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Telecommunications and Radio Engineering
SJR: 0.202 SNIP: 0.2 CiteScore™: 0.23

ISSN Imprimer: 0040-2508
ISSN En ligne: 1943-6009

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Telecommunications and Radio Engineering

DOI: 10.1615/TelecomRadEng.v72.i18.70
pages 1719-1729

ATMOSPHERE MONITORING OVER THE KHARKIV REGION BY MEANS OF GPS

A. L. Kovorotniy
O.Ya. Usikov Institute for Radio Physics and Electronics, National Academy of Sciences of Ukraine, 12, Academician Proskura St., Kharkov 61085, Ukraine
Yu. V. Goncharenko
A. Usikov Institute of Radio Physics and Electronics, National Academy of Sciences of Ukraine, 12, Academician Proskura St., Kharkov 61085, Ukraine; Applied Physics Laboratory, University of Washington, Seattle, USA
V. N. Gorobets
O.Ya. Usikov Institute for Radio Physics and Electronics, National Academy of Sciences of Ukraine, 12, Academician Proskura St., Kharkov 61085, Ukraine
F. V. Kivva
O.Ya. Usikov Institute for Radiophysics and Electronics of the National Academy of Sciences of Ukraine, 12, Academician Proskura St., Kharkiv 61085, Ukraine
A. I. Gorb
Navigation and geodesic center, Electronics, Kharkiv 61018,f Ukraine
A. Yu. Balan
Leica Geosystems AG, Representation office in Ukraine; Navigation and geodesic center, Electronics, Kharkiv 61018,f Ukraine

RÉSUMÉ

The state of the atmosphere rating, weather and climate forecasting were actual for other areas of science and engineering. This paper deals with the development of methods for determining the tropospheric zenith delay (ZTD) from remote sensing data using GPS systems and of the experimental validation of proposed algorithm. The initial data were obtained by means of a regional system of high-precision satellite geodesic measurements in the Kharkiv region (NGCNET). Later they were used to calculate the zenith delay and weather parameters in each of the receiving points. The paper describes a technique for determining the hydrostatic and "wet" (ZWD) component of the tropospheric delay based on the data obtained by the twofrequency GPS receivers. A comparison between the data calculated from the known models, and received from NGCNET is performed. It is shown that the correlation coefficients between the values of the "wet" ingredients tropospheric delay is 0.5−0.6 for summer and 0.7−0.8 for winter and spring measurements. The correlation radii of ZWD values for different seasons are estimated in this paper.


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