LiDAR is effective tool for environment monitoring especially when for express analysis of atmosphere constituents such as aerosols, gas mixtures etc. Multi-wavelength raman lidar of IACP FEB RAS operates on thee wavelength Nd:YAG laser allows retrieving full set of optical and microphysical properties of atmosphere aerosols. This paper presents the results of using our lidar to retrieve atmospheric aerosol parameters in the vicinity of Vladivostok.
The paper presents an analysis of the results of the photometric sensing of atmospheric aerosols in the vicinity of Vladivostok for the period from 2010 to 2015. We consider the seasonal and interannual course of the optical characteristics. The results are compared with the data of satellite remote sensing and measurement on AERONET station (Ussuriisk).
The analysis of results of aerosol microphysical properties measurements (particlulate size distribution function, number and mass concentrations, of aerosol and black carbon) in the lowermost part of atmosphere of Primorskii krai for the period of 2010-2015 are presented. In paper we analyse seasonal, interannual and diurnial variations of aerosol properties.
The paper deals with surface slicks, their nature and the reasons of formation in the context of remote detection and investigation of dynamic processes in the ocean, as well as at the ocean-atmosphere system. We introduce a simple formalism of formation of contrasts between slick and free sea surface, which takes into account water leaving radiance and qualitatively explains the results of field measurements. The paper gives the results of experimental studies on the registration of slick spots on the surface of coastal waters. Together with the proposed simplified formalism we provide optimal conditions for registration of contrasts between the slick and the free sea surface: the measurement of contrast of P component of the reflected radiation should be taken at angles close to the horizon.
Atmosphere responses for more than 90% of all radiation measured by satellite. Due to this, atmospheric correction plays an important role in separating water leaving radiance from the signal, evaluating concentration of various water pigments (chlorophyll-A, DOM, CDOM, etc). The elimination of atmospheric intrinsic radiance from remote sensing signal referred to as atmospheric correction.
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.