The production of environmental change records using time-series data retrieved from ice cores has seen minimal application in the Transantarctic Mountains despite the existence of a well-developed lower resolution glacial geologic record for this area which forms the primary basis for understanding the glacial history of East Antarctica. In addition, records derived from marine and lake cores, glacier margin fluctuation studies, measures of volcanic activity, and meteorological data sets from within or close to the Transantarctic Mountains are available for comparison. This emerging environmental data-base provides the tools needed to define the change characteristics, over a period of thousands of years, of several major dynamic component...
The first section of this study presents major ion, trace element, heavy metal, rare earth element ...
Deep Antarctic ice cores document the former states of the climatic system, the atmosphere, and the ...
[From the introduction] During the 1980-81 field season we conducted a two-part program: the first p...
The production of environmental change records using time-series data retrieved from ice cores has s...
Advances in climate prediction depend on a knowledge of historical climatic sequences ranging in sca...
Localized-accumulation basins in the Transantarctic Mountains contain sites yielding ice-cores that ...
The complex atmospheric and glaciological dynamics of West Antarctica make this region of particular...
Several sites within the Transantarctic Mountains fit the requirements necessary for the retrieval o...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
Ice core records (major anions and cations, MSA, oxygen isotopes and particles) developed from two s...
Between 20 November and 14 December 1984, a remote tent camp was operated in the Dominion Range (cen...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
[From the introduction] Rock glaciers, large-scale masses of frozen debris...form a group of feature...
Deep ice cores collected from the interior of the west antarctic ice sheet and the interice stream r...
The first section of this study presents major ion, trace element, heavy metal, rare earth element ...
Deep Antarctic ice cores document the former states of the climatic system, the atmosphere, and the ...
[From the introduction] During the 1980-81 field season we conducted a two-part program: the first p...
The production of environmental change records using time-series data retrieved from ice cores has s...
Advances in climate prediction depend on a knowledge of historical climatic sequences ranging in sca...
Localized-accumulation basins in the Transantarctic Mountains contain sites yielding ice-cores that ...
The complex atmospheric and glaciological dynamics of West Antarctica make this region of particular...
Several sites within the Transantarctic Mountains fit the requirements necessary for the retrieval o...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
Ice core records (major anions and cations, MSA, oxygen isotopes and particles) developed from two s...
Between 20 November and 14 December 1984, a remote tent camp was operated in the Dominion Range (cen...
The Transantarctic Mountains of East Antarctica provide a new milieu for retrieval of ice-core recor...
[From the introduction] Rock glaciers, large-scale masses of frozen debris...form a group of feature...
Deep ice cores collected from the interior of the west antarctic ice sheet and the interice stream r...
The first section of this study presents major ion, trace element, heavy metal, rare earth element ...
Deep Antarctic ice cores document the former states of the climatic system, the atmosphere, and the ...
[From the introduction] During the 1980-81 field season we conducted a two-part program: the first p...