In different synoptic conditions and at different time scales,the analysis of the energy budgets by Bowen Ratio Method and Bulk Schemes over Huaihe River Basin during the field observation periods of HUBEX in 1999 sho...In different synoptic conditions and at different time scales,the analysis of the energy budgets by Bowen Ratio Method and Bulk Schemes over Huaihe River Basin during the field observation periods of HUBEX in 1999 shows that,(1)the averaged latent heat flux is an order of magnitude more than the averaged sensible heat flux during the observation period:(2)the variation of total cloud amount is out of phase with the terms of energy budgets except for the downward longwave radiation which maybe is related to the cloud's height and class:(3)the values of sensible and latent heat fluxes are small during rain episodes,but thereafter,the values become high and then up to maximum.It is similar to the other terms of the energy budgets except for the downward longwave radiation.The diurnal variation of energy budgets indicates that the daytime precipitation exerts great influence to the energy budgets,but the nighttime precipitation makes little influence; (4)the variation of the latent heat flux is in phase with the evaporation,which indicates that the latent heat flux calculated by bulk schemes is reliable:(5)the means of the sensible and latent heat flux and momentum flux by bulk schemes for the time period from May to August are, respectively,30.71W/m^2.116.81W/m^2.2.86×10^(-2)N/m^2 in 1998 and 30.28W/m^2,107.35 W/m^2,2.74×10^(-2)N/m^2 in 1999.The values of these two years are similar.During summer in 1999 the magnitude and activity of sensible heat flux are strongest in June and those of the latent heat flux are in August.展开更多
基金the National Natural Science Foundation of China(No.49794030).
文摘In different synoptic conditions and at different time scales,the analysis of the energy budgets by Bowen Ratio Method and Bulk Schemes over Huaihe River Basin during the field observation periods of HUBEX in 1999 shows that,(1)the averaged latent heat flux is an order of magnitude more than the averaged sensible heat flux during the observation period:(2)the variation of total cloud amount is out of phase with the terms of energy budgets except for the downward longwave radiation which maybe is related to the cloud's height and class:(3)the values of sensible and latent heat fluxes are small during rain episodes,but thereafter,the values become high and then up to maximum.It is similar to the other terms of the energy budgets except for the downward longwave radiation.The diurnal variation of energy budgets indicates that the daytime precipitation exerts great influence to the energy budgets,but the nighttime precipitation makes little influence; (4)the variation of the latent heat flux is in phase with the evaporation,which indicates that the latent heat flux calculated by bulk schemes is reliable:(5)the means of the sensible and latent heat flux and momentum flux by bulk schemes for the time period from May to August are, respectively,30.71W/m^2.116.81W/m^2.2.86×10^(-2)N/m^2 in 1998 and 30.28W/m^2,107.35 W/m^2,2.74×10^(-2)N/m^2 in 1999.The values of these two years are similar.During summer in 1999 the magnitude and activity of sensible heat flux are strongest in June and those of the latent heat flux are in August.
