analysis of lidar receiver saturation zone versus atmosphere and lidar parameters in uv spectral band

Clicks: 180
ID: 185994
2016
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Popular

Ranked #397 of 442 articles by views in BMJ open

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 442 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract

One of the problems of location and remote sensing laser systems is the overload of photoreceiver because of the intensive clutter from the backscatter (towards the lidar) signal in the lidar “near zone. The intensive clutter arises from elastic scattering of laser radiation by aerosol particles, which are always available in the earth's atmosphere.

To solve this problem the long-range high-speed laser systems use mechanical shutters to disable physically a receiving optical channel for a time of the possible arrival of the backscatter signal from the "near zone". The easiest way to solve the problem of the photo-receiver overload in the "near zone" here is to use a biaxial circuit of location where a laser beam comes in sight of photo-receiver only within a certain predetermined range. This location circuit allows us to reduce the intensity of the atmospheric aerosol-based radiation scattered in the lidar "near zone" and avoid the clutter of the photo-receiver.

The size of the lidar clutter zone can be estimated by comparing a detected signal, caused by scattering the atmospheric aerosol laser pulse of lidar, with a maximum output current of the photo-receiver.

The clutter zone (and its size) depends on many factors, namely: factors that are directly or indirectly dependent on the wavelength of the radiation (atmospheric factors, i.e. index of attenuation and scattering of the atmosphere, scattering indicatrix, radiation energy of the laser pulse, the photo-receiver parameters - spectral sensitivity, gain, maximum output current, etc.) as well as geometric factors (distance between the optical axes of the source and the receiver, divergence of laser radiation, fields in sight of photo-receiver, size of transmitting aperture and receiving lens).

The calculation results of UV and visible spectral bands show that with a small base, depending on the photomultiplier (PMT) parameters (gain, maximum anode current) and the atmosphere parameters, conditions for arising clutter zone of lidar photo-receiver may be implemented or not. In the more transparent atmosphere at a lower PMT gain and a higher value of the PMT maximum anode current the sizes of the clutter zone are less (or it is absent). At a wavelength of 0.355 μ the size of the clutter zone is mostly more than at the wavelength of 0.532 μ.

With increasing base between the optical axes of the source and receiver the clutter zone is reduced, and the results of calculations enable selecting a base value to ensure a lack of the clutter zone in a certain range of parameter values of the PMT and the Earth's atmosphere.

Reference Key
filimonov2016naukaanalysis Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;P. A. Filimonov;M. L. Belov;V. A. Gorodnichev;S. E. Ivanov
Journal BMJ open
Year 2016
DOI
10.7463/0316.0835419
URL
Keywords

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.