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| Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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| Format: | Preprint |
| Published: |
2025
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| Subjects: | |
| Online Access: | https://arxiv.org/abs/2504.09189 |
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| _version_ | 1866910910519443456 |
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| author | Ke, Piyu Ciais, Philippe Yao, Yitong Sitch, Stephen Li, Wei Xu, Yidi Du, Xiaomeng Gui, Xiaofan Bastos, Ana Zaehle, Sonke Poulter, Ben Colligan, Thomas van der Woude, Auke M. Peters, Wouter Liu, Zhu Jin, Zhe Tian, Xiangjun Wang, Yilong Liu, Junjie Pandey, Sudhanshu O'Dell, Chris Bian, Jiang Zhou, Chuanlong Miller, John Lan, Xin O'Sullivan, Michael Friedlingstein, Pierre van der Werf, Guido R. Peters, Glen P. Piao, Shilong Chevallier, Frederic |
| author_facet | Ke, Piyu Ciais, Philippe Yao, Yitong Sitch, Stephen Li, Wei Xu, Yidi Du, Xiaomeng Gui, Xiaofan Bastos, Ana Zaehle, Sonke Poulter, Ben Colligan, Thomas van der Woude, Auke M. Peters, Wouter Liu, Zhu Jin, Zhe Tian, Xiangjun Wang, Yilong Liu, Junjie Pandey, Sudhanshu O'Dell, Chris Bian, Jiang Zhou, Chuanlong Miller, John Lan, Xin O'Sullivan, Michael Friedlingstein, Pierre van der Werf, Guido R. Peters, Glen P. Piao, Shilong Chevallier, Frederic |
| contents | The high growth rate of atmospheric CO2 in 2023 was found to be caused by a severe reduction of the global net land carbon sink. Here we update the global CO2 budget from January 1st to July 1st 2024, during which El Niño drought conditions continued to prevail in the Tropics but ceased by March 2024. We used three dynamic global vegetation models (DGVMs), machine learning emulators of ocean models, three atmospheric inversions driven by observations from the second Orbiting Carbon Observatory (OCO-2) satellite, and near-real-time fossil CO2 emissions estimates. In a one-year period from July 2023 to July 2024 covering the El Niño 2023/24 event, we found a record-high CO2 growth rate of 3.66~$\pm$~0.09 ppm~yr$^{-1}$ ($\pm$~1 standard deviation) since 1979. Yet, the CO2 growth rate anomaly obtained after removing the long term trend is 1.1 ppm~yr$^{-1}$, which is marginally smaller than the July--July growth rate anomalies of the two major previous El Niño events in 1997/98 and 2015/16. The atmospheric CO2 growth rate anomaly was primarily driven by a 2.24 GtC~yr$^{-1}$ reduction in the net land sink including 0.3 GtC~yr$^{-1}$ of fire emissions, partly offset by a 0.38 GtC~yr$^{-1}$ increase in the ocean sink relative to the 2015--2022 July--July mean. The tropics accounted for 97.5\% of the land CO2 flux anomaly, led by the Amazon (50.6\%), central Africa (34\%), and Southeast Asia (8.2\%), with extra-tropical sources in South Africa and southern Brazil during April--July 2024. Our three DGVMs suggest greater tropical CO2 losses in 2023/2024 than during the two previous large El Niño in 1997/98 and 2015/16, whereas inversions indicate losses more comparable to 2015/16. Overall, this update of the low latency budget highlights the impact of recent El Niño droughts in explaining the high CO2 growth rate until July 2024. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2504_09189 |
| institution | arXiv |
| publishDate | 2025 |
| record_format | arxiv |
| spellingShingle | Low latency global carbon budget reveals a continuous decline of the land carbon sink during the 2023/24 El Nino event Ke, Piyu Ciais, Philippe Yao, Yitong Sitch, Stephen Li, Wei Xu, Yidi Du, Xiaomeng Gui, Xiaofan Bastos, Ana Zaehle, Sonke Poulter, Ben Colligan, Thomas van der Woude, Auke M. Peters, Wouter Liu, Zhu Jin, Zhe Tian, Xiangjun Wang, Yilong Liu, Junjie Pandey, Sudhanshu O'Dell, Chris Bian, Jiang Zhou, Chuanlong Miller, John Lan, Xin O'Sullivan, Michael Friedlingstein, Pierre van der Werf, Guido R. Peters, Glen P. Piao, Shilong Chevallier, Frederic Atmospheric and Oceanic Physics The high growth rate of atmospheric CO2 in 2023 was found to be caused by a severe reduction of the global net land carbon sink. Here we update the global CO2 budget from January 1st to July 1st 2024, during which El Niño drought conditions continued to prevail in the Tropics but ceased by March 2024. We used three dynamic global vegetation models (DGVMs), machine learning emulators of ocean models, three atmospheric inversions driven by observations from the second Orbiting Carbon Observatory (OCO-2) satellite, and near-real-time fossil CO2 emissions estimates. In a one-year period from July 2023 to July 2024 covering the El Niño 2023/24 event, we found a record-high CO2 growth rate of 3.66~$\pm$~0.09 ppm~yr$^{-1}$ ($\pm$~1 standard deviation) since 1979. Yet, the CO2 growth rate anomaly obtained after removing the long term trend is 1.1 ppm~yr$^{-1}$, which is marginally smaller than the July--July growth rate anomalies of the two major previous El Niño events in 1997/98 and 2015/16. The atmospheric CO2 growth rate anomaly was primarily driven by a 2.24 GtC~yr$^{-1}$ reduction in the net land sink including 0.3 GtC~yr$^{-1}$ of fire emissions, partly offset by a 0.38 GtC~yr$^{-1}$ increase in the ocean sink relative to the 2015--2022 July--July mean. The tropics accounted for 97.5\% of the land CO2 flux anomaly, led by the Amazon (50.6\%), central Africa (34\%), and Southeast Asia (8.2\%), with extra-tropical sources in South Africa and southern Brazil during April--July 2024. Our three DGVMs suggest greater tropical CO2 losses in 2023/2024 than during the two previous large El Niño in 1997/98 and 2015/16, whereas inversions indicate losses more comparable to 2015/16. Overall, this update of the low latency budget highlights the impact of recent El Niño droughts in explaining the high CO2 growth rate until July 2024. |
| title | Low latency global carbon budget reveals a continuous decline of the land carbon sink during the 2023/24 El Nino event |
| topic | Atmospheric and Oceanic Physics |
| url | https://arxiv.org/abs/2504.09189 |