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91rafted 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

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Language: English - Date: 2011-05-06 05:02:23
92Underlying 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

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Language: English - Date: 2011-05-06 18:01:20
93also 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

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Language: English - Date: 2011-05-06 21:06:22
94The 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

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Language: English - Date: 2011-05-06 06:17:33
95region 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

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Language: English - Date: 2011-05-06 20:46:50
96RlV 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

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Language: English - Date: 2011-05-06 18:40:53
97bottom 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

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Language: English - Date: 2011-05-06 18:58:00
98w.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

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Language: English - Date: 2011-05-06 03:27:51
99shale, 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

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Language: English - Date: 2011-05-06 03:38:06
100From 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

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Language: English - Date: 2011-05-06 15:43:24