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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Calla, O P N | - |
| dc.contributor.author | Bohra, Dinesh | - |
| dc.date.accessioned | 2014-05-12T10:54:01Z | - |
| dc.date.available | 2014-05-12T10:54:01Z | - |
| dc.date.issued | 2014-04 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://hdl.handle.net/123456789/28797 | - |
| dc.description | 178-185 | en_US |
| dc.description.abstract | The thrust of this study is to analyse the
effect of scattering of electromagnetic waves on microwave links and tracking
of low flying objects in the presence of strong ground bounce return from water
bound areas. For this purpose, a ground
based bi-static forward scatterometer has been used to generate co-polarized
specular data at CJ, X, and Ku bands. The measurements are carried out
on three types of water surfaces, i.e. tap water, natural lake water and saline
water. All the three water surfaces are assumed to be slightly rough surfaces
at the frequency of interest. Therefore, small perturbation model of slightly
rough surface for forward scattering is a good selection to analyse data. The
scattered microwave power from the terrain measured for 25° - 70° scattering
angle ( s) with an interval of 5° in specular direction with transmitting antenna placed at an
incidence angle ( i)
of 45° from nadir illuminates the terrain keeping i = s = 0° at 5.825, 9.472 and 13.4 GHz
in CJ, X and KU bands, respectively for vv
and hh polarization with different
antenna heights. The forward scattering coefficient computed with the help of experimental
geometry parameters, which then compared with estimated value of scattering
coefficient obtained from small
perturbation model of slightly rough surface. A good agreement between observed and estimated scattering coefficient
for horizontal (hh) and vertical (vv) polarization has been found
in
X and KU bands with a polarization reversal in CJ band. It is also observed
that dissolved salt or impurities increase the value of scattering coefficient.
The basic purpose of this study is to map and monitor
the natural resources and to provide timely inputs for the planners to develop
appropriate strategies for optimum utilisation of the resources.
| en_US |
| dc.language.iso | en_US | en_US |
| dc.publisher | NISCAIR-CSIR, India | en_US |
| dc.relation.ispartof | 78.20.Ci; 92.40.Qk | en_US |
| dc.rights | CC Attribution-Noncommercial-No Derivative Works 2.5 India | en_US |
| dc.source | IJRSP Vol.43(2) [April 2014] | en_US |
| dc.subject | Forward scattering coefficient | en_US |
| dc.subject | Water resources | en_US |
| dc.subject | Dielectric coefficient | en_US |
| dc.title | Measurement of forward scattering coefficient of different water bodies at different frequencies | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.43(2) [April 2014] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 43(2) 178-185.pdf | 242.61 kB | Adobe PDF | View/Open |
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s) with an interval of 5° in specular direction with transmitting antenna placed at an
incidence angle (
i =