CO2 and N2O dynamics in the ocean - sea ice - atmosphere system
Greenhouse gases such as carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) are well known to be indirectly responsible for many changes in the sea ice cover in the polar regions, as these regions are sensitive to global warming. The objective of this manuscript is to look at the two climat...
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| Other Authors: | , , |
| Format: | Doctoral or Postdoctoral Thesis |
| Language: | English |
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ULiège - Université de Liège
2019
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| Online Access: | https://orbi.uliege.be/handle/2268/239427 https://orbi.uliege.be/bitstream/2268/239427/1/PhD.THESIS.Final.pdf |
| Summary: | Greenhouse gases such as carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) are well known to be indirectly responsible for many changes in the sea ice cover in the polar regions, as these regions are sensitive to global warming. The objective of this manuscript is to look at the two climatic gases addressed (CO2 and N2O) and their behaviour in the ocean – sea ice – atmosphere system in the actual warming climate, thus more specifically in the Arctic. On the one hand, the dynamic of CO2 has been studied through artificial sea ice during an experiment performed on two series of mesocosms: one was filled with seawater (SW) and the other one with seawater with added filtered humic-rich river water (SWR). The addition of river water almost doubled the dissolved organic carbon (DOC) concentration in SWR and consequently affected the partial pressure of carbon dioxide (pCO2). This experiment supports previous observations showing that the pCO2 in sea ice brines is generally higher in Arctic sea ice compared to that from the Southern Ocean, especially in winter and early spring. Indeed, DOC is larger in the Arctic seawater: higher concentrations of DOC would be reflected in a greater DOC incorporation in sea ice, enhancing bacterial respiration, which in turn would increase the pCO2 in the ice. Within the same experiment, air–ice CO2 fluxes were measured continuously using automated chambers from the initial freezing of a sea ice cover until its decay. Cooling seawater prior to sea ice formation acted as a sink for atmospheric CO2, but as soon as the first ice crystals started to form, sea ice turned to a source of CO2, which lasted throughout the whole ice growth phase. Once ice decay was initiated, sea ice shifted back again to a sink of CO2. Combining measured air–ice CO2 fluxes with the pCO2 in the air and sea ice, we determined two strongly different gas transfer coefficients of CO2 at the air–ice interface between the growth and the decay phases (2.5 mol m−2 d−1 atm−1 and 0.4 mol m−2 d−1 atm−1 ... |
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