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1.WATER VAPOR FLUX OVER EAST AND SOUTH ASIA DURING JUNE OF 1979
1979年6月东亚和南亚上空的水汽通量收藏指正
2.The results show that before the summer monsoon onset, the air-sea heat exchange near Xisha area is weak, the vapor flux is small and the main trend is that the ocean is being heated; while after its onset, the air-sea heat exchange is balanced roughly.
结果表明：季风爆发前，西沙海气界面热量交换较弱，水汽通量较小，以海洋获得热量为主；季风爆发后，海气界面热量交换接近平衡。收藏指正
3.The zonal index and the divergence of summer water vapor transport flux over Northwest China are analysed by using NCEP/NCAR monthly mean reanalysis data from 1970 to 1997. The analysed results show that the interannual change of moisture flux divergence resulted by moisture advection is constant, but resulted by wind field convergence or divergence is unstable.
利用1970—1997年NCEP/NCAR再分析月平均资料,设计了区域西风指数。 通过分析西北地区夏季的水汽输送通量散度,发现该地区水汽平流引起的水汽输送通量散度项年际变化极小,而风场辐合(辐散)引起的水汽输送通量散度项年际变化却很大,在西北地区区域西风指数较强年份风场辐合比区域西风指数较弱年份强。收藏指正
4.Eddy covariance (EC) technique has become a standard method to measure the carbon, water vapor and energy flux in the heterogeneous area, and the energy balance closure (EBC) is an important mean to test the reliability of EC technique.
运用线性回归、能量平衡闭合率和能量不平衡标准差等方法对湍流通量与可利用能量的关系进行分析。收藏指正
5.Condensation heat transfer coefficients of R410a are lower than that of R22 at low mass flux and vapor but nearly equivalent at intermediate or more higher mass flux.
与R22相比,R410a的凝结换热系数在较低质量流率时低于R22,在中高质量流率时与R22相当。收藏指正
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