тропосферна затримка

The purpose of this work is to build 3D models of components of zenith tropospheric delay (ZTD) according to the surface measurements of meteorological values obtained at 100 points, which is almost evenly distributed throughout Ukraine. Method. Saastamoinen formulas calculated dry and wet components of the zenith tropospheric delay. According to the obtained results, the fields of dry and wet components of tropospheric delay were compiled, the fields of their change were constructed using a different number of studied points.

The aim of this work is to study the fluctuations of the components of the zenith tropospheric delay during the annual period according to the ground meteorological measurements in Ukraine. Methodolodgy. The surface values of meteorological values at the stations: Lviv, Kyiv, Kharkiv and Odesa, obtained in 2019 with an interval of 3 hours were used for the research. A total amount of 2020 measurements at each of the stations has been presented.

The aim of this work is the research of the magnitude of the components change of the zenith tropospheric delay for the territory of Ukraine according to several-day terrestrial meteorological measurements, as well as the construction and study of the field of their change.  Method. The accuracy of the determination of the tropospheric delay and its components depends on the amount of meteorological data that can be used for its caclulation.

An algorithm for constructing isosurfaces tropospheric delays in the real-time monitoring.

The aim.  The aim of the research in this paper is to determine the components of zenith tropospheric delay for different stations in Ukraine and comparing them with each other. Method. When determination the tropospheric delay it is obtained as a sum of dry and wet components. Calculations of components of zenith troposphere delay were implemented by integral method using data upper-air sounding of atmosphere.