Climate Dynamics Group

at Chalmers University of Technology

We study the interactions between different components of the climate system to understand how they give rise to patterns and variations on timescales ranging from days to decades.

On this site you can find more information about our group, what we do, and our output in terms of publications and other related resources. Got a question? Feel free to reach out to us!

About us

We are the Climate Dynamics Group (CDG), led by Hans Chen at the Division of Geoscience and Remote Sensing within the Department of Space, Earth and Environment at Chalmers University of Technology. We are situated in the west coast city of Gothenburg, Sweden.

Photo of members of the Climate Dynamics Group.
Climate Dynamics Group members at the Swedish Climate Symposium 2024.

In our research, we use observations, numerical models, statistical methods, model–data fusion methods such as data assimilation, and machine learning approaches to study the climate system. Our focus is on the atmosphere and its connections with other Earth system components on global to regional scales and diurnal to interdecadal timescales.

Highlighted research topics

Illustration of jet streams

Atmospheric circulation

We study the atmospheric circulation and synoptic-scale teleconnections to understand both the atmosphere’s natural internal variability, as well as how climate change has affected and will affect the circulation patterns.

Data assimilation schematic

Data assimilation

Data assimilation is a class of methods that seek to optimally combine information from observations and models. We use and develop data assimilation methods, for example to estimate surface carbon fluxes.

Atmospheric river from satellite

Atmospheric rivers

Atmospheric rivers are long and narrow bands of strong water vapor transport in the atmosphere. We study atmospheric rivers with a focus on their occurrence and impact on climate in the northern high-latitudes and Arctic region.

News

Recent publications

Zhong, Z., H. W. Chen, A. Dai, T. Zhou, B. He, and B. Su, 2025: Sub-diurnal asymmetric warming has amplified atmospheric dryness since the 1980s. Nature Communications, 16, 8247, https://doi.org/10.1038/s41467-025-63672-z.

Chen, J., H. W. Chen, Z. Li, Q. Wang, G. Wang, K. Jia, X. Yan, 2025: Divergent radiative forcing of fine-mode aerosols across tree genera during wildfires in North America and Europe. Journal of Hazardous Materials, 495, 138881, https://doi.org/10.1016/j.jhazmat.2025.138881.

Liu, Y., Q. Tang, L. R. Leung, D. Chen, J. A. Francis, C. Zhang, H. W. Chen, and S. C. Sherwood, 2025: Changes in atmospheric circulation amplify extreme snowfall fueled by Arctic sea ice loss over high-latitude land. Weather and Climate Extremes, https://doi.org/10.1016/j.wace.2025.100802.

Zhong, Z., H. W. Chen, B. He, and B. Su, 2025: Contrasting vegetation productivity responses in arid and humid zones to recent changes in diurnal temperature range. The Innovation Geoscience, 3, 100163, https://doi.org/10.59717/j.xinn-geo.2025.100163.

Zou, J., H. W. Chen, H. Li, Q. Wang, G. Wang, K. Jia, Z. Chen, C. Zhao, W. Shi, Y. Yang, Y. Tang, J. Chen, Y. Zhang, T. Xu, Y. Wang, G. Liu, and X. Yan, 2025: Amplified urban heat island effect in southern China’s old towns following atmospheric regulation policies. Sustainable Cities and Society, 131, 106675, https://doi.org/10.1016/j.scs.2025.106675.