Improving the WRF model's (version 3.6.1) simulation over sea ice surface through coupling with a?complex thermodynamic sea ice model (HIGHTSI)

摘要

Sea ice plays an important role in the air–ice–ocean interaction, but it is often represented simply in many regional atmospheric models. The Noah sea ice scheme, which is the only option in the current Weather Research and Forecasting (WRF) model (versio