Improved constants of the total density TD-88 model for the Earth's neutral thermosphere are calculated. The model is fully functional within the height range of 200 to 500 km, with fixed values of the mean solar flux and geomagnetic index. The control data of the atmospheric air density are derived from the aeronomical NRLMSISE-00 model which was used as the reference one. The upgraded TD-88, named TD-88Up, model is obtained by the extended LSQ method with varying all model parameters
A method to estimate the neutral atmospheric density near the ionospheric main peak of Mars is intro...
A new empirical atmospheric density model, Jacchia-Bowman 2008, is developed as an improved revision...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...
SUMMARY: Improved constants of the total density TD-88 model for the Earth’s neutral thermosphere ar...
In this paper we have examined possibilities for preserving and improving the total density model...
In this paper we have examined possibilities for preserving and improving the total density model of...
This Technical Memorandum describes the NASA Marshall Engineering Thermosphere Model-Version 2.0 (ME...
This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoD...
An atmospheric model for the height range 100–700 km, likely to hold for solar minimum conditions, h...
Aims – The Drag Temperature Model (DTM) is a semi-empirical model describing the temperature, densit...
ability to measure the surface forces present. The total density can be easily derived from this mea...
The neutral temperature, neutral densities for N2, O2, O, Ar, He and H, mean molecular weight, and t...
International audienceAims: The semi-empirical Drag Temperature Models (DTM) predict the Earth’s the...
The thermosphere is located above the mesosphere and below the exosphere, and its highly ionized sta...
Aims: The quality of the Committee on Space Research (COSPAR) International Reference Atmosphere mod...
A method to estimate the neutral atmospheric density near the ionospheric main peak of Mars is intro...
A new empirical atmospheric density model, Jacchia-Bowman 2008, is developed as an improved revision...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...
SUMMARY: Improved constants of the total density TD-88 model for the Earth’s neutral thermosphere ar...
In this paper we have examined possibilities for preserving and improving the total density model...
In this paper we have examined possibilities for preserving and improving the total density model of...
This Technical Memorandum describes the NASA Marshall Engineering Thermosphere Model-Version 2.0 (ME...
This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoD...
An atmospheric model for the height range 100–700 km, likely to hold for solar minimum conditions, h...
Aims – The Drag Temperature Model (DTM) is a semi-empirical model describing the temperature, densit...
ability to measure the surface forces present. The total density can be easily derived from this mea...
The neutral temperature, neutral densities for N2, O2, O, Ar, He and H, mean molecular weight, and t...
International audienceAims: The semi-empirical Drag Temperature Models (DTM) predict the Earth’s the...
The thermosphere is located above the mesosphere and below the exosphere, and its highly ionized sta...
Aims: The quality of the Committee on Space Research (COSPAR) International Reference Atmosphere mod...
A method to estimate the neutral atmospheric density near the ionospheric main peak of Mars is intro...
A new empirical atmospheric density model, Jacchia-Bowman 2008, is developed as an improved revision...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...