,thermal conduction algorithm combined with mathematical fitting method and thermal conduction-convection algorithm) in order to better understand the physical property and procedures of the soil over the Loess Plateau quantitatively and to form a basis of improvements of soil temperature diagnosis in land surface models.
10 m深度的土壤层温度,结果表明:由于忽略土壤的垂直不均匀性和水分的垂直运动而只考虑热传导过程,热传导方法不仅高估了土壤温度振幅,而且高估了位相的延迟。
,thermal conduction algorithm combined with mathematical fitting method and thermal conduction-convection algorithm) in order to better understand the physical property and procedures of the soil over the Loess Plateau quantitatively and to form a basis of improvements of soil temperature diagnosis in land surface models.
本文还利用热传导-对流方法计算0。
