A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica

Net accumulation rates for sites on the West Antarctic Ice Sheet in Marie Byrd Land, West Antarctica are calculated based on the interpretation of nuclear bomb fallout horizons and ice core drilling data. Fallout horizons within the ice cores are correlated with known beta-particle activity levels d...

Full description

Bibliographic Details
Main Author: White, David Joseph
Other Authors: Whillans, I. M. (Ian M.)
Format: Thesis
Language:English
Published: The Ohio State University 1987
Subjects:
Online Access:http://hdl.handle.net/1811/59875
id ftohiostateu:oai:kb.osu.edu:1811/59875
record_format openpolar
spelling ftohiostateu:oai:kb.osu.edu:1811/59875 2024-06-02T07:56:04+00:00 A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica White, David Joseph Whillans, I. M. (Ian M.) 1987-12 application/pdf http://hdl.handle.net/1811/59875 en_US eng The Ohio State University The Ohio State University. Department of Geology and Mineralogy Senior Theses; 1987 http://hdl.handle.net/1811/59875 Thesis 1987 ftohiostateu 2024-05-06T11:01:40Z Net accumulation rates for sites on the West Antarctic Ice Sheet in Marie Byrd Land, West Antarctica are calculated based on the interpretation of nuclear bomb fallout horizons and ice core drilling data. Fallout horizons within the ice cores are correlated with known beta-particle activity levels deposited in Antarctic ice during the austral summers of 1954-55 and 1965-66. A BASIC program calculates the depth of the fallout horizons utilizing a database of field drilling logs. The program calculates an ice-equivilent height for the snow column above the "bomb" core sample and divides this ice column height by the age of the fallout horizon to determine the accumulation rate. An error analysis was performed to determine the effect on accumulation rate by measurements of core sample size, mass and the interpretation of fallout horizon histograms. These calculations show that the determination of ice accumulation rate changes in direct proportion to changes in measurements of the core sample's length, mass, or the precise identification of the fallout horizons. Changes in measurements of the core diameter doubly affect the accumulation rate. Accumulation rate varies locally, but a regional trend is observed in that the rate generally appears to increase with increases in elevation, local surface slope and distance from coastal regions. No embargo Thesis Antarc* Antarctic Antarctica ice core Ice Sheet Marie Byrd Land West Antarctica Ohio State University (OSU): Knowledge Bank Antarctic Austral Byrd Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) West Antarctic Ice Sheet West Antarctica
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
description Net accumulation rates for sites on the West Antarctic Ice Sheet in Marie Byrd Land, West Antarctica are calculated based on the interpretation of nuclear bomb fallout horizons and ice core drilling data. Fallout horizons within the ice cores are correlated with known beta-particle activity levels deposited in Antarctic ice during the austral summers of 1954-55 and 1965-66. A BASIC program calculates the depth of the fallout horizons utilizing a database of field drilling logs. The program calculates an ice-equivilent height for the snow column above the "bomb" core sample and divides this ice column height by the age of the fallout horizon to determine the accumulation rate. An error analysis was performed to determine the effect on accumulation rate by measurements of core sample size, mass and the interpretation of fallout horizon histograms. These calculations show that the determination of ice accumulation rate changes in direct proportion to changes in measurements of the core sample's length, mass, or the precise identification of the fallout horizons. Changes in measurements of the core diameter doubly affect the accumulation rate. Accumulation rate varies locally, but a regional trend is observed in that the rate generally appears to increase with increases in elevation, local surface slope and distance from coastal regions. No embargo
author2 Whillans, I. M. (Ian M.)
format Thesis
author White, David Joseph
spellingShingle White, David Joseph
A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
author_facet White, David Joseph
author_sort White, David Joseph
title A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
title_short A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
title_full A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
title_fullStr A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
title_full_unstemmed A determination of ice accumulation rates on the West Antarctic Ice Sheet, Marie Byrd Land, West Antarctica
title_sort determination of ice accumulation rates on the west antarctic ice sheet, marie byrd land, west antarctica
publisher The Ohio State University
publishDate 1987
url http://hdl.handle.net/1811/59875
long_lat ENVELOPE(-130.000,-130.000,-78.000,-78.000)
geographic Antarctic
Austral
Byrd
Marie Byrd Land
West Antarctic Ice Sheet
West Antarctica
geographic_facet Antarctic
Austral
Byrd
Marie Byrd Land
West Antarctic Ice Sheet
West Antarctica
genre Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
Marie Byrd Land
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
Marie Byrd Land
West Antarctica
op_relation The Ohio State University. Department of Geology and Mineralogy Senior Theses; 1987
http://hdl.handle.net/1811/59875
_version_ 1800753305513623552