Do upwelled waters from the California Undercurrent contribute to high pCO2 within the fjord system of Nootka Sound, BC?

dc.contributor.authorHinde, Genevieve
dc.date.accessioned2016-07-06T02:33:24Z
dc.date.available2016-07-06T02:33:24Z
dc.date.issued2016-06
dc.descriptionSenior thesis written for Oceanography 445en_US
dc.description.abstract[author abstract] An understanding of coastal ocean-atmosphere CO2 exchange is important for modelling future greenhouse gas scenarios. This study focuses on the fjord system of Nootka Sound in December 2015. 16 stations were sampled from 60km offshore to the head of Muchalat Inlet with the aim of evaluating the influence of nutrient rich, high pCO2 waters from the California Undercurrent on the fjord system. Samples were taken throughout the water column to obtain oxygen, nutrient and carbonate system data. Net autotrophy and high nutrient waters were observed at the mouth of the fjord system; though it was thought these waters did not originate from the California Undercurrent as isopycnals were suggestive of coastal downwelling. Deep waters in the fjord had pCO2> 1500μatm and high levels of denitrification were observed. Higher pCO2 was observed in surface water compared to the atmosphere at most stations, indicating the fjord was acting as a source of atmospheric CO2.en_US
dc.description.sponsorshipUniversity of Washington School of Oceanographyen_US
dc.identifier.urihttp://hdl.handle.net/1773/36336
dc.language.isoen_USen_US
dc.subjectAtmospheric carbon dioxide -- North Pacific Ocean -- measurementen_US
dc.subjectCarbon dioxide sinks -- British Columbia -- Nootka Sounden_US
dc.titleDo upwelled waters from the California Undercurrent contribute to high pCO2 within the fjord system of Nootka Sound, BC?en_US
dc.typeOtheren_US

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