EGU24-1442, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-1442
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Extreme atmospheric rivers in a warming climate

Shuyu Wang1, Xiaohui Ma1,2, Shenghui Zhou2, Lixin Wu1,2, Hong Wang1,2, Zhili Tang1, Guangzhi Xu3, Zhao Jing1,2, Zhaohui Chen1,2, and Bolan Gan1,2
Shuyu Wang et al.
  • 1Frontiers Science Center for Deep Ocean Multispheres and Earth System and Key Laboratory of Physical Oceanography, Ocean University of China, Qingdao, China
  • 2Laoshan Laboratory, Qingdao, China
  • 3College of Global Change and Earth System Science, Beijing Normal University, Beijing, China.

Extreme atmospheric rivers (EARs) are responsible for most of the severe precipitation and disastrous flooding along the coastal regions in midlatitudes. However, the current non-eddy-resolving climate models severely underestimate (~50%) EARs, casting significant uncertainties on their future projections. Here, using an unprecedented set of eddy-resolving high-resolution simulations from the Community Earth System Model simulations, we show that the models’ ability of simulating EARs is significantly improved (despite a slight overestimate of ~10%) and the EARs are projected to increase almost linearly with temperature warming. Under the Representative Concentration Pathway 8.5 warming scenario, there will be a global doubling or more of the occurrence, integrated water vapor transport and precipitation associated with EARs, and a more concentrated tripling for the landfalling EARs, by the end of the 21st century. We further demonstrate that the coupling relationship between EARs and storms will be reduced in a warming climate, potentially influencing the predictability of future EARs.

How to cite: Wang, S., Ma, X., Zhou, S., Wu, L., Wang, H., Tang, Z., Xu, G., Jing, Z., Chen, Z., and Gan, B.: Extreme atmospheric rivers in a warming climate, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-1442, https://doi.org/10.5194/egusphere-egu24-1442, 2024.