The phrase "atmosphere model" is correct and usable in written English.
It can be used in contexts related to science, particularly in meteorology, climate science, or physics, to describe a representation of the atmosphere's behavior or characteristics.
Example: "The researchers developed an advanced atmosphere model to predict weather patterns more accurately."
Alternatives: "climate model" or "weather model".
The components of Community Climate System Model (CCSM) include an atmospheric model (Community Atmosphere Model), a land-surface model (Community Land Model), an ocean model (Parallel Ocean Program), and a sea ice model (Community Sea Ice Model).
Parameterization schemes of atmospheric normal modes (NMs) and orographic gravity waves (OGWs) have been implemented into the mechanistic Middle and Upper Atmosphere Model (MUAM) simulating atmospheric general circulation.
The neutral atmosphere model covers the entire atmospheric region from the surface up to the top of the thermosphere, which is about 500 km altitude.
Not only fine horizontal resolution but also improvements in the atmospheric physics used in the atmosphere model will be required to improve the typhoon predictions.
Here we investigate Earth's energy imbalance over the period since 1960 in observations, atmospheric models forced by observed sea surface temperatures and radiative changes (Atmosphere Model Intercomparison Project, AMIP), and fully coupled model simulations (Coupled Model Intercomparison Project, CMIP5).
First, a two-dimensional soil-atmosphere model required two input categories, namely: soil properties and atmospheric parameters.
The model outputs were in the form of soil suction (kPa) and vertical deformation (mm) for the soil-atmosphere model and the soil-deformation model, respectively.
This included a coupled soil-atmosphere model for seepage through the soil that generated suction data and suction-based displacement model that takes into account the effect of overburden soil pressure.
The reference temperature of Standard Atmosphere model at stratospheric altitudes is about −56 °C.
Figure 5 shows average temperature by Standard Atmosphere model and average temperature at different latitudes by CIRA Model. Figure 6 shows the temperature variation around the operative altitude.
