| 17 Titles Match Your Query |
Showing 1 through 17 of 17
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1.
Rates of depletion of lubricant and fuel contaminants from Antarctic regions during natural attenuation and remediation procedures [ASAC_2915]
CHILD DIFs
PARENT DIF
Metadata record for data expected from ASAC Project 2915
See the link below for public details on this project.
Petroleum contamination poses a major threat to Antarctic and subantarctic ecosystems ...
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2.
Subantarctic zone oceanography - SAZ Project 1997-1998 - Sediment Trap Data [ASAC_2256_Sediment]
PARENT DIF
Oceanographic processes in the subantarctic region contribute crucially to the physical and biogeochemical aspects of the global climate system. To explore and quantify these contributions, the Antarctic ...
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3.
AFI 02/48_01 - Ice-rafted debris on the Antarctic continental margin and dynamics of the Antarctic Ice Sheet - Swath Bathymetry, EM120 and TOPAS data collected from the Weddell Sea and Marguerite Bay, Feb - March 2002 [GB-NERC-BAS-AEDC-00290]
Ice-rafted (Heinrich) layers in the North Atlantic provide clear evidence that basins of large Quaternary ice sheets have, in the past, exhibited major dynamic instabilities. The presence of large ...
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4.
AFI 02/48_02 - Ice-rafted debris on the Antarctic continental margin and dynamics of the Antarctic Ice Sheet - Vibro gravity cores, and sediments data collected from the Weddell Sea, Marguerite Bay, Feb - March 2002 [GB-NERC-BAS-AEDC-00289]
Ice-rafted (Heinrich) layers in the North Atlantic provide clear evidence that basins of large Quaternary ice sheets have, in the past, exhibited major dynamic instabilities. The presence of large ...
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5.
AFI 04/17_01 - Glacial-interglacial changes in the lost drainage basin on the West Antarctic Ice Sheet - EM120 Swath Bathymetry and TOPAS sub-bottom profiler data, Bellingshausen Sea, 2004 [GB-NERC-BAS-AEDC-00273]
The main aim of this project was to carry out the first systematic investigation of the former ice drainage basin in the southern Bellingshausen Sea, using sediment cores, swath bathymetry by means ...
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6.
AFI 04/17_02 - Glacial-interglacial changes in the lost drainage basin on the West Antarctic Ice Sheet - Sediment cores collected in the Bellingshausen Sea, 2004 [GB-NERC-BAS-AEDC-00272]
The main aim of this project was to carry out the first systematic investigation of the former ice drainage basin in the southern Bellingshausen Sea, using sediment cores, swath bathymetry by means ...
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7.
Analysis of bottom sediments within the Ross Sea to determine the sedimentation regime of the area [K008_1972_1973_NZ_2]
The collection of a series of bottom grab samples in the Ross Sea were made over three weeks from the USCGS Northwind. The aim was to study the sedimentation regime in the Ross Sea. 30 grab stations ...
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8.
Do density driven bottom currents originate from beneath the Mackay Glacier Tongue in Granite Harbour? Data from current meters, bathymetry profile and sediment trap samples [K042_1988_1989_NZ_1]
Previous studies suggest that a current originating from beneath the Mackay Glacier Tongue in Granite Harbour could contribute to the deposits of mud flooring the deeper parts of McMurdo Sound and ...
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9.
Deep structure, continental margins nature and evolution of oceanic gateways in the NE border of the Antarctic Peninsula (Eastern Bransfield and Drake Passage, Antarctica [CNDP-ESP_IPY_POL2006-13836-C03-01]
En Espa?ol:
El proyecto PASOC (campa?a DRAKE2008) se desarrolla en el marco del A?o Polar Internacional 2007-09 y se integra dentro del proyecto Plates and Gates. Esta iniciativa pretende establecer ...
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10.
Wilkes Land Glacial History (WEGA) [ASAC_1044]
A collaborative Italian/Australian marine geoscience research voyage to the George Vth Land sector of the East Antarctic continental margin was carried out between 11th February and 20th March, 2000, ...
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11.
The interactions between a polar glacier tongue (Mackay Glacier Tongue and Blue Glacier), sediment and sea water at the grounding line using an ROV [K042_1991_1992_NZ_1]
The Mackay Glacier Tongue and Blue Glacier was explored with a submersible remotely operated vehicle (ROV) to determine whether sediment was being shielded by freezing or melting out onto the sea ...
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12.
The nature (speed/direction/persistence) of mud carrying bottom currents entering Granite Harbour to determine the movement of sediments entering the harbour [K042_1989_1990_NZ_2]
The movement of sediment entering Granite Harbour from the Ross Sea was investigated with the nature (speed/direction/peristence) of mud carrying bottom currents in Granite Harbour determined. The ...
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13.
The Australian Oceanographic Data Center Hydrocomp Database via World Wide Web [AODC_WWW]
The Australian Oceanographic Data Center (AODC) provides a variety of oceanographic data for the area bounded by the coordinates 80S by 150W and 30N by 20E. Data sets are currently available through ...
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14.
Barium Accumulation in the Southern Atlantic [NOAA_NCDC_PALEO_97-012]
This data set consists of
Surface data: Surface sediment sampling positions, depth, Ba xs, and Al.
Core data: Sediment core sampling positions, depth, age, linear sedimentation
rate (LSR), mass ...
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15.
Establishing the pattern of Holocene-LGM changes in sediment contributions from Antarctica to the Southern Ocean [Goldstein_OPP_0088054]
Terrigenous clastic sediments are brought to the ocean from continental sources
via rivers, ice and wind, and distributed within the ocean by surface and deep
currents. By investigating long-lived ...
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16.
Great Barrier Reef Coral Ba/Ca Data, NOAA/NCDC/WDC Paleoclimatology [NOAA_NGDC_PALEO_MCCULLOGH]
CHILD DIFs
The effect of European settlement on water quality in the Great
Barrier Reef of Australia is a long-standing and controversial
issue. Erosion and sediment transport in river catchments in this
region ...
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17.
Particle dynamics in the water column & in the water-sediment interface & their relationship with the ecophysiology of benthic particle feeders, Potter Cove [JCADM_CDA_DNA_BENTHO-PELAGIC]
In the present project the dynamics of particulate matter at the
water-bottom interface will be studied, identifying the role of the
main physical forcing factors controlling such dynamics. The relative ...
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Showing 1 through 17 of 17
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