2007 IEEE Aerospace Conference 2007
DOI: 10.1109/aero.2007.353074
|View full text |Cite
|
Sign up to set email alerts
|

Technology Demonstration of Ka-band Digitally-Beam formed Radar for Ice Topography Mapping

Abstract: GLISTIN (Glacier and Land Ice Surface Topography Interferometer) is a spaceborne interferometric synthetic aperture radar for topographic mapping of ice sheets and glaciers. GLISTIN will collect ice topography measurements over a wide swath with sub-seasonal repeat intervals using a Ka-Band digitally-beamformed antenna. This paper will give an overview of the system design and key technology demonstrations including a Im x Im digitally-beamformed Ka-band waveguide slot antenna with integrated digital receivers… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
3
0

Year Published

2009
2009
2022
2022

Publication Types

Select...
3
3

Relationship

0
6

Authors

Journals

citations
Cited by 9 publications
(4 citation statements)
references
References 4 publications
0
3
0
Order By: Relevance
“…Millimetre-wave radars operate in the frequency range of 30-300 GHz (wavelengths of 1 mm to 1 cm) (Currie and Brown, 1987), although most remote-sensing studies are carried out in the low absorption 'atmospheric windows' near 35 GHz (Ka-band) and 94 GHz (W-band). While a handful of studies have mapped glacier and snow surfaces between 27 and 40 GHz (Ka-band) (Sadowy and others, 2007;Moller and others, 2011), there are no studies that have used 94 GHz (W-band) for this purpose despite the potential advantages of using higher frequency radar systems for close-range sensing of cryospheric terrain.…”
Section: Ghz Radar For Glacier Monitoringmentioning
confidence: 99%
“…Millimetre-wave radars operate in the frequency range of 30-300 GHz (wavelengths of 1 mm to 1 cm) (Currie and Brown, 1987), although most remote-sensing studies are carried out in the low absorption 'atmospheric windows' near 35 GHz (Ka-band) and 94 GHz (W-band). While a handful of studies have mapped glacier and snow surfaces between 27 and 40 GHz (Ka-band) (Sadowy and others, 2007;Moller and others, 2011), there are no studies that have used 94 GHz (W-band) for this purpose despite the potential advantages of using higher frequency radar systems for close-range sensing of cryospheric terrain.…”
Section: Ghz Radar For Glacier Monitoringmentioning
confidence: 99%
“…With different combinations of forward and reverse biased PIN diodes, the beamforming can be achieved. Compared with the ESPAR antenna described in [9], which uses six parasitic elements and six PIN diodes and which can form 2 6 = 64 patterns, the ESPAR antenna described here uses 12 parasitic elements and 12 PIN diodes and can form 2 12 = 4096 patterns. Therefore by controlling the DC voltages supplied to the PIN diodes, the beamforming can be performed.…”
Section: Antenna Design and Analysismentioning
confidence: 99%
“…By steering its main beam towards a desired signal while forming a null in the direction of an interference signal, an intelligent antenna can increase the wireless channel capacity and improve the communication quality. An intelligent antenna can be formed by an analogue beamforming array [1][2][3][4] or a digital beamforming (DBF) array [5][6][7]. These conventional intelligent antennas are bulky, expensive and have high-power consumption.…”
Section: Introductionmentioning
confidence: 99%
“…With the introduction of its successor DBSAR-2, it has been recently been upgraded to 16 channels and higher spatial resolution [9]. SweepSAR is another airborne digital beamforming SAR demonstrator of NASA [10]. It is a reflector-based 16-channel Ka-band system foreseen to simulate L-band spaceborne scenarios, such as NISAR [11] and Tandem-L [12], with a main focus on ice and solid earth topography.…”
Section: Introductionmentioning
confidence: 99%