4.6 Article

WRF-based dynamical downscaling ofERA5reanalysis data for High Mountain Asia: Towards a new version of the High Asia Refined analysis

期刊

INTERNATIONAL JOURNAL OF CLIMATOLOGY
卷 41, 期 1, 页码 743-762

出版社

WILEY
DOI: 10.1002/joc.6686

关键词

cold bias; dynamical downscaling; ERA5; HAR; High Mountain Asia; snow depth; WRF

资金

  1. German Federal Ministry of Education and Research (BMBF) [FKZ 03G0878G]
  2. TU Berlin

向作者/读者索取更多资源

The study aims to improve the performance of the new version (HAR v2) of High Asia Refined analysis (HAR) by optimizing settings and correcting data, achieving better accuracy and results closer to actual observations.
The High Asia Refined analysis (HAR) is a regional atmospheric data set generated by dynamical downscaling of the Final operational global analysis (FNL) using the Weather Research and Forecasting (WRF) model. It has been successfully and widely utilized. A new version (HAR v2) with longer temporal coverage and extended domains is currently under development. ERA5 reanalysis data is used as forcing data. This study aims to find the optimal set-up for the production of the HAR v2 to provide similar or even better accuracy as the HAR. First, we conducted a sensitivity study, in which different cumulus, microphysics, planetary boundary layer, and land surface model schemes were compared and validated against in situ observations. The technique for order preference by similarity to the ideal solution (TOPSIS) method was applied to identify the best schemes. Snow depth in ERA5 is overestimated in High Mountain Asia (HMA) and causes a cold bias in the WRF output. Therefore, we used Japanese 55-year Reanalysis (JRA-55) to correct snow depth initialized from ERA5 based on the linear scaling approach. After applying the best schemes identified by the TOPSIS method and correcting the initial snow depth, the model performance improves. Finally, we applied the improved set-up for the HAR v2 and computed a one-year run for 2011. Compared to the HAR, the HAR v2 has a better representation of air temperature at 2 m. It produces slightly higher precipitation amounts, but the spatial distribution of seasonal mean precipitation is closer to observations.

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