Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet
An analysis of 96 snow pit and ice cores distributed over the Greenland ice sheet is used to determine the main drivers of variability in the preserved records of nitrate concentration. The data set provides samples from spatially distributed locations, allowing us to investigate the effect of snow...
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American Geophysical Union
2009
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ftnerc:oai:nora.nerc.ac.uk:10781 2023-05-15T16:28:41+02:00 Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet Burkhart, John F. Bales, Roger C. McConnnell, Joseph R. Hutterli, Manuel A. Frey, Markus M. 2009 http://nora.nerc.ac.uk/id/eprint/10781/ https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2008JD010600 unknown American Geophysical Union Burkhart, John F.; Bales, Roger C.; McConnnell, Joseph R.; Hutterli, Manuel A.; Frey, Markus M. orcid:0000-0003-0535-0416 . 2009 Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet. Journal of Geophysical Research, 114 (D6), D06301. 15, pp. https://doi.org/10.1029/2008JD010600 <https://doi.org/10.1029/2008JD010600> Meteorology and Climatology Glaciology Publication - Article PeerReviewed 2009 ftnerc https://doi.org/10.1029/2008JD010600 2023-02-04T19:26:54Z An analysis of 96 snow pit and ice cores distributed over the Greenland ice sheet is used to determine the main drivers of variability in the preserved records of nitrate concentration. The data set provides samples from spatially distributed locations, allowing us to investigate the effect of snow accumulation rate, temperature, and sublimation on nitrate concentration. The mean ice sheet concentration in the dry snow zone (2000 >= mean annual sea level (masl)) is 132 ng g(-1), ranging between 47 and 265 ng g(-1) with a standard deviation of +/-37 ng g(-1). Nitrate flux varies between 1.1 and 14.7 mu g cm(-2) a(-1) with a mean of 4 +/- 2 mu g cm(-2) a(-1). Large-scale spatial variability exists as a result of accumulation gradients, with concentration 5% greater in the northern plateau, yet flux over the northern plateau is 30% lower than the dry snow zone as a whole. While spatially, flux appears to be more dependent on accumulation, preservation of flux shows increasing dependence on concentration with increasing accumulation. The relationship between concentration and accumulation is nonlinear, showing less dependence in the low-accumulation regions versus high-accumulation regions. Accumulation alone is insufficient to account for the observed variability in nitrate flux in the low-accumulation regions, and evidence supports the need for additional components to a transfer function model for nitrate that includes photochemistry, temperature, and sublimation. Spatial variability across the ice sheet is nonuniform, and changes in nitrate concentration have occurred in some regions at a greater rate than others. While the data support that overall the ice sheet acts as an archive of paleoatmospheric concentration despite the effects of postdepositional processing, one needs to consider spatial variables to properly account for trends and variability in the records. This is tested by evaluating past spatial relationships and yields the result that the significant geographic shifts with respect to reactive N ... Article in Journal/Newspaper Greenland Ice Sheet Natural Environment Research Council: NERC Open Research Archive Greenland Journal of Geophysical Research 114 D6 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
topic |
Meteorology and Climatology Glaciology |
spellingShingle |
Meteorology and Climatology Glaciology Burkhart, John F. Bales, Roger C. McConnnell, Joseph R. Hutterli, Manuel A. Frey, Markus M. Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
topic_facet |
Meteorology and Climatology Glaciology |
description |
An analysis of 96 snow pit and ice cores distributed over the Greenland ice sheet is used to determine the main drivers of variability in the preserved records of nitrate concentration. The data set provides samples from spatially distributed locations, allowing us to investigate the effect of snow accumulation rate, temperature, and sublimation on nitrate concentration. The mean ice sheet concentration in the dry snow zone (2000 >= mean annual sea level (masl)) is 132 ng g(-1), ranging between 47 and 265 ng g(-1) with a standard deviation of +/-37 ng g(-1). Nitrate flux varies between 1.1 and 14.7 mu g cm(-2) a(-1) with a mean of 4 +/- 2 mu g cm(-2) a(-1). Large-scale spatial variability exists as a result of accumulation gradients, with concentration 5% greater in the northern plateau, yet flux over the northern plateau is 30% lower than the dry snow zone as a whole. While spatially, flux appears to be more dependent on accumulation, preservation of flux shows increasing dependence on concentration with increasing accumulation. The relationship between concentration and accumulation is nonlinear, showing less dependence in the low-accumulation regions versus high-accumulation regions. Accumulation alone is insufficient to account for the observed variability in nitrate flux in the low-accumulation regions, and evidence supports the need for additional components to a transfer function model for nitrate that includes photochemistry, temperature, and sublimation. Spatial variability across the ice sheet is nonuniform, and changes in nitrate concentration have occurred in some regions at a greater rate than others. While the data support that overall the ice sheet acts as an archive of paleoatmospheric concentration despite the effects of postdepositional processing, one needs to consider spatial variables to properly account for trends and variability in the records. This is tested by evaluating past spatial relationships and yields the result that the significant geographic shifts with respect to reactive N ... |
format |
Article in Journal/Newspaper |
author |
Burkhart, John F. Bales, Roger C. McConnnell, Joseph R. Hutterli, Manuel A. Frey, Markus M. |
author_facet |
Burkhart, John F. Bales, Roger C. McConnnell, Joseph R. Hutterli, Manuel A. Frey, Markus M. |
author_sort |
Burkhart, John F. |
title |
Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
title_short |
Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
title_full |
Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
title_fullStr |
Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
title_full_unstemmed |
Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet |
title_sort |
geographic variability of nitrate deposition and preservation over the greenland ice sheet |
publisher |
American Geophysical Union |
publishDate |
2009 |
url |
http://nora.nerc.ac.uk/id/eprint/10781/ https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2008JD010600 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_relation |
Burkhart, John F.; Bales, Roger C.; McConnnell, Joseph R.; Hutterli, Manuel A.; Frey, Markus M. orcid:0000-0003-0535-0416 . 2009 Geographic variability of nitrate deposition and preservation over the Greenland Ice Sheet. Journal of Geophysical Research, 114 (D6), D06301. 15, pp. https://doi.org/10.1029/2008JD010600 <https://doi.org/10.1029/2008JD010600> |
op_doi |
https://doi.org/10.1029/2008JD010600 |
container_title |
Journal of Geophysical Research |
container_volume |
114 |
container_issue |
D6 |
_version_ |
1766018355304595456 |