Low frequency changes in CO2 concentration in East Asia related to Pacific decadal oscillation and Atlantic multi-decadal oscillation for mid-summer and early fall

被引:2
|
作者
Yeh, Sang-Wook [1 ,5 ]
Ma, Seung-Joo [1 ]
Park, In -Hong [1 ]
Park, Hee-Jeong [1 ]
Kug, Jong-Seong [2 ,3 ,4 ]
机构
[1] Hanyang Univ, Dept Marine Sci & Convergent Technol, ERICA, Pohang, South Korea
[2] Pohang Univ Sci & Technol, Div Environm Sci & Engn, Pohang, South Korea
[3] Yonsei Univ, Inst Convergence Res & Educ Adv Technol, Seoul, South Korea
[4] Yonsei Univ, Irreversible Climate Change Res Ctr, Dept Atmospher Sci, Seoul, South Korea
[5] Hanyang Univ, Ansan, South Korea
关键词
CO2; concentration; Low-frequency variability; Sea surface temperatures; Terrestrial vegetation activity; Precipitation; SEASONAL AMPLITUDE INCREASE; ATMOSPHERIC CO2; TERRESTRIAL ECOSYSTEMS; CARBON FLUXES; MAUNA-LOA; EL-NINO; VARIABILITY; CYCLE; TEMPERATURE; CLIMATE;
D O I
10.1016/j.scitotenv.2023.162377
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The climatological seasonal maximum and minimum CO2 concentrations in East Asia for 1987-2020 have been re-corded at April and August, respectively. We found that the CO2 concentration in East Asia during July, August, and September (JAS) is lower than normal before the late 1990s and after the early 2010s (Low_CO2 period), and higher than normal from the late 1990s to the early 2010s (High_CO2 period). The low-frequency variability of CO2 concen-tration in East Asia during JAS correlates with both Pacific Decadal Oscillation (PDO) and Atlantic Multi-decadal Os-cillation (AMO)-related sea surface temperatures (SSTs). We analyzed atmospheric and oceanic conditions during JAS between the two periods, finding that precipitation in East Asia decreased during JAS in High_CO2 period than that in Low_CO2 period, possibly due to PDO and AMO-related SST forcing, which decreases vegetation's photosynthetic ac-tivity. This may lead to a higher CO2 concentration than normal in East Asia in High_CO2 period through reduced up-take of CO2 from the atmosphere. This implies that terrestrial vegetation activity influenced by remote SST forcings should be monitored to better understand regional carbon cycles in East Asia.
引用
收藏
页数:11
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