Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica
The concentration of microparticles in the 216 4 m long ice core from “Byrd” station Antarctica, varies cyclically. Highest concentrations of 0.65 μm diameter microparticles occur where oxygen-isotope studies show lowest paleotemperatures. The age of the bottom ice estimated from microparticle-conce...
Published in: | Journal of Glaciology |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1975
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000021948 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021948 |
id |
crcambridgeupr:10.1017/s0022143000021948 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0022143000021948 2024-03-03T08:38:16+00:00 Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica Thompson, Lonnie G. Hamilton, Wayne L. Bull, Colin 1975 http://dx.doi.org/10.1017/s0022143000021948 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021948 en eng Cambridge University Press (CUP) Journal of Glaciology volume 14, issue 72, page 433-444 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000021948 2024-02-08T08:37:11Z The concentration of microparticles in the 216 4 m long ice core from “Byrd” station Antarctica, varies cyclically. Highest concentrations of 0.65 μm diameter microparticles occur where oxygen-isotope studies show lowest paleotemperatures. The age of the bottom ice estimated from microparticle-concentration variations, assuming an annual cycle, is 27 000 years, much less than from oxygen-isotope studies. Article in Journal/Newspaper Antarc* Antarctica ice core Journal of Glaciology Cambridge University Press Byrd Byrd Station ENVELOPE(-119.533,-119.533,-80.017,-80.017) Journal of Glaciology 14 72 433 444 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Thompson, Lonnie G. Hamilton, Wayne L. Bull, Colin Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
topic_facet |
Earth-Surface Processes |
description |
The concentration of microparticles in the 216 4 m long ice core from “Byrd” station Antarctica, varies cyclically. Highest concentrations of 0.65 μm diameter microparticles occur where oxygen-isotope studies show lowest paleotemperatures. The age of the bottom ice estimated from microparticle-concentration variations, assuming an annual cycle, is 27 000 years, much less than from oxygen-isotope studies. |
format |
Article in Journal/Newspaper |
author |
Thompson, Lonnie G. Hamilton, Wayne L. Bull, Colin |
author_facet |
Thompson, Lonnie G. Hamilton, Wayne L. Bull, Colin |
author_sort |
Thompson, Lonnie G. |
title |
Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
title_short |
Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
title_full |
Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
title_fullStr |
Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
title_full_unstemmed |
Climatological, Implications of Microparticle Concentrations in the Ice Core From “Byrd” Station, Western Antarctica |
title_sort |
climatological, implications of microparticle concentrations in the ice core from “byrd” station, western antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1017/s0022143000021948 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021948 |
long_lat |
ENVELOPE(-119.533,-119.533,-80.017,-80.017) |
geographic |
Byrd Byrd Station |
geographic_facet |
Byrd Byrd Station |
genre |
Antarc* Antarctica ice core Journal of Glaciology |
genre_facet |
Antarc* Antarctica ice core Journal of Glaciology |
op_source |
Journal of Glaciology volume 14, issue 72, page 433-444 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021948 |
container_title |
Journal of Glaciology |
container_volume |
14 |
container_issue |
72 |
container_start_page |
433 |
op_container_end_page |
444 |
_version_ |
1792506127402926080 |