The clm was originally developed by dr . dai yongjiu on the basis of the bats 26 , ncar lsm 27 , and iap94 28 , which have been already adopted by the ncar ccsm 29 . the clm mainly represents inter - actions between the atmosphere , vegetation and land , and reflects the change of the water , heat state and the transfers of heat and water . soil moisture in this model is predicted from a ten - layer model fixed depth Clm是由戴永久博士在bats 27模式ncar lsm 28 , iap94 29的基礎(chǔ)之上開發(fā)出并為美國(guó)國(guó)家大氣研究中心的氣候系統(tǒng)模式ncar ccsm所采用的陸面模型30 . clm模式主要考慮慮了大氣植被土壤之間的物質(zhì)交換過(guò)程,反映土壤植被大氣中水熱狀態(tài)變化和水熱傳輸