FN Archimer Export Format
PT J
TI Enhance seasonal amplitude of atmospheric CO2 by the changing Southern Ocean carbon sink
BT 
AF Yun, Jeongmin
   Jeong, Sujong
   Gruber, Nicolas
   Gregor, Luke
   Ho, Chang-Hoi
   Piao, Shilong
   Ciais, Philippe
   Schimel, David
   Kwon, Eun Young
AS 1:1,2;2:1,2;3:3;4:3;5:4;6:5,6;7:7;8:8;9:9,10;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 Department of Environmental Planning, Graduate School of Environmental Studies, Seoul National University, Seoul, Republic of Korea.
   Environmental Planning Institute, Seoul National University, Seoul, Republic of Korea.
   Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, Zurich, Switzerland.
   School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea.
   Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.
   Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China.
   Laboratoire des Sciences du Climat et de l’Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France.
   Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91101, USA.
   Center for Climate Physics, Institute for Basic Science, Busan, Republic of Korea.
   Pusan National University, Busan, Republic of Korea.
C2 UNIV SEOUL NATL, SOUTH KOREA
   UNIV SEOUL NATL, SOUTH KOREA
   ETH ZURICH, SWITZERLAND
   UNIV SEOUL NATL, SOUTH KOREA
   UNIV PEKING, CHINA
   ITP, CHINA
   LSCE, FRANCE
   JET PROP LAB, USA
   IBS, SOUTH KOREA
   UNIV PUSAN NATL, SOUTH KOREA
IN DOAJ
IF 13.6
TC 6
UR https://archimer.ifremer.fr/doc/00801/91321/97131.pdf
LA English
DT Article
CR OISO - OCÉAN INDIEN SERVICE D'OBSERVATION
AB The enhanced seasonal amplitude of atmospheric CO 2 has been viewed so far primarily as a Northern Hemisphere phenomenon. Yet, analyses of atmospheric CO 2 records from 49 stations between 1980 and 2018 reveal substantial trends and variations in this amplitude globally. While no significant trends can be discerned before 2000 in most places, strong positive trends emerge after 2000 in the southern high latitudes. Using factorial simulations with an atmospheric transport model and analyses of surface ocean P co 2 observations, we show that the increase is best explained by the onset of increasing seasonality of air-sea CO 2 exchange over the Southern Ocean around 2000. Underlying these changes is the long-term ocean acidification trend that tends to enhance the seasonality of the air-sea fluxes, but this trend is modified by the decadal variability of the Southern Ocean carbon sink. The seasonal variations of atmospheric CO 2 thus emerge as a sensitive recorder of the variations of the Southern Ocean carbon sink. 
PY 2022
PD OCT
SO Science Advances
SN 2375-2548
PU American Association for the Advancement of Science (AAAS)
VL 8
IS 41
UT 000882137600013
DI 10.1126/sciadv.abq0220
ID 91321
ER

EF