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A Study on the Air to Water Interfac...
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Porraz, Julianna.
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A Study on the Air to Water Interface: CO2 Flux Rate from Uvas Reservoir Located in a Mediterranean Climatic Region.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
A Study on the Air to Water Interface: CO2 Flux Rate from Uvas Reservoir Located in a Mediterranean Climatic Region./
作者:
Porraz, Julianna.
出版者:
Ann Arbor : ProQuest Dissertations & Theses, : 2023,
面頁冊數:
70 p.
附註:
Source: Masters Abstracts International, Volume: 85-02.
Contained By:
Masters Abstracts International85-02.
標題:
Biogeochemistry. -
電子資源:
https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=30522452
ISBN:
9798380038638
A Study on the Air to Water Interface: CO2 Flux Rate from Uvas Reservoir Located in a Mediterranean Climatic Region.
Porraz, Julianna.
A Study on the Air to Water Interface: CO2 Flux Rate from Uvas Reservoir Located in a Mediterranean Climatic Region.
- Ann Arbor : ProQuest Dissertations & Theses, 2023 - 70 p.
Source: Masters Abstracts International, Volume: 85-02.
Thesis (M.S.)--University of California, Davis, 2023.
Freshwater reservoirs are hotspots for methane (CH4) and carbon dioxide (CO2) fluxes released into the atmosphere; however, there is little knowledge about CO2 flux rates from reservoirs in Mediterranean climate regions. Studies show that reservoirs can either emit or absorb CO2, depending on the season and time of day. The goal of this study was to analyze CO2 and gain knowledge of the temporal variability of CO2 fluxes at Uvas Reservoir, Santa Clara County, California, in a Mediterranean climate zone. Results showed a strong diel variability of CO2, with negative flux rates (CO2 sinks) generally occurring during the nighttime. For example, in June 2021 at Uvas Reservoir, CO2 emissions decreased from -0.27 mg m-2 h-1 to -0.48 mg m-2 h-1 at night. These fluxes were also variable seasonally, where positive values (CO2 sources) in CO2 flux rates occurred during fall turnover, with a peak flux rate calculated at +1.57 mg m-2 h-1 in the daytime. This example from the fall season occurred after the reservoir had used up all the nutrients and when algae were decomposing. Lastly, the CO2 surface gas flux results from Uvas Reservoir were compared to other freshwater reservoirs within the same climatic region, different climatic regions, and other land classification types. This comparative analysis showed that Uvas Reservoir had 20% and 6.2% higher CO2 flux rates compared to a tropical climate and a temperate climate in a dry year, respectively.
ISBN: 9798380038638Subjects--Topical Terms:
545717
Biogeochemistry.
Subjects--Index Terms:
Carbon cycle
A Study on the Air to Water Interface: CO2 Flux Rate from Uvas Reservoir Located in a Mediterranean Climatic Region.
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Freshwater reservoirs are hotspots for methane (CH4) and carbon dioxide (CO2) fluxes released into the atmosphere; however, there is little knowledge about CO2 flux rates from reservoirs in Mediterranean climate regions. Studies show that reservoirs can either emit or absorb CO2, depending on the season and time of day. The goal of this study was to analyze CO2 and gain knowledge of the temporal variability of CO2 fluxes at Uvas Reservoir, Santa Clara County, California, in a Mediterranean climate zone. Results showed a strong diel variability of CO2, with negative flux rates (CO2 sinks) generally occurring during the nighttime. For example, in June 2021 at Uvas Reservoir, CO2 emissions decreased from -0.27 mg m-2 h-1 to -0.48 mg m-2 h-1 at night. These fluxes were also variable seasonally, where positive values (CO2 sources) in CO2 flux rates occurred during fall turnover, with a peak flux rate calculated at +1.57 mg m-2 h-1 in the daytime. This example from the fall season occurred after the reservoir had used up all the nutrients and when algae were decomposing. Lastly, the CO2 surface gas flux results from Uvas Reservoir were compared to other freshwater reservoirs within the same climatic region, different climatic regions, and other land classification types. This comparative analysis showed that Uvas Reservoir had 20% and 6.2% higher CO2 flux rates compared to a tropical climate and a temperate climate in a dry year, respectively.
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https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=30522452
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