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Enhanced regional terrestrial carbon uptake over Korea revealed by atmospheric CO2 measurements from 1999 to 2017.
Yun, Jeongmin; Jeong, Sujong; Ho, Chang-Hoi; Park, Hoonyoung; Liu, Junjie; Lee, Haeyoung; Sitch, Stephen; Friedlingstein, Pierre; Lienert, Sebastian; Lombardozzi, Danica; Haverd, Vanessa; Jain, Atual; Zaehle, Sönke; Kato, Etsushi; Tian, Hanqin; Vuichard, Nicolas; Wiltshire, Andy; Zeng, Ning.
Afiliación
  • Yun J; School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea.
  • Jeong S; Department of Environmental Planning, Graduate School of Environmental Studies, Seoul National University, Seoul, Republic of Korea.
  • Ho CH; School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea.
  • Park H; Department of Environmental Planning, Graduate School of Environmental Studies, Seoul National University, Seoul, Republic of Korea.
  • Liu J; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.
  • Lee H; Environmental Meteorology Research Division, National Institute of Meteorological Sciences, Jeju, Republic of Korea.
  • Sitch S; College of Life and Environmental Sciences, University of Exeter, Exeter, UK.
  • Friedlingstein P; College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, UK.
  • Lienert S; Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland.
  • Lombardozzi D; Climate and Global Dynamics, Terrestrial Sciences Section, National Center for Atmospheric Research, Boulder, CO, USA.
  • Haverd V; CSIRO Oceans and Atmosphere, Canberra, ACT, Australia.
  • Jain A; Department of Atmospheric Sciences, University of Illinois, Urbana, IL, USA.
  • Zaehle S; Biogeochemical Integration Department, Max Planck Institute for Biogeochemistry, Jena, Germany.
  • Kato E; Research & Development Division, Institute of Applied Energy (IAE), Tokyo, Japan.
  • Tian H; School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL, USA.
  • Vuichard N; Laboratoire des Sciences du Climat et de l'Environnement, Institut Pierre-Simon Laplace, CEA-CNRS-UVSQ, CE Orme des Merisiers, Gif-sur-Yvette CEDEX, France.
  • Wiltshire A; Met Office Hadley Centre, Exeter, UK.
  • Zeng N; Department of Atmospheric and Oceanic Science and Earth System Science, Interdisciplinary Center, University of Maryland, College Park, MD, USA.
Glob Chang Biol ; 26(6): 3368-3383, 2020 06.
Article en En | MEDLINE | ID: mdl-32125754
ABSTRACT
Understanding changes in terrestrial carbon balance is important to improve our knowledge of the regional carbon cycle and climate change. However, evaluating regional changes in the terrestrial carbon balance is challenging due to the lack of surface flux measurements. This study reveals that the terrestrial carbon uptake over the Republic of Korea has been enhanced from 1999 to 2017 by analyzing long-term atmospheric CO2 concentration measurements at the Anmyeondo Station (36.53°N, 126.32°E) located in the western coast. The influence of terrestrial carbon flux on atmospheric CO2 concentrations (ΔCO2 ) is estimated from the difference of CO2 concentrations that were influenced by the land sector (through easterly winds) and the Yellow Sea sector (through westerly winds). We find a significant trend in ΔCO2 of -4.75 ppm per decade (p < .05) during the vegetation growing season (May through October), suggesting that the regional terrestrial carbon uptake has increased relative to the surrounding ocean areas. Combined analysis with satellite measured normalized difference vegetation index and gross primary production shows that the enhanced carbon uptake is associated with significant nationwide increases in vegetation and its production. Process-based terrestrial model and inverse model simulations estimate that regional terrestrial carbon uptake increases by up to 18.9 and 8.0 Tg C for the study period, accounting for 13.4% and 5.7% of the average annual domestic carbon emissions, respectively. Atmospheric chemical transport model simulations indicate that the enhanced terrestrial carbon sink is the primary reason for the observed ΔCO2 trend rather than anthropogenic emissions and atmospheric circulation changes. Our results highlight the fact that atmospheric CO2 measurements could open up the possibility of detecting regional changes in the terrestrial carbon cycle even where anthropogenic emissions are not negligible.
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Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Carbono / Dióxido de Carbono País/Región como asunto: Asia Idioma: En Año: 2020 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Carbono / Dióxido de Carbono País/Región como asunto: Asia Idioma: En Año: 2020 Tipo del documento: Article