Abstract
The spatiotemporal variability of temperature in the atmospheric boundary layer has been studied comparatively in the city of Tomsk (Russia) and in the coastal zones of Lake Baikal (Russia) and Lake Issyk-Kul (Kirghizia). Measurements with the MTP-5 temperature profiler have demonstrated that in the summer season the conditions of thermal stratification of the lower 1-km atmospheric layer under urban conditions in the absence of large water reservoirs nearby and in the mountain areas on the coasts of big lakes differ widely. The types of stratification and parameters of the atmospheric boundary layer in the regions under study are determined.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
