An experimental wind wave monitoring station has been set up on the eastern coast of Middle Baikal. Tests were carried out by direct measurements using a video recorder installed on a measuring pole near the coastline. The characteristics of the wind were measured synchronously with an anemometer. In the conditions of open Baikal in shallow water in the daytime, the dependence of the height of the waves on the speed and direction of the wind has been established. In the morning, with an increase in the wind speed of the southwestern direction, the generation of wind waves begins. The maximum height of the waves in the second half of the day with the western wind direction is established. The measurements were taken in autumn.
This paper presents the results of synchronous observations of the ozone concentration and meteorological parameters obtained using an automated system for measuring the characteristics of gaseous impurities and the AMK-02 meteorological complex in the near-air layer of the atmosphere on the southeastern coast of Lake Baikal. The vertical ozone fluxes in the friction layer h = 3 m above the water surface were estimated during the summer period (July- August). Estimation of the rate of dry ozone deposition showed that, in the region of high wind velocity gradients in the friction layer, its distribution depends on the wave parameters and varies over a wide range.
Access to the requested content is limited to institutions that have purchased or subscribe to SPIE eBooks.
You are receiving this notice because your organization may not have SPIE eBooks access.*
*Shibboleth/Open Athens users─please
sign in
to access your institution's subscriptions.
To obtain this item, you may purchase the complete book in print or electronic format on
SPIE.org.
INSTITUTIONAL Select your institution to access the SPIE Digital Library.
PERSONAL Sign in with your SPIE account to access your personal subscriptions or to use specific features such as save to my library, sign up for alerts, save searches, etc.