Page Content
Assessment of Snow and Ice Reflections with In-Situ data
- View from setup location, with GNSS antennas in the lower part, to the inner Kongsfjorden in north-eastern direction.
[1]
- © L. Peraza (GFZ)
A GNSS station with a reflectometry receiver was set
up at Kongsfjorden (Spitsbergen), 78°54’14’’N,
11°52’37’’E, 512m above ellipsoid (WGS-84). This permanent
station is operated by GFZ in collaboration with NPI (Norwegian Polar
Institute) at the Zeppelin mountain outpost. It accumulates a data set
since summer 2013 observing reflections over the fjord and the
adjacent land surface. Especially the changing surface types: the
fjord, adjacent glaciers and the variable snow-cover over land are of
interest to investigate GNSS reflectometry applications.
The setup contains a GORS (GNSS Occultation Reflectometry
Scatterometry) four-frontend receiver, which is based on commercial
JAVAD hardware. The receiver is connected to an uplooking antenna and
two further antennas tilted towards the horizon. The tilted antennas
have right-handed and left-handed circular polarization, respectively.
The antenna mount is installed approximately 476m above mean sea level
with an extensive view over Kongsfjorden.
Reflections are observed at low transmitter elevation
angles (between 10° and 2°) over Kongsfjorden and adjacent land
areas. A topography adapted reflection model, which considers sloped
surface facets, has been developed and presented [1]. It incorporates
a digital elevation model, provided by NPI. The relative Doppler shift
(reflected to direct signal) is computed for each facet.
Challenges in data processing persist due to drifts in
GNSS satellite orbit. Reflection points at large distances are,
therefore, variable even though the satellite recur after a sidereal
day. The long-term objective is to map the signal-to-noise ratio (SNR)
of the more than 50 recurring reflection events for a 3-year period.
The influence of surface roughness and liquid water content on SNR
shall be examined for soil, snow- or ice-covered surfaces. The 2014
data set of SNR over the fjord has been analysed already in a master
thesis [2].
References:
[1] Semmling, M.; Peraza, L.; Falck, C.; Gerland, S. &
Wickert, J.: Doppler shift estimation for GNSS reflectometry using a
land topography adapted reflection model. Geophysical Research
Abstracts, EGU General Assembly, 2016, Vol. 18, EGU2016-17139
[2] Peraza, L.: Signal Power Analysis of GNSS Reflections
recorded at Kongsfjorden, Spitsbergen. Technical University Berlin,
2016
Im Original geändert:
.jpg