摘要
首先利用“中国西北干旱区陆 气相互作用试验”2 0 0 0年 5～ 6月在甘肃敦煌进行的陆 气相互作用野外试验的观测资料 ,确定了西北干旱区荒漠戈壁的陆面过程参数 ,并用这些参数改进了已有的陆面过程模式。然后用该陆面过程模式对敦煌陆 气相互作用野外试验荒漠戈壁上的大气感热通量、潜热通量、摩擦速度以及净辐射、地表和土壤温度、土壤水份等重要陆面变量进行了模拟 ,结果表明 ,模拟值与观测值非常接近 。
In this paper, the parameters of the land-surface process over Gobi in arid region of Northwest China are ascertained firstly by utilizing the field observation data of “ Land-Atmosphere Interaction Experiment over Arid Region of Northwest China” in Dunhuang of Gansu Province from May to June of 2000.For example, the soil thermal capacity mean is (1.12±0.27)×10 6 J/(m 3·K), the soil thermal conductivity mean is 0.274±0.017 W/(m·K), the soil thermal diffusivity mean is (2.52±0.63)×10 -7 m 2/s. The results are smaller than those got in HEIFE. The surface roughness length is 0.0019 m. The atmospheric transparent coefficient mean is 0.61 which is smaller than that in the wet region. And the parameterized formula of the atmospheric transparent coefficient is got over the desert and Gobi affected by the sand weather. With these parameters the land-surface process model is advanced. Then, the numerical simulations of the sensible heat,the latent heat,the friction velocity,the net radiation,the surface and soil temperatures and the soil moisture over Gobi in the field experiment are done. The correlation coefficients between the simulation results and the observations for the sensible heat flux, the latent heat flux and the friction velocity are 0.95,0.58 and 0.64 respectively. The net radiation maximum is close to 500 W/m 2. The results show that the simulation and the real observation are very close and the advanced model has strong simulative ability for the land-surface process over arid region.
出处
《气象学报》
CAS
CSCD
北大核心
2003年第2期219-225,共7页
Acta Meteorologica Sinica
基金
国家自然科学基金项目 (编号 40 175 0 0 4)
国家重点基础研究发展规化项目"我国重大气候和天气灾害形成机理和预测理论的研究"(编号G19980 40 90 4-2 )
