Zobrazeno 1 - 10
of 49
pro vyhledávání: '"G. G. Shchukin"'
Publikováno v:
Russian Meteorology and Hydrology. 47:946-952
Autor:
V. Yu. Zhukov, G. G. Shchukin
Publikováno v:
Russian Meteorology and Hydrology. 47:909-914
Publikováno v:
Russian Meteorology and Hydrology. 47:976-981
Publikováno v:
Russian Meteorology and Hydrology. 47:962-968
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783031190117
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb9a10b12506fe34fce75cb22a6ebb3e
https://doi.org/10.1007/978-3-031-19012-4_12
https://doi.org/10.1007/978-3-031-19012-4_12
Publikováno v:
Russian Meteorology and Hydrology. 46:345-350
Modern weather radars have difficulties in detecting wind-related weather hazards (wind shear, microburst, tornado, etc.). For this purpose, the authors propose a method based on using a new parameter: bandwidth-duration product (hereinafter, the bas
Publikováno v:
Russian Meteorology and Hydrology. 45:876-880
Weather hazards caused by the vertical air movement are considered. It is stated that the only effective mean for their detection is the weather radar. The methods used for this purpose in modern radiolocation are listed, and the difficulties encount
Publikováno v:
Cosmic Research. 58:365-371
Ground-truth experiments are needed to calibrate and validate satellite microwave data and to improve the quality and utilization efficiency of satellite data in solving problems of hydrometeorological support. This paper considers the arrangement of
Publikováno v:
Measurement Techniques. 63:301-307
It is shown that for microwave radiometric systems for remote sensing of natural environments, the issue of unambiguous determination of the correspondence of the output signal to the value of the radio brightness temperature of the probed region, fr
Publikováno v:
HYDROMETEOROLOGY AND ECOLOGY. PROCEEDINGS OF THE RUSSIAN STATE HYDROMETEOROLOGICAL UNIVERSITY. :9-19
The article deals in detail with the case of observation of a cloud array characterized by a large (15 km) height of the upper boundary of cloud cover and the presence of areas with radar reflectivity of more than 60 dBZ by the DMRL-S meteorological