Challenges in sub-kilometer grid modeling of the convective planetary boundary layer

HIGHLIGHTS

• who: Jimy Dudhia from the It can be seen that such a term enables a vertical flux even in the absence of a local vertical gradient, and this can result in a neutral to slightly stable potential temperature profile that is more realistic as was seen in Figure The commonly used Yonsei University (YSU) PBL scheme by Hong et_al [13] adopts this method and the u0393 term is regarded as a nonlocal mixing term because it is not proportional to the local gradient such as pure diffusion schemes are. With the countergradient method, note that the same . . .
  

   

  

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