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Author |
A. Dommergue, P. Martinerie, J. Courteaud, E. Witrant, D. M. Etheridge |
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Title |
A new reconstruction of atmospheric gaseous elemental mercury trend over the last 60 years from Greenland firn records |
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Journal |
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Year |
2016 |
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Atmospheric Environment |
Abbreviated Journal |
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Volume |
136 |
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156-164 |
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Keywords |
Archive Arctic Atmospheric mercury Firn Greenland Mercury |
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1025 |
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1352-2310 |
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8171 |
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2011 |
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Solid Earth |
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Volume |
2 |
Issue |
2 |
Pages |
303-313 |
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1021 |
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1869-9510 |
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8170 |
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Title |
Anisotropic lithosphere under the Fennoscandian shield from P receiver functions and SKS waveforms of the POLENET/LAPNET array |
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Journal |
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Year |
2014 |
Publication |
Tectonophysics |
Abbreviated Journal |
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Volume |
628 |
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Pages |
45-54 |
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Keywords |
Asthenosphere Lithosphere Mantle flow Receiver functions Seismic anisotropy Shear-wave splitting |
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1021 |
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0040-1951 |
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8169 |
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Author |
Olga Usoltseva, Elena Kozlovskaya |
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Title |
Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array |
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Journal |
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2016 |
Publication |
Solid Earth |
Abbreviated Journal |
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Volume |
7 |
Issue |
4 |
Pages |
1095-1108 |
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1021 |
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1869-9510 |
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8168 |
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Author |
Elena Kozlovskaya, Janne Narkilahti, Jouni Nevalainen, Riitta Hurskainen, Hanna Silvennoinen |
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Journal |
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Year |
2016 |
Publication |
Geoscientific Instrumentation, Methods and Data Systems |
Abbreviated Journal |
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5 |
Issue |
2 |
Pages |
365-382 |
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1201 |
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2193-0856 |
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8167 |
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Author |
Lev Vinnik, Elena Kozlovskaya, Sergey Oreshin, Grigoriy Kosarev, Katerina Piiponen, Hanna Silvennoinen |
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Title |
The lithosphere, LAB, LVZ and Lehmann discontinuity under central Fennoscandia from receiver functions |
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Journal |
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Year |
2016 |
Publication |
Tectonophysics |
Abbreviated Journal |
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Volume |
667 |
Issue |
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Pages |
189-198 |
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Keywords |
LAB Lehmann discontinuity Low-velocity zone Partial melting Receiver functions Seismic anisotropy |
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1021 |
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0040-1951 |
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8166 |
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Author |
Hanna Silvennoinen, Elena Kozlovskaya, Eduard Kissling |
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Title |
POLENET/LAPNET teleseismic P wave travel time tomography model of the upper mantle beneath northern Fennoscandia |
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Journal |
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Year |
2016 |
Publication |
Solid Earth |
Abbreviated Journal |
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Volume |
7 |
Issue |
2 |
Pages |
425-439 |
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1201 |
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1869-9510 |
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Serial ![sorted by Serial field, descending order (down)](img/sort_desc.gif) |
8165 |
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Title |
Role of Nitrite in the Photochemical Formation of Radicals in the Snow |
Type |
Journal |
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Year |
2014 |
Publication |
Environmental Science & Technology |
Abbreviated Journal |
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Volume |
48 |
Issue |
1 |
Pages |
165-172 |
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Abstract |
Photochemical reactions in snow can have an important impact on the composition of the atmosphere over snow-covered areas as well as on the composition of the snow itself. One of the major photochemical processes is the photolysis of nitrate leading to the formation of volatile nitrogen compounds. We report nitrite concentrations determined together with nitrate and hydrogen peroxide in surface snow collected at the coastal site of Barrow, Alaska. The results demonstrate that nitrite likely plays a significant role as a precursor for reactive hydroxyl radicals as well as volatile nitrogen oxides in the snow. Pollution events leading to high concentrations of nitrous acid in the atmosphere contributed to an observed increase in nitrite in the surface snow layer during nighttime. Observed daytime nitrite concentrations are much higher than values predicted from steady-state concentrations based on photolysis of nitrate and nitrite indicating that we do not fully understand the production of nitrite and nitrous acid in snow. The discrepancy between observed and expected nitrite concentrations is probably due to a combination of factors, including an incomplete understanding of the reactive environment and chemical processes in snow, and a lack of consideration of the vertical structure of snow. |
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1017 |
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0013-936X |
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8164 |
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Author |
H. W. Jacobi, D. Voisin, J. L. Jaffrezo, J. Cozic, T. A. Douglas |
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Title |
Chemical composition of the snowpack during the OASIS spring campaign 2009 at Barrow, Alaska |
Type |
Journal |
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Year |
2012 |
Publication |
Journal of Geophysical Research: Atmospheres |
Abbreviated Journal |
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Volume |
117 |
Issue |
D14 |
Pages |
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Keywords |
Alaska Arctic Barrow Chemistry Snow |
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Abstract |
The chemical composition of the seasonal snowpack was determined close to Barrow, an Arctic coastal location in northern Alaska. One hundred and twelve samples of different snow types including fresh snow, surface hoar, diamond dust, blowing snow, rounded snow grains, and depth hoar were collected and analyzed for major sea salt components, bromide, and nitrate. Sodium, chloride, sulfate, and potassium are mainly introduced into the snowpack by the deposition of sea salt, while magnesium and calcium result from a combination of sea salt and dust. Sulfate was strongly depleted in most samples compared to other sea salt components. This is attributed to the precipitation of mirabilite in newly formed sea ice and frost flowers that leads to an efficient fractionation of sulfate. Uptake of volatile but soluble species from the gas phase also contributed to the observed chloride, sulfate, and nitrate in the snow. However, for chloride and sulfate the input from the marine sources was overwhelming and the uptake from the gas phase was only visible in the samples with low concentrations like fresh snow, diamond dust, and surface hoar. Nitrate concentrations in the snowpack were less variable and for aged snow nitrate was related to the specific surface area of the snow indicating the adsorption of nitric acid can be an important nitrate source in the aged snow. Bromide was also introduced into the snowpack from marine sources, but due to its high reactivity it was partly transferred back to the atmosphere in the form of reactive species. The result of these processes was evident in bromide concentrations, which were both enriched and depleted at the snowpack surface while deeper layers were mostly depleted. Blowing snow also exhibited a depleted bromide composition. For all compounds except nitrate, many depth hoar samples exhibited the greatest concentrations, probably as a result of higher input earlier in the season as well as increases due to the sublimation of water during the metamorphism of the snow. |
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1017 |
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2156-2202 |
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8163 |
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Title |
The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities |
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Year |
2015 |
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Geoscientific Model Development |
Abbreviated Journal |
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Volume |
8 |
Issue |
10 |
Pages |
2991-3005 |
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1015,1244 |
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Bachelor's thesis |
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1991-959X |
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8162 |
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