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Sökning: id:"swepub:oai:DiVA.org:uu-384042" > Implications of riv...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004358naa a2200457 4500
001oai:DiVA.org:uu-384042
003SwePub
008190528s2019 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3840422 URI
024a https://doi.org/10.1080/20442041.2019.15680732 DOI
040 a (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Pasche, Natachau Limnology Center, EPFL-ENT-LIMNC, Lausanne, Switzerland; Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, EPFL-ENAC-IEE-APHYS, Lausanne, Switzerland4 aut
2451 0a Implications of river intrusion and convective mixing on the spatial and temporal variability of under-ice CO2
264 c 2019-04-30
264 1b Informa UK Limited,c 2019
338 a electronic2 rdacarrier
520 a Ice-covered periods might significantly contribute to lake emissions at ice-melt, yet a comprehensive understanding of under-ice carbon dioxide (CO2) dynamics is still lacking. This study investigated the processes driving spatiotemporal patterns of under-ice CO2 in large Lake Onego. In March 2015 and 2016, under-ice CO2, dissolved inorganic carbon (DIC), and dissolved organic carbon (DOC) distributions were measured along a river to an open-lake transect. CO2 decreased from 120/129 μmol L−1 in the river to 51/98 μmol L−1 in the bay, and 34/36 μmol L−1 in the open lake, while DOC decreased from 1.18/1.55 mmol L−1 in the river to 0.67/1.04 mmol L−1 in the bay in 2015 and 2016, respectively. These decreases in concentrations with increasing distance from the river mouth indicate that river discharge modulates spatial patterns of under-ice CO2. The variability between the 2 years was mainly driven by river discharge and ice transparency affecting the extent of under-ice convection. Higher discharge during winter 2016 resulted in higher CO2 concentrations in the bay. By contrast, intensive under-ice convection led to lower, more homogeneously distributed CO2 in 2015. In conclusion, the river-to-bay transition zone is characterized by strong CO2 variability and is therefore an important zone to consider when assessing the CO2 budget of large lakes.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Miljövetenskap0 (SwePub)105022 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Environmental Sciences0 (SwePub)105022 hsv//eng
653 a carbon dioxide
653 a convective mixing
653 a humic lake
653 a river intrusion
653 a spatial distribution
653 a under-ice
700a Hofmann, Hilmaru Environmental Physics Group, University of Konstanz - Limnological Institute, Konstanz, Germany4 aut
700a Bouffard, Damienu Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, EPFL-ENAC-IEE-APHYS, Lausanne, Switzerland; Eawag,Swiss Federal Institute of Aquatic Science and Technology, Department of Surface Waters-Research and Management, Kastanienbaum,Switzerland4 aut
700a Schubert, Carsten J.u Eawag,Swiss Federal Institute of Aquatic Science and Technology, Department of Surface Waters-Research and Management, Kastanienbaum, Switzerland4 aut
700a Lozovik, Petr A.u Northern Water Problems Institute, Karelian Research Center, Russian Academy of Sciences, Petrozavodsk, Russia4 aut
700a Sobek, Sebastianu Uppsala universitet,Limnologi4 aut0 (Swepub:uu)sebasobe
710a Limnology Center, EPFL-ENT-LIMNC, Lausanne, Switzerland; Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, EPFL-ENAC-IEE-APHYS, Lausanne, Switzerlandb Environmental Physics Group, University of Konstanz - Limnological Institute, Konstanz, Germany4 org
773t Inland Watersd : Informa UK Limitedg 9:2, s. 162-176q 9:2<162-176x 2044-2041x 2044-205X
856u https://doi.org/10.1080/20442041.2019.1568073y Fulltext
856u https://uu.diva-portal.org/smash/get/diva2:1318722/FULLTEXT01.pdfx primaryx Raw objecty fulltext:print
856u https://www.tandfonline.com/doi/pdf/10.1080/20442041.2019.1568073?needAccess=true
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-384042
8564 8u https://doi.org/10.1080/20442041.2019.1568073

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