1) neutral atmosphere model
中性大气模式
2) Mesoscale atmospheric model
中尺度大气模式
1.
In this paper,a mesoscale atmospheric model Polar MM5 used for the polar studies is introduced,and the dynamic and physical features of Polar MM5 different from those of standard MM5 are expounded.
介绍了一个用于极地研究的中尺度大气模式———Polar MM5,阐述了该模式区别于标准的中尺度大气模式MM5的动力学和物理特征。
3) Middle atmosphere models
中层大气模式
4) atmospheric model
大气模式
1.
Modeling is made during the same period using the atmospheric model MM5,with and without a frozen soil parameterization scheme.
对黑河流域上游山区水源涵养林区2003年春季土壤温度、湿度变化进行分析,运用耦合冻土参数化和没有耦合冻土参数化的大气模式MM5对该区春季过程进行了模拟,并与观测值进行对比,对模拟的产流量做了初步分析。
2.
The results show that the boundary layer scheme in atmospheric model may play an important role in simulating concentration of dust storm.
通过分析 ,作者认为大气模式中的边界层模式差异对沙尘暴中沙尘浓度的模拟能产生较大影响。
3.
The variation of infrared atmospheric transmittance based on atmospheric models in typical regions of China as a function of month is analyzed in this paper by using the combined atmospheric radiative transfer(CART) software.
利用已经建立的通用大气辐射传输软件(CART)中嵌入的我国典型地区大气模式,分析了红外波段大气透过率随月份的变化特征,并分析了用国外模式近似可能带来的误差。
5) model atmosphere
模式大气
1.
This paper discusses the effect of the atmospheric environment on two infrared channel atmospheric transmission value of different model atmosphere with LOWTRAN7 model.
利用 LOWTRAN 7大气辐射计算模式 ,对 2个红外通道分别选取不同的模式大气进行计算 ,得到了各种模式大气的大气透过率。
2.
By using the simulation results of an AGCM, which had been run from 1945 to 1993 forced by COADS SST, the interdecadal variability of the model atmosphere was investigated and compared with that of NCEP reanalysis data.
用1945～1993年的COADS SST强迫AGCM进行了连续49年的模拟积分,分析了模式大气中的年代际变化,并和NCEP再分析资料进行了比较。
3.
In the FC, effect of atmospheric internal dynamic processes on shortterm climate anomaly in the model atmosphere can be better separated.
在ＦＣ中，可以更好地分离出大气内动力过程对于模式大气短期气候异常的影响。
6) The mode of CUHK
中大模式
补充资料：中性
1.谓不表示性别。 2.化学上指既不呈酸性又不呈碱性的性质，如纯水的性质。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条