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BASIC PREMISE: There is a clear north to south gradient in concentration with highest concentrations of nitrate observed in the northern regions of the ice sheet. However, there are also temperature and accumulation gradients from north to south. Are the concentration gradients a function of post-de...

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Main Authors: John F. Burkhart, Roger C. Bales, Joseph R Mcconnell, Manuel A Hutterli, Neil Moore, All V. Martin, Markus Frey
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice Sheet
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.185
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.542.185 2023-05-15T16:40:27+02:00 Corresponding author: John F. Burkhart Roger C. Bales Joseph R Mcconnell Manuel A Hutterli Neil Moore All V. Martin Markus Frey The Pennsylvania State University CiteSeerX Archives http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.185 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.185 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://eng.ucmerced.edu/people/rbales/Manuscripts/ClimasFolder/SummitFolder/no3_sva_071012/ text ftciteseerx 2016-01-08T11:07:05Z BASIC PREMISE: There is a clear north to south gradient in concentration with highest concentrations of nitrate observed in the northern regions of the ice sheet. However, there are also temperature and accumulation gradients from north to south. Are the concentration gradients a function of post-depositional effects driven by accumulation and temperature? Or are they representative of background atmospheric concentrations? If they are representative of atmospheric concentrations, has this gradient existed prior to anthropogenic influences? Text Ice Sheet Unknown
institution Open Polar
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language English
description BASIC PREMISE: There is a clear north to south gradient in concentration with highest concentrations of nitrate observed in the northern regions of the ice sheet. However, there are also temperature and accumulation gradients from north to south. Are the concentration gradients a function of post-depositional effects driven by accumulation and temperature? Or are they representative of background atmospheric concentrations? If they are representative of atmospheric concentrations, has this gradient existed prior to anthropogenic influences?
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author John F. Burkhart
Roger C. Bales
Joseph R Mcconnell
Manuel A Hutterli
Neil Moore
All V. Martin
Markus Frey
spellingShingle John F. Burkhart
Roger C. Bales
Joseph R Mcconnell
Manuel A Hutterli
Neil Moore
All V. Martin
Markus Frey
Corresponding author:
author_facet John F. Burkhart
Roger C. Bales
Joseph R Mcconnell
Manuel A Hutterli
Neil Moore
All V. Martin
Markus Frey
author_sort John F. Burkhart
title Corresponding author:
title_short Corresponding author:
title_full Corresponding author:
title_fullStr Corresponding author:
title_full_unstemmed Corresponding author:
title_sort corresponding author:
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.185
genre Ice Sheet
genre_facet Ice Sheet
op_source https://eng.ucmerced.edu/people/rbales/Manuscripts/ClimasFolder/SummitFolder/no3_sva_071012/
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.185
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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