nt der
and sediment cores, reflecting the limited access to the these features were caused by the action of a grounded shelf ice. An alternative interpretation is provided by Kristoffersen et al. (2004) who argue that the mapped idge were formed Quaternary Research 63 (20Introduction A diversity of hypothe...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.463.2872 2023-05-15T14:52:47+02:00 nt der The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.463.2872 http://people.su.se/~mjako/PDF/Jakobsson_etal_2005_QR.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.463.2872 http://people.su.se/~mjako/PDF/Jakobsson_etal_2005_QR.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://people.su.se/~mjako/PDF/Jakobsson_etal_2005_QR.pdf Ice grounding Chukchi Borderland Multibeam bathymetry Iceberg scour text ftciteseerx 2016-01-08T06:44:52Z and sediment cores, reflecting the limited access to the these features were caused by the action of a grounded shelf ice. An alternative interpretation is provided by Kristoffersen et al. (2004) who argue that the mapped idge were formed Quaternary Research 63 (20Introduction A diversity of hypotheses and speculations exists about past glacial conditions in the Arctic Ocean. These vary from sea-ice-free conditions with limited glaciation on surrounding shelves (Olausson, 1985) to huge floating ice shelves, N1 km thick and fed by large ice caps that occupied the surrounding shelves (e.g., Grosswald, 1980; Hughes et al., 1977; Mercer, 1970). Testing these ideas has been difficult because of the lack of geophysical data central Arctic Ocean by surface ships. Over the past 10– 15 years, however, scientific icebreaker and nuclear Text Arctic Arctic Ocean Chukchi Ice Shelves Iceberg* Sea ice Unknown Arctic Arctic Ocean Chukchi Borderland ENVELOPE(-165.000,-165.000,77.000,77.000) Mercer ENVELOPE(65.647,65.647,-70.227,-70.227) |
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English |
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Ice grounding Chukchi Borderland Multibeam bathymetry Iceberg scour |
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Ice grounding Chukchi Borderland Multibeam bathymetry Iceberg scour nt der |
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Ice grounding Chukchi Borderland Multibeam bathymetry Iceberg scour |
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and sediment cores, reflecting the limited access to the these features were caused by the action of a grounded shelf ice. An alternative interpretation is provided by Kristoffersen et al. (2004) who argue that the mapped idge were formed Quaternary Research 63 (20Introduction A diversity of hypotheses and speculations exists about past glacial conditions in the Arctic Ocean. These vary from sea-ice-free conditions with limited glaciation on surrounding shelves (Olausson, 1985) to huge floating ice shelves, N1 km thick and fed by large ice caps that occupied the surrounding shelves (e.g., Grosswald, 1980; Hughes et al., 1977; Mercer, 1970). Testing these ideas has been difficult because of the lack of geophysical data central Arctic Ocean by surface ships. Over the past 10– 15 years, however, scientific icebreaker and nuclear |
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The Pennsylvania State University CiteSeerX Archives |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.463.2872 http://people.su.se/~mjako/PDF/Jakobsson_etal_2005_QR.pdf |
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ENVELOPE(-165.000,-165.000,77.000,77.000) ENVELOPE(65.647,65.647,-70.227,-70.227) |
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Arctic Arctic Ocean Chukchi Borderland Mercer |
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Arctic Arctic Ocean Chukchi Borderland Mercer |
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Arctic Arctic Ocean Chukchi Ice Shelves Iceberg* Sea ice |
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Arctic Arctic Ocean Chukchi Ice Shelves Iceberg* Sea ice |
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http://people.su.se/~mjako/PDF/Jakobsson_etal_2005_QR.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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