Skillful Kilometer-Scale Regional Weather Forecasting via Global and Regional Coupling
Authors: Weiqi Chen, Wenwei Wang, Qilong Yuan, Lefei Shen, Bingqing Peng, Jiawei Chen, Bo Wu, Liang Sun
Organizations: DAMO Academy, Alibaba Group Hangzhou, China · Northwest Polytechnical University Xi’an, China · Zhejiang University Hangzhou, China · Institute of Atmospheric Physics, Chinese Academy of Sciences Beijing, China
Data-driven weather models have advanced global medium-range forecasting, yet high-resolution regional prediction remains challenging due to unresolved multiscale interactions between large-scale dynamics and small-scale processes such as terrain-induced circulations and coastal effects. This paper presents a global-regional coupling framework for kilometer-scale regional weather forecasting that synergistically couples a pretrained Transformer-based global model with a high-resolution regional network via a novel bidirectional coupling module, ScaleMixer. ScaleMixer dynamically identifies meteorologically critical regions through adaptive key-position sampling and enables cross-scale feature interaction through dedicated attention mechanisms. The framework produces forecasts at 0.05∘ (∼5km ) and 1-hour resolution over China, significantly outperforming operational NWP and AI baselines on both gridded reanalysis data and real-time weather station observations. It exhibits exceptional skill in capturing fine-grained phenomena such as orographic wind patterns and Foehn warming, demonstrating effective global-scale coherence with high-resolution fidelity. The code is available at https://anonymous.4open.science/r/ScaleMixer-6B66.
Figures & tables
Figure 1. Left: The Architecture of Global-Regional Weather Forecasting Model: Synoptic-scale context ( Mglobal ) drives mesoscale regional refinement ( Mregional ) via ScaleMixer, ensuring cross-scale coupling and consistency. Right: ScaleMixer Module: Bidirectional Cross-Scale Coupling via Key Position Identification and encoding. Key components include (1) key position identification, (2) coupling regional dynamics with global context via global-to-position and position-to-regional attention, and (3) global token adaptation incorporating regional features.
Variable
Latitude-weighted RMSE
Latitude-weighted ACC
IFS-HRES
Baguan
Mglobal
Mregional
OneForecast
LAM
ScaleMixer
ΔRMSE
IFS-HRES
Mglobal
Mregional
OneForecast
LAM
ScaleMixer
ΔACC
T2M
1.815
1.928
1.991
2.452
1.571
1.742
1.382
↓ 23.86%
0.862
0.881
0.845
0.897
0.901
0.921
↑ 6.84%
U10
1.934
1.956
1.967
2.631
2.251
1.889
1.644
↓ 14.99%
0.721
0.753
0.716
0.744
0.742
0.793
↑ 9.99%
V10
1.928
1.937
1.970
2.886
2.316
1.905
1.617
↓ 16.13%
0.723
0.751
0.713
0.732
0.737
0.785
↑ 8.57%
Q
0.807
0.611
0.811
1.243
0.714
0.676
0.559
↓ 30.73%
0.774
0.768
0.771
0.751
0.781
0.812
↑ 4.91%
P
13.27
22.97
10.27
4.241
2.545
2.14
1.874
↓ 85.88%
0.887
0.902
0.894
0.899
0.912
0.920
↑ 3.72%
Table 1. Average RMSE and ACC across Δt=1∼48 hours lead time regional weather hindcast at 0.05 ∘ resolution. The best results are bolded .
Figure 2. ScaleMixer demonstrates superior deterministic forecasting skill compared to IFS-HRES at 0.05° resolution. Seven surface variables (T2M, U10, V10, Q, P, TCC, and SSRD) are evaluated using latitude-weighted RMSE (lower values indicate superior performance). (a) Hindcast results show ScaleMixer outperforms IFS-HRES across all variables during 2024/10–2024/12. (b) Operational forecasts confirm ScaleMixer maintains superiority performance (2025/01–2025/04).
Figure 3. Left: Temporal evolution of 10m wind speed predictions initialized at 2024/10/30 12 UTC over the Hengduan Mountains (25.0–35.0°N, 95.0–105.0°E), China. Black arrows represent wind flow fields. ScaleMixer resolves enhanced resolution of orographic wind heterogeneity (peaking >10 m/s at crests and <2 m/s in valleys). Right: Corresponding temperature fields. Foehn effects are illustrated in the picture, characterized by 4–8°C leeward warming relative to windward slopes through adiabatic compression processes. ScaleMixer captures fine-grained temperature gradients, contrasting with IFS-HRES exhibiting spatial smoothing forecasts.
Figure 4. Station distrbution map. The station observation dataset contains 2216 weather stations across China, which record hourly observations of meteorological variables such as temperature, air pressure, and wind speed.
