Zobrazeno 1 - 10
of 46
pro vyhledávání: '"N.-X. Geilfus"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 1811-1824 (2022)
The episodic buildup of gas-phase reactive bromine species over sea ice and snowpack in the springtime Arctic plays an important role in boundary layer processes, causing annual concurrent depletion of ozone and gaseous elemental mercury (GEM) during
Externí odkaz:
https://doaj.org/article/d9dcfe13481f49b2934c8b7f38074e39
Autor:
N.-X. Geilfus, R. J. Galley, B. G. T. Else, K. Campbell, T. Papakyriakou, O. Crabeck, M. Lemes, B. Delille, S. Rysgaard
Publikováno v:
The Cryosphere, Vol 10, Pp 2173-2189 (2016)
The precipitation of ikaite and its fate within sea ice is still poorly understood. We quantify temporal inorganic carbon dynamics in sea ice from initial formation to its melt in a sea ice–seawater mesocosm pool from 11 to 29 January 2013. Base
Externí odkaz:
https://doaj.org/article/43e154d45fe24beaa19fffddc07f2430
Autor:
O. Crabeck, R. Galley, B. Delille, B. Else, N.-X. Geilfus, M. Lemes, M. Des Roches, P. Francus, J.-L. Tison, S. Rysgaard
Publikováno v:
The Cryosphere, Vol 10, Iss 3, Pp 1125-1145 (2016)
Although the presence of a gas phase in sea ice creates the potential for gas exchange with the atmosphere, the distribution of gas bubbles and transport of gases within the sea ice are still poorly understood. Currently no straightforward technique
Externí odkaz:
https://doaj.org/article/e962a857b96d496c95c06a9de9b17744
Publikováno v:
Biogeosciences, Vol 12, Iss 6, Pp 2047-2061 (2015)
Melt pond formation is a common feature of spring and summer Arctic sea ice, but the role and impact of sea ice melt and pond formation on both the direction and size of CO2 fluxes between air and sea is still unknown. Here we report on the CO2–car
Externí odkaz:
https://doaj.org/article/0015826b181043dd9040f8baab09d969
Publikováno v:
Biogeosciences, Vol 11, Iss 23, Pp 6525-6538 (2014)
We present the CH4 concentration [CH4], the partial pressure of CO2 (pCO2) and the total gas content in bulk sea ice from subarctic, land-fast sea ice in the Kapisillit fjord, Greenland. Fjord systems are characterized by freshwater runoff and riveri
Externí odkaz:
https://doaj.org/article/23c393a71be2431995f81ee8f95e2434
Autor:
N.-X. Geilfus, J.-L. Tison, S. F. Ackley, R. J. Galley, S. Rysgaard, L. A. Miller, B. Delille
Publikováno v:
The Cryosphere, Vol 8, Iss 6, Pp 2395-2407 (2014)
Temporal evolution of pCO2 profiles in sea ice in the Bellingshausen Sea, Antarctica, in October 2007 shows physical and thermodynamic processes controls the CO2 system in the ice. During the survey, cyclical warming and cooling strongly influenced t
Externí odkaz:
https://doaj.org/article/fff735d5b2e34991ab42eefecb50bca2
Autor:
S. Rysgaard, F. Wang, R. J. Galley, R. Grimm, D. Notz, M. Lemes, N.-X. Geilfus, A. Chaulk, A. A. Hare, O. Crabeck, B. G. T. Else, K. Campbell, L. L. Sørensen, J. Sievers, T. Papakyriakou
Publikováno v:
The Cryosphere, Vol 8, Iss 4, Pp 1469-1478 (2014)
Ikaite (CaCO3 · 6H2O) is a metastable phase of calcium carbonate that normally forms in a cold environment and/or under high pressure. Recently, ikaite crystals have been found in sea ice, and it has been suggested that their precipitation may play
Externí odkaz:
https://doaj.org/article/c1c1adab077e4cf4a0c0b9a3aa0feb90
Publikováno v:
The Cryosphere, Vol 8, Iss 3, Pp 1019-1029 (2014)
We report on methane (CH4) dynamics in landfast sea ice, brine and under-ice seawater at Barrow in 2009. The CH4 concentrations in under-ice water ranged from 25.9 to 116.4 nmol L−1sw, indicating a supersaturation of 700 to 3100% relative to the at
Externí odkaz:
https://doaj.org/article/d2e2cfa4ebc54cfe892f521a88fbdd8a
Autor:
N.-X. Geilfus, J.-L. Tison, S. F. Ackley, R. J. Galley, S. Rysgaard, L. A. Miller, B. Delille
Publikováno v:
Geilfus, N-X, Tison, J-L, Ackley, S F, Galley, R J, Rysgaard, S, Miller, L A & Delille, B 2014, ' Sea ice pCO 2 dynamics and air-ice CO 2 fluxes during the Sea Ice Mass Balance in the Antarctic (SIMBA) experiment-Bellingshausen Sea, Antarctica ', The Cryosphere Discussions, vol. 8, pp. 2395-2407 . https://doi.org/10.5194/tc-8-2395-2014
The Cryosphere, Vol 8, Iss 6, Pp 2395-2407 (2014)
The Cryosphere, Vol 8, Iss 6, Pp 2395-2407 (2014)
Temporal evolution of pCO2 profiles in sea ice in the Bellingshausen Sea, Antarctica, in October 2007 shows physical and thermodynamic processes controls the CO2 system in the ice. During the survey, cyclical warming and cooling strongly influenced t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cae96ca0b7656da36855fc18850bf790
https://www.the-cryosphere.net/8/2395/2014/
https://www.the-cryosphere.net/8/2395/2014/
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