice-rafted debris betwe](https://www.pdfsearch.io/img/c259a3f9a91efd7d8dbf72bcfa2ed9f6.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 05:02:23
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92![Underlying the surface water all locations was the Weddell winter water. This layer reflected cooling and freezing which occurred during the preceding winter and had temperatures between about -1.5° and -1.7°C and a sa Underlying the surface water all locations was the Weddell winter water. This layer reflected cooling and freezing which occurred during the preceding winter and had temperatures between about -1.5° and -1.7°C and a sa](https://www.pdfsearch.io/img/ee26a074d617a7fd92fe7fdbc0b65afd.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 18:01:20
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93![also seen with the Polarstern 1986 data (Gordon and Huber in press). This is a strong indicator of the WDW heat which enters the mixed layer and is trapped below the insulating blanket of sea ice. The relationship of the also seen with the Polarstern 1986 data (Gordon and Huber in press). This is a strong indicator of the WDW heat which enters the mixed layer and is trapped below the insulating blanket of sea ice. The relationship of the](https://www.pdfsearch.io/img/b72405f64994e497c00a19fba17a8cec.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 21:06:22
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94![The Minnesota and Union Glaciers cut across the dominant structural trend of the mountains, while the Newcomer and Nimitz Glaciers follow it. We also sounded along six gravity profiles made earlier by U.S. scientists stu The Minnesota and Union Glaciers cut across the dominant structural trend of the mountains, while the Newcomer and Nimitz Glaciers follow it. We also sounded along six gravity profiles made earlier by U.S. scientists stu](https://www.pdfsearch.io/img/85431c392bd0ceb8cc85aaab36285676.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 06:17:33
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95![region on the long hydrographic section is shown in figure 2. The structure of the temperature field is similar to that obtained in 1987 in this section with the exception of the top 100 meters or so where there is some region on the long hydrographic section is shown in figure 2. The structure of the temperature field is similar to that obtained in 1987 in this section with the exception of the top 100 meters or so where there is some](https://www.pdfsearch.io/img/1e8553324a41ab4f74ddfd3bb3d7ebfc.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 20:46:50
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96![RlV Nathaniel B. Palmer NBP93-1 cruise to the Larsen Ice Shelf region of the Antarctic Peninsula BENJAMIN J. SLOAN, Department of Geological Sciences, University of Texas, Austin, TexasLAWRENCE A. LAW yER, Instit RlV Nathaniel B. Palmer NBP93-1 cruise to the Larsen Ice Shelf region of the Antarctic Peninsula BENJAMIN J. SLOAN, Department of Geological Sciences, University of Texas, Austin, TexasLAWRENCE A. LAW yER, Instit](https://www.pdfsearch.io/img/0de02eaeb8d89f485f415285d338f15e.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 18:40:53
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97![bottom water out of the Weddell Sea and, thus, to estimate the formation rate of Antarctic Bottom Water. Unfortunately, we were once again frustrated in our recovery attempts. The acoustic releases that we planned to use bottom water out of the Weddell Sea and, thus, to estimate the formation rate of Antarctic Bottom Water. Unfortunately, we were once again frustrated in our recovery attempts. The acoustic releases that we planned to use](https://www.pdfsearch.io/img/59c25a36f455375248b2b73da78b691d.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 18:58:00
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98![w.ri111.1 Atlantic boundaries of the Scotia Sea, principally over the North Scotia Ridge in the region between Burdwood Bank and South Georgia Island. Evidence of geostrophic determination in the deep gap near longitude w.ri111.1 Atlantic boundaries of the Scotia Sea, principally over the North Scotia Ridge in the region between Burdwood Bank and South Georgia Island. Evidence of geostrophic determination in the deep gap near longitude](https://www.pdfsearch.io/img/45fdefccbb19e2e4d488bbf875baec76.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:27:51
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99![shale, coal, and petrified wood of Beacon Formation; many dike rocks in Beacon Formation; and Ferrar dolerite and McMurdo volcanic rocks. 4. Search for Antarctic meteorites. A joint U.S.—Japan search for meteorites was shale, coal, and petrified wood of Beacon Formation; many dike rocks in Beacon Formation; and Ferrar dolerite and McMurdo volcanic rocks. 4. Search for Antarctic meteorites. A joint U.S.—Japan search for meteorites was](https://www.pdfsearch.io/img/5c6ac9e732833d9431328192d38c78a5.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 03:38:06
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100![From a number of ridge transects, we found no ridges of greater than 4 meters draft. Over 4,400 holes were drilled for the ice thickness characterization. Figure 2 shows the mean ice thickness as a function of latitude d From a number of ridge transects, we found no ridges of greater than 4 meters draft. Over 4,400 holes were drilled for the ice thickness characterization. Figure 2 shows the mean ice thickness as a function of latitude d](https://www.pdfsearch.io/img/4bfd4c69437a8580da1253d39d85caf7.jpg) | Add to Reading ListSource URL: s3.amazonaws.comLanguage: English - Date: 2011-05-06 15:43:24
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