Abstract
and ocean, separately, and then merging them along the coastline without including full dynamics and physics interaction,’’ as mentioned in LZY. In this reply, we will show that their converting the flight-level (at an altitude of 2.5‐3.2 km) data with a simple, one-dimensional planetary boundary layer (PBL) model tended to introduce large errors in surface winds, while their merging, without considering a transition zone produced by horizontal momentum advection, accounts for the unrealistic sharp discontinuity. These problems could be clear
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