Počet záznamů: 1  

Continuous High-Frequent Measurements of CO2, CH4 and N2O Fluxes in a Riparian Deciduous Forest: The Role of Hot Moments in 2.5 Year Period

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    SYSNO ASEP0544675
    Druh ASEPA - Abstrakt
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    NázevContinuous High-Frequent Measurements of CO2, CH4 and N2O Fluxes in a Riparian Deciduous Forest: The Role of Hot Moments in 2.5 Year Period
    Tvůrce(i) Mander, Ülo (UEK-B) RID, SAI, ORCID
    Krasnova, A. (EE)
    Schindler, Thomas (UEK-B) SAI, RID, ORCID
    Escuer-Gatius, J. (EE)
    Espenberg, M. (EE)
    Macháčová, Kateřina (UEK-B) RID, ORCID, SAI
    Pärn, J. (EE)
    Kasak, K. (EE)
    Niinemets, Ü. (EE)
    Soosaar, Kaido (UEK-B) SAI, ORCID
    Celkový počet autorů10
    Zdroj.dok.AGU Fall Meeting. - : American Geophysical Union, 2020
    Poč.str.1 s.
    AkceAGU Fall Meeting 2020
    Datum konání01.12.2020 - 17.12.2020
    Místo konáníonline everywhere
    ZeměUS - Spojené státy americké
    Typ akceWRD
    Jazyk dok.eng - angličtina
    Země vyd.US - Spojené státy americké
    Klíč. slovamethane ; nitrous oxide ; carbon dioxide ; alder ; alnus incana ; hemi-boreal forest ; soil ; tree stem ; eddy covariance
    Obor OECDPlant sciences, botany
    Institucionální podporaUEK-B - RVO:86652079
    AnotaceThe carbon and nitrogen budgets of temperate riparian forests are sensitive to interannual climatic variability. In turn, riparian
    forests are hot spots of greenhouse gas (GHG) fluxes in landscapes. Here we analyse data from the first long-term (Sept.
    2017-Dec. 2019) continuous high-frequent study of soil emissions (automated chambers) and ecosystem (eddy-covariance,
    EC) fluxes of CO , CH and N O in a 40-year old riparian grey alder forest in Estonia. It is supported by a 1.5-year study of
    CH and N O fluxes from tree stems (manual chambers).
    Based on EC data, the forest is a sequesterer of CO (-5.6 kg C ha y ) and CH (-0.35 kg C ha y ) and emitter of N O
    (0.3 kg N O-N ha y ). Hot moments (Wet: Sept.-Nov. 2017, Dry with Drought Onset: May–July 2018, Freeze–Thaw: Feb.
    2019, and Dry Minor: June 2019) play an important role in GHG fluxes. For ecosystem level fluxes of all three gases no hot
    moments were observed however, unlike several forests in the area, during the severe heat wave in summer 2018, the riparian
    forest continued sequester CO . The Wet period was remarkable due to high CH emissions from stems – almost 100% of
    ecosystem (EC) level CH came from stems. Small N O emission from stems was found in the Wet period. In contrast, soil
    N O flux was mainly depending on hot moments: about 60% of all emissions came from these periods. Especially, during
    Drought Onset when soil water content (SWC) rapidly decreased, average flux reached >150 μg N O-N m h . In this
    period, we observed a very clear optimum related to SWC – N O emission peaked at 50% SWC. During the Freeze–Thaw
    period, another hot moment of N O, clear correlation was found with near-surface air temperature. Likewise, CH emission
    from stems in the Wet period showed an optimum at 75% SWC. Surprisingly, total N O emission from the soil was about 5
    times higher than that measured at the ecosystem level. For CH the EC level flux was coherent with the sum of soil and stem
    fluxes.
    PracovištěÚstav výzkumu globální změny
    KontaktNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Rok sběru2022
Počet záznamů: 1  

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