首页 | 本学科首页   官方微博 | 高级检索  
   检索      


Enhanced regional terrestrial carbon uptake over Korea revealed by atmospheric CO2 measurements from 1999 to 2017
Authors:Jeongmin Yun  Sujong Jeong  Chang‐Hoi Ho  Hoonyoung Park  Junjie Liu  Haeyoung Lee  Stephen Sitch  Pierre Friedlingstein  Sebastian Lienert  Danica Lombardozzi  Vanessa Haverd  Atual Jain  Snke Zaehle  Etsushi Kato  Hanqin Tian  Nicolas Vuichard  Andy Wiltshire  Ning Zeng
Institution:Jeongmin Yun,Sujong Jeong,Chang‐Hoi Ho,Hoonyoung Park,Junjie Liu,Haeyoung Lee,Stephen Sitch,Pierre Friedlingstein,Sebastian Lienert,Danica Lombardozzi,Vanessa Haverd,Atual Jain,Sönke Zaehle,Etsushi Kato,Hanqin Tian,Nicolas Vuichard,Andy Wiltshire,Ning Zeng
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.
Keywords:atmospheric CO2 measurements  carbon cycle  CT2017  GEOS‐Chem  NDVI  Republic of Korea  terrestrial carbon flux  terrestrial ecosystems  TRENDY
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号