Variable
IFS-HRES
Baguan
ScaleMixer
ΔRMSE
T2M
3.158
3.108
1.822
↓ 41.4%
D2M
2.812
2.655
1.789
↓ 36.4%
WS10
1.401
1.402
1.329
↓ 5.10%
Table 2. Average RMSE across Δt=1∼48 hours lead time regional weather operational forecasting against weather station observations.
Model Variant
Configuration Details
T2M RMSE
U10 RMSE
ScaleMixer
Adaptive Sampling + Bidirectional
1.382
1.644
Variant A
Random Sampling + Bidirectional
1.605 (+16.1%)
1.882 (+14.5%)
Variant B
Fixed Uniform Grid + Bidirectional
1.512 (+9.4%)
1.795 (+9.2%)
Variant C
Adaptive Sampling + Unidirectional
1.468 (+6.2%)
1.721 (+4.7%)
Variant D
No Interaction (Standalone)
1.991 (+44.1%)
1.967 (+19.6%)
Table 3. Ablation study of ScaleMixer components on 48-hour forecast performance.
Metric
Regional Encoder Layers ( k )
k=2
k=4
k=8
T2M RMSE
1.485
1.382
1.379
U10 RMSE
1.752
1.644
1.641
Inference Time
22ms
28ms
51ms
Table 4. Sensitivity analysis of Regional Encoder Layers ( k ).
Appendix figures & tables16 assets
Supplementary material from the paper’s appendix.
Appendix
Module
Hyperparameter
Description
Value
Global Model Mglobal
P
Patch size of global tokens
6
d
hidden dimension
1536
M
Number of Transformer encoder layers of in the global model
24
Heads
Number of attention heads
8
MLP ratio
Expansion factor for MLP
4.
Depth of prediction head
Number of deconvolution layers of the final prediction head
2
Appendix
Table 5. Default hyperparameters of the framework.
Type
Variable Name
Abbrev.
Description
Pressure Levels
Static Variable
Land-sea mask
lsm
Binary mask distinguishing land (1) from sea (0)
N/A
Orography
oro
Height of Earth’s surface
N/A
Latitude
lat
Latitude of each grid point
N/A
Surface Variable
2 metre temperature
t2m
Temperature measured 2 meters above the surface
Single level
10 metre U wind component
u10
East-west wind speed at 10 meters above the surface
Single level
10 metre V wind component
v10
North-south wind speed at 10 meters above the surface
Single level
Appendix
Table 6. Summary of ECMWF variables utilized in the ERA5 and operational analysis dataset with 0.25 ° resolution. The variables lsm and oro are constant and invariant with time.
Type
Variable Name
Abbrev.
Description
Surface Variable
2 metre temperature
T
Temperature measured 2 meters above the surface
10 metre U wind component
U
East-west wind speed at 10 meters above the surface
10 metre V wind component
V
North-south wind speed at 10 meters above the surface
Surface specific humidity
Q
Mixing ratio of water vapor to total air mass at 2 meters above the surface
Surface pressure
P
Pressure of the atmosphere on the surface of land, sea and in-land water
Total cloud cover
TCC
Cloud occurring at different model levels through the atmosphere
Appendix
Table 7. Summary of variables utilized in CLDAS with 0.05 ° resolution.
Figure 5. 2 metre temperature forecasts over China
Figure 6. 2 metre temperature forecasts over a subregion of latitudes in [30,40] and longitudes in [95,115]
Figure 7. surface pressure forecasts over China
Figure 8. surface pressure forecasts over a subregion of latitudes in [30,40] and longitudes in [95,115]
Figure 9. 10 metre Wind speed U component forecasts over China
Figure 10. 10 metre wind speed U component forecasts over a subregion of latitudes in [16.3,26] and longitudes in [115,125]
Figure 11. 10 metre Wind speed V component forecasts over China
Figure 12. 10 metre wind speed V component forecasts over a subregion of latitudes in [16.3,26] and longitudes in [115,125]
Figure 13. surface solar radiation downwards forecasts over China
Figure 14. surface solar radiation downwards forecasts over a subregion of latitudes in [35,50] and longitudes in [115,135]
Figure 15. total cloud cover forecasts over China
Figure 16. total cloud cover forecasts over a subregion of latitudes in [35,50] and longitudes in [115,135]
Figure 17. RMSE and ACC for some key variables of various AI-based weather models on Weatherbench2
Weather forecasting predicts future atmospheric conditions, from local storms to global patterns, using physical models, observations, and machine learning.
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Guowen Li, Yang Liu, Yujie Wang +5
Tsinghua University · The Chinese University of Hong Kong · Sun Yat-Sen University +1
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