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dc.rights.licenseCC-BY-NC-ND
dc.contributor.advisorWolthers, Mariëtte
dc.contributor.authorRoozendaal, Anne
dc.date.accessioned2023-10-25T23:01:13Z
dc.date.available2023-10-25T23:01:13Z
dc.date.issued2023
dc.identifier.urihttps://studenttheses.uu.nl/handle/20.500.12932/45427
dc.description.abstractThe anthropogenic carbon (Cant) concentration at 40°S in the Atlantic Ocean was calculated over the period 1972-2014. The C* method was used to eliminate the biological fraction of the total DIC, both AOU and NO3 were used in the calculations. With the use of a multiple linear regression method the size of the oceanic CO2 sink over this period was determined as 34.9 ± 3.19 mol m-2 for Cant-AOU and 35.9 ± 3.71 mol m-2 for Cant-NO3. Roughly 100% of the total DIC increase over this period can be related to the increase in Cant concentration. In the depth range where the products of organic matter remineralization are high on top of the Cant increase, the decreased TA/DIC ratio results in an increased sensitivity for the pCO2, pH and H+ ions. The carbonate system acts as a whole and is altered upon additions of CO2 to the surface ocean.
dc.description.sponsorshipUtrecht University
dc.language.isoEN
dc.subjectIk heb een methode gebruikt om het menselijke aandeel van de totale koolstof in de oceaan op 40°ZB te berekenen waar de koolstof die door biologische activiteit is toegevoegd wordt geëlimineerd, waardoor de koolstof die overblijft het menselijke aandeel is. Dit was gedaan voor alle jaren waar data voor was om te zien hoe dit door de tijd is veranderd.
dc.titleAnthropogenic carbon in the Atlantic Ocean at 40°S from 1972 to 2014
dc.type.contentMaster Thesis
dc.rights.accessrightsOpen Access
dc.subject.keywordsAnthropogenic carbon
dc.subject.courseuuEarth, Life and Climate
dc.thesis.id25523


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