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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ftcdlib:qt4jf45773 2023-05-15T16:28:58+02:00 Geographic variability of nitrate deposition and preservation over the Greenland ice sheet Burkhart, JF Bales, RC McConnell, JR Hutterli, MA Frey, MM D06301 2009-03-27 application/pdf http://www.escholarship.org/uc/item/4jf45773 english eng eScholarship, University of California qt4jf45773 http://www.escholarship.org/uc/item/4jf45773 public Burkhart, JF; Bales, RC; McConnell, JR; Hutterli, MA; & Frey, MM. (2009). Geographic variability of nitrate deposition and preservation over the Greenland ice sheet. Journal of Geophysical Research Atmospheres, 114(6), D06301. doi:10.1029/2008JD010600. UC Merced: Retrieved from: http://www.escholarship.org/uc/item/4jf45773 article 2009 ftcdlib https://doi.org/10.1029/2008JD010600 2018-07-13T22:52:33Z 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 μg cm -2 a -1 with a mean of 4 ± 2 μg 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 concentrations have occurred over the ice sheet in the past century. Copyright 2009 by the American Geophysical Union. Article in Journal/Newspaper Greenland Ice Sheet University of California: eScholarship Greenland Journal of Geophysical Research 114 D6 |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
English |
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 μg cm -2 a -1 with a mean of 4 ± 2 μg 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 concentrations have occurred over the ice sheet in the past century. Copyright 2009 by the American Geophysical Union. |
format |
Article in Journal/Newspaper |
author |
Burkhart, JF Bales, RC McConnell, JR Hutterli, MA Frey, MM |
spellingShingle |
Burkhart, JF Bales, RC McConnell, JR Hutterli, MA Frey, MM Geographic variability of nitrate deposition and preservation over the Greenland ice sheet |
author_facet |
Burkhart, JF Bales, RC McConnell, JR Hutterli, MA Frey, MM |
author_sort |
Burkhart, JF |
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 |
eScholarship, University of California |
publishDate |
2009 |
url |
http://www.escholarship.org/uc/item/4jf45773 |
op_coverage |
D06301 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
Burkhart, JF; Bales, RC; McConnell, JR; Hutterli, MA; & Frey, MM. (2009). Geographic variability of nitrate deposition and preservation over the Greenland ice sheet. Journal of Geophysical Research Atmospheres, 114(6), D06301. doi:10.1029/2008JD010600. UC Merced: Retrieved from: http://www.escholarship.org/uc/item/4jf45773 |
op_relation |
qt4jf45773 http://www.escholarship.org/uc/item/4jf45773 |
op_rights |
public |
op_doi |
https://doi.org/10.1029/2008JD010600 |
container_title |
Journal of Geophysical Research |
container_volume |
114 |
container_issue |
D6 |
_version_ |
1766018652198404096 |