On the basis of the ideal of local scale similarity theory, the profile equations of wind, temperature and humidity for the eonvective marine boundary layer have been obtained. The marine boundary layer measurements w...On the basis of the ideal of local scale similarity theory, the profile equations of wind, temperature and humidity for the eonvective marine boundary layer have been obtained. The marine boundary layer measurements were made over the western Pacific Ocean as past of the Tropical Ocean and Global Atmosphere (TOGA) Programme during Nov. 1986-Feb. 1987. The similarity profiles predicledfor wind. temperature and humidity in the MBL are in good agreement with the observational data.展开更多
In the present study the data of wind and temperature profiles and sensible heat flux observed in Beijing in July and December of 1986,together with the results of water tank experiments for comparison,are used to tes...In the present study the data of wind and temperature profiles and sensible heat flux observed in Beijing in July and December of 1986,together with the results of water tank experiments for comparison,are used to test the prediction models of the atmospheric mixed layer with zero order and first order assumption,respectively. The results show that the entrainment rates in summer and winter used in the zero order model are 0.15 and 0.10,respectively,while its value in the first order model ranges between 0.15 and 0.19 with a lower rate at the initial stage of mixed layer development. Emphasis in the study is also placed on the relationship between the entrainmert rate and the development of the mixed layer.展开更多
文摘On the basis of the ideal of local scale similarity theory, the profile equations of wind, temperature and humidity for the eonvective marine boundary layer have been obtained. The marine boundary layer measurements were made over the western Pacific Ocean as past of the Tropical Ocean and Global Atmosphere (TOGA) Programme during Nov. 1986-Feb. 1987. The similarity profiles predicledfor wind. temperature and humidity in the MBL are in good agreement with the observational data.
文摘In the present study the data of wind and temperature profiles and sensible heat flux observed in Beijing in July and December of 1986,together with the results of water tank experiments for comparison,are used to test the prediction models of the atmospheric mixed layer with zero order and first order assumption,respectively. The results show that the entrainment rates in summer and winter used in the zero order model are 0.15 and 0.10,respectively,while its value in the first order model ranges between 0.15 and 0.19 with a lower rate at the initial stage of mixed layer development. Emphasis in the study is also placed on the relationship between the entrainmert rate and the development of the mixed layer.
