Sea ice and the air-sea exchange of CO2

The objective of this thesis was to improve the state of knowledge concerning the inorganic carbon dynamics, including the precipitation of CaCO3 in sea ice and its significance for the polar carbon cycle as well as to obtain improved estimates of the diurnal and long-term CO2 flux on small scales d...

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Bibliographic Details
Main Author: Fischer, Michael
Other Authors: Wolf-Gladrow, Dieter, Dieckmann, Gerhard, Eicken, Hajo
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2013
Subjects:
CO2
550
Online Access:https://media.suub.uni-bremen.de/handle/elib/463
https://nbn-resolving.org/urn:nbn:de:gbv:46-00103066-17
id ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/463
record_format openpolar
spelling ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/463 2023-05-15T14:04:15+02:00 Sea ice and the air-sea exchange of CO2 Meereis und der Austausch von CO2 zwischen Ozean und Atmosphäre Fischer, Michael Wolf-Gladrow, Dieter Dieckmann, Gerhard Eicken, Hajo 2013-02-12 application/pdf https://media.suub.uni-bremen.de/handle/elib/463 https://nbn-resolving.org/urn:nbn:de:gbv:46-00103066-17 eng eng Universität Bremen FB2 Biologie/Chemie https://media.suub.uni-bremen.de/handle/elib/463 urn:nbn:de:gbv:46-00103066-17 info:eu-repo/semantics/openAccess sea ice Arctic Antarctic CO2 flux ikaite biogeochemistry carbonate chemistry polar oceans chamber technique 550 550 Earth sciences and geology ddc:550 Dissertation doctoralThesis 2013 ftsubbremen 2022-11-09T07:09:22Z The objective of this thesis was to improve the state of knowledge concerning the inorganic carbon dynamics, including the precipitation of CaCO3 in sea ice and its significance for the polar carbon cycle as well as to obtain improved estimates of the diurnal and long-term CO2 flux on small scales during the winter-spring-summer transition. To study the exchange of CO2 between sea ice and the atmosphere as well as the biogeochemical parameters and the spatial and temporal distribution of ikaite in sea ice during different seasons, three field studies were conducted in the Arctic and Antarctic. High pCO2 values in sea ice of up to 3900 μatm were observed. The resulting fluxes ranged between -3.41 and 9.5 mmol m-2 d-1. Ikaite was found mostly in the uppermost layers of sea ice. Based on the observations the efflux from Arctic sea ice to the atmosphere can be expected to result in a flux of several Tg C a-1. The findings in this thesis support the concept of the sea ice driven carbon pump. Doctoral or Postdoctoral Thesis Antarc* Antarctic Arctic Sea ice Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) Antarctic Arctic
institution Open Polar
collection Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen)
op_collection_id ftsubbremen
language English
topic sea ice
Arctic
Antarctic
CO2
flux
ikaite
biogeochemistry
carbonate chemistry
polar oceans
chamber technique
550
550 Earth sciences and geology
ddc:550
spellingShingle sea ice
Arctic
Antarctic
CO2
flux
ikaite
biogeochemistry
carbonate chemistry
polar oceans
chamber technique
550
550 Earth sciences and geology
ddc:550
Fischer, Michael
Sea ice and the air-sea exchange of CO2
topic_facet sea ice
Arctic
Antarctic
CO2
flux
ikaite
biogeochemistry
carbonate chemistry
polar oceans
chamber technique
550
550 Earth sciences and geology
ddc:550
description The objective of this thesis was to improve the state of knowledge concerning the inorganic carbon dynamics, including the precipitation of CaCO3 in sea ice and its significance for the polar carbon cycle as well as to obtain improved estimates of the diurnal and long-term CO2 flux on small scales during the winter-spring-summer transition. To study the exchange of CO2 between sea ice and the atmosphere as well as the biogeochemical parameters and the spatial and temporal distribution of ikaite in sea ice during different seasons, three field studies were conducted in the Arctic and Antarctic. High pCO2 values in sea ice of up to 3900 μatm were observed. The resulting fluxes ranged between -3.41 and 9.5 mmol m-2 d-1. Ikaite was found mostly in the uppermost layers of sea ice. Based on the observations the efflux from Arctic sea ice to the atmosphere can be expected to result in a flux of several Tg C a-1. The findings in this thesis support the concept of the sea ice driven carbon pump.
author2 Wolf-Gladrow, Dieter
Dieckmann, Gerhard
Eicken, Hajo
format Doctoral or Postdoctoral Thesis
author Fischer, Michael
author_facet Fischer, Michael
author_sort Fischer, Michael
title Sea ice and the air-sea exchange of CO2
title_short Sea ice and the air-sea exchange of CO2
title_full Sea ice and the air-sea exchange of CO2
title_fullStr Sea ice and the air-sea exchange of CO2
title_full_unstemmed Sea ice and the air-sea exchange of CO2
title_sort sea ice and the air-sea exchange of co2
publisher Universität Bremen
publishDate 2013
url https://media.suub.uni-bremen.de/handle/elib/463
https://nbn-resolving.org/urn:nbn:de:gbv:46-00103066-17
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Sea ice
op_relation https://media.suub.uni-bremen.de/handle/elib/463
urn:nbn:de:gbv:46-00103066-17
op_rights info:eu-repo/semantics/openAccess
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