Preprint Article Version 1 Preserved in Portico This version is not peer-reviewed

A Temporal Downscaling Model for Gridded Geophysical Data with Enhanced Residual U-Net

Version 1 : Received: 18 September 2023 / Approved: 20 September 2023 / Online: 21 September 2023 (08:36:54 CEST)

A peer-reviewed article of this Preprint also exists.

Wang, L.; Li, Q.; Peng, X.; Lv, Q. A Temporal Downscaling Model for Gridded Geophysical Data with Enhanced Residual U-Net. Remote Sensing 2024, 16, 442, doi:10.3390/rs16030442. Wang, L.; Li, Q.; Peng, X.; Lv, Q. A Temporal Downscaling Model for Gridded Geophysical Data with Enhanced Residual U-Net. Remote Sensing 2024, 16, 442, doi:10.3390/rs16030442.

Abstract

Temporal downscaling of gridded geophysical data is essential for improving climate models, weather forecasting, and environmental assessments. However, existing methods often could not accurately capture multi-scale temporal features, affecting their accuracy and reliability. To address this issue, we introduce an Enhanced Residual U-Net architecture for temporal downscaling. The architecture, which incorporates residual blocks, allows for deeper network structures without the risk of overfitting or vanishing gradients, thus capturing more complex temporal dependencies. The U-Net design inherently could capture multi-scale features, making it ideal for simulating various temporal dynamics. Moreover, we implement a flow regularization technique with advection loss to ensure that the model adheres to physical laws governing geophysical fields. Our experimental results across various variables within the ERA5 dataset demonstrate an improvement in downscaling accuracy, outperforming other methods.

Keywords

temporal downscaling; U-Net; flow regularization; residual blocks; ERA5

Subject

Environmental and Earth Sciences, Atmospheric Science and Meteorology

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