Investigating the impact of COVID-19 on the atmospheric 14C trend and fossil carbon load at urban and background sites in Hungary
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41320%2F25%3A103472" target="_blank" >RIV/60460709:41320/25:103472 - isvavai.cz</a>
Výsledek na webu
<a href="https://resolve.cambridge.org/core/journals/radiocarbon/article/investigating-the-impact-of-covid19-on-the-atmospheric-14c-trend-and-fossil-carbon-load-at-urban-and-background-sites-in-hungary/304174642BFDF8C7887DAC4AF45A7C6A" target="_blank" >https://resolve.cambridge.org/core/journals/radiocarbon/article/investigating-the-impact-of-covid19-on-the-atmospheric-14c-trend-and-fossil-carbon-load-at-urban-and-background-sites-in-hungary/304174642BFDF8C7887DAC4AF45A7C6A</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1017/RDC.2024.133" target="_blank" >10.1017/RDC.2024.133</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Investigating the impact of COVID-19 on the atmospheric 14C trend and fossil carbon load at urban and background sites in Hungary
Popis výsledku v původním jazyce
The study analyses in situ CO2 mole fraction, (CO2)-C-14, and fossil based excess CO2 mole fraction (C-foss) data at Hegyh & aacute;ts & aacute;l (HUN) rural monitoring station (Central Europe) supplemented by passive monitoring of C-14 content of tree-rings. Through the observed period (2014-2020) we focused on revealing trends in atmospheric CO2 and C-14 levels, particularly during the year of the first COVID lockdown, in comparison to the preceding five years. In addition, monthly integrated samples of atmospheric CO2 and tree-rings from the six years were subjected to C-14 analysis. The passive tree-ring measurements focuses on two major urban areas (Budapest and Debrecen) in Hungary, along with the rural monitoring site. Results show a steady increase in CO2 levels at HUN between 2014 and 2020. The calculated fossil based excess CO2 concentrations for the initial year of COVID are in good agreement with the previous five-year averages both at 115 m and 10 m elevations. These results also show seasonal variations of CO2 mole fractions, peaking in winter and decreasing in summer. Tree-ring results from Debrecen show a good alignment with the results of the atmospheric monitoring station, and it does not show a significant fossil contribution in the urban background area during the vegetation periods. Tree-ring results from Budapest show a stronger fossil contribution compared to the Debrecen ones. Our atmospheric CO2 results do not show a large decrease in fossil CO2 atmospheric contribution during the first lockdown. We found that the use of this passive CO2 monitoring technique can provide a valuable tool for investigating such differences
Název v anglickém jazyce
Investigating the impact of COVID-19 on the atmospheric 14C trend and fossil carbon load at urban and background sites in Hungary
Popis výsledku anglicky
The study analyses in situ CO2 mole fraction, (CO2)-C-14, and fossil based excess CO2 mole fraction (C-foss) data at Hegyh & aacute;ts & aacute;l (HUN) rural monitoring station (Central Europe) supplemented by passive monitoring of C-14 content of tree-rings. Through the observed period (2014-2020) we focused on revealing trends in atmospheric CO2 and C-14 levels, particularly during the year of the first COVID lockdown, in comparison to the preceding five years. In addition, monthly integrated samples of atmospheric CO2 and tree-rings from the six years were subjected to C-14 analysis. The passive tree-ring measurements focuses on two major urban areas (Budapest and Debrecen) in Hungary, along with the rural monitoring site. Results show a steady increase in CO2 levels at HUN between 2014 and 2020. The calculated fossil based excess CO2 concentrations for the initial year of COVID are in good agreement with the previous five-year averages both at 115 m and 10 m elevations. These results also show seasonal variations of CO2 mole fractions, peaking in winter and decreasing in summer. Tree-ring results from Debrecen show a good alignment with the results of the atmospheric monitoring station, and it does not show a significant fossil contribution in the urban background area during the vegetation periods. Tree-ring results from Budapest show a stronger fossil contribution compared to the Debrecen ones. Our atmospheric CO2 results do not show a large decrease in fossil CO2 atmospheric contribution during the first lockdown. We found that the use of this passive CO2 monitoring technique can provide a valuable tool for investigating such differences
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10511 - Environmental sciences (social aspects to be 5.7)
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2025
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
RADIOCARBON
ISSN
0033-8222
e-ISSN
0033-8222
Svazek periodika
67
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
14
Strana od-do
251-264
Kód UT WoS článku
001401047700001
EID výsledku v databázi Scopus
—