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document title / titre du document TRP W ORK PLAN ... - emits - ESA

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<strong>TRP</strong> Work Plan 2005-2007<br />

Description of Activities<br />

TEC-SB/7935/dc<br />

12/Feb/09<br />

<strong>TRP</strong> Reference:<br />

Title:<br />

T102-44ET<br />

Research into GPS Sea-Ice and Dry Snow Reflectometry<br />

Sea-Ice applications:<br />

Reflected GPS signals obtained over sea-ice <strong>du</strong>ring airborne campaigns and via the UK-DMC satellite suggest that phase<br />

coherency can be maintained for some time allowing accurate altimetry to be performed. UK-DMC data however, suffers from<br />

poor datation and relatively low SNR whereas airborne data is limited, expensive to acquire and provides only a snapshot of<br />

ice conditions. In order to investigate fully the potential for GNSS Reflectometry to derive sea-ice parameters including<br />

freeboard a longer term alternative needs to be found. This could be in the form of mounting up and down looking GPS<br />

antennas at a suitable location overlooking sea-ice e.g. Zeppelin Mountain on Svalbard, and then collecting and analysing<br />

data over a protracted period, say 6 months. The resultant dataset would be invaluable in determining the ability of GNSS-R<br />

techniques to retrieve sea-ice parameters.<br />

Dry-snow applications:<br />

Dome Concordia in Antarctica is currently being investigated for its suitability as a calibration site for SMOS. The extremely<br />

dry snow with minimal precipitation each year, make it very attractive for this purpose. To test this a radiometer has been<br />

mounted on a tower at Dome C. Research into GPS Reflectometry over land has shown that provided the moisture content<br />

does not change then the forward scattering of GPS signals correlates extremely well over the same ground-track on different<br />

days. Since L-band penetrates many metres into dry snow, by mounting a down-looking GPS on the same tower at Dome C,<br />

a dataset could be built up over time showing L-band forward scattering as a function of incidence angle at this location. This<br />

would be of great interest to scientists and add insight into the radiometer retrieved signal. In addition, if both L1 and L2<br />

reflections could be captured then high accuracy TEC maps could be generated for the area.<br />

Deliverables:<br />

Long-term GPS-R dataset collected from a fixed position over sea-ice. Data analysis for altimetric purposes and ice<br />

properties.<br />

Dataset of L-band forward scattering as a function of incidence angle over the SMOS calibration site Dome C, Antarctica. High<br />

resolution TEC maps for the sky above Dome C.<br />

Current TRL: TRL2 Target TRL: TRL3 Application Need/Date: TRL5 by 2010<br />

Future altimeter/ice mission, SMOS /<br />

Application/Mission: Contract Duration: 18 months<br />

SMOS ops<br />

SW Clause : - Dossier0 Ref.:<br />

Consistency with Harmonisation<br />

N/A<br />

Roadmap and Conclusions:<br />

Page 12 of 227

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