Xu et al. (2026) Multiscale processes maintaining a baroclinic Mongolian Plateau high and anchoring extreme rainfall over North China during Typhoon Doksuri (2023)

Identification

• Journal: Atmospheric Research
• Year: 2026
• Date: 2026-04-01
• Authors: Chengyu Xu, Li Tao
• DOI: 10.1016/j.atmosres.2026.108982

Research Groups

• Chengyu Xu
• Li Tao

Short Summary

This study investigates the multiscale atmospheric processes responsible for maintaining a baroclinic Mongolian Plateau high and its role in anchoring extreme rainfall over North China during Typhoon Doksuri in 2023.

Objective

• To identify and analyze the multiscale processes that maintain a baroclinic Mongolian Plateau high and explain how these processes anchor extreme rainfall over North China during Typhoon Doksuri (2023).

Study Configuration

• Spatial Scale: Regional (Mongolian Plateau, North China)
• Temporal Scale: Event-specific (Typhoon Doksuri, 2023)

Methodology and Data

• Models used: Not specified in the provided text.
• Data sources: Not specified in the provided text.

Main Results

• Not specified in the provided text.

Contributions

• Not specified in the provided text.

Funding

• Not specified in the provided text.

Citation

@article{Xu2026Multiscale,
  author = {Xu, Chengyu and Tao, Li},
  title = {Multiscale processes maintaining a baroclinic Mongolian Plateau high and anchoring extreme rainfall over North China during Typhoon Doksuri (2023)},
  journal = {Atmospheric Research},
  year = {2026},
  doi = {10.1016/j.atmosres.2026.108982},
  url = {https://doi.org/10.1016/j.atmosres.2026.108982}
}