Abstract
With the continuous improvement of Global Navigation Satellite System (GNSS) theory, the signal-to-noise ratio (SNR) of a GNSS reflectometry signal can be applied to detect snow depth. However, there are still some issues, such as insufficient observation data, low detection precision, etc. To solve the above problems, this paper uses the SNR reflectometry data of GLONASS L1 and L2 to detect snow depth in Yellowknife, Canada, from July 2015 to June 2016. Then we analyzed the L1 and L2 SNR-derived snow depths and the average snow depths. The results show that snow depth detected using the two SNR signals can reach centimeter level. There is weak bias and strong correlation when comparing the detected snow depth based on which single-frequency SNR observations with in situ measurements are used. For L1 and L2 SNR-derived snow depths in a separate 365-day campaign, the former bias is superior to the latter. Both RMSE values are 4.5 and 2.6 cm. The stability of L2 SNR-derived snow depth was improved by over 40% than that of L1 SNR. The average snow depths detected using the two SNR signals have no significant improvement on the precision, but improve the spatial resolution because of more satellites. The experimental results show that the applications of GNSS technology can be further extended by GLONASS-MR technology based on L2 reflectometry signals.
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References
Frei A et al (2012) A review of global satellite-derived snow products. Adv Space Res 50(8):1007–1029
Gleason S (2010) Towards sea ice remote sensing with space detected gps signals: demonstration of technical feasibility and initial consistency check using low resolution sea ice information. In: AGU Fall Meeting, 2010
Solomon S (2013) Climate Change 2007: the physical science basis: contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change, 2013, pp 159–254
Wang X, Zhang Q, Zhang S (2017) Water levels measured with SNR using wavelet decomposition and Lomb-Scargle periodogram. GPS Solut 22(1):22
Jin S, Qian X, Wu X (2017) Sea level change from BeiDou navigation satellite system-reflectometry (BDS-R): first results and evaluation. Glob Planet Change 149:20–25
Yu K (2016) Weak tsunami detection using GNSS-R-based sea surface height measurement. IEEE Trans Geosci Remote Sens 54(3):1363–1375
Zhu Y et al (2017) Sea ice detection based on differential Delay-Doppler maps from UK TechDemoSat-1. Sensors 17(7):1614
Yan Q, Huang W, Moloney C (2017) Neural networks based sea ice detection and concentration retrieval from GNSS-R Delay-Doppler maps. IEEE J Sel Top Appl Earth Obs Remote Sens 10(8):3789–3798
Strandberg J, Hobiger T, Haas R (2017) Coastal sea ice detection using ground-based GNSS-R. IEEE Geosci Remote Sens Lett 99:1–5
Jing C et al (2016) Retrieval of sea surface winds under hurricane conditions from GNSS-R observations. Acta Oceanol Sin 35(9):91–97
Zhou X (2012) Simulation techniques of GNSS-R sea surface wind field retrieval from airborne remote sensing. J Remote Sens 16(1):143–153
Yan S et al (2017) Feasibility of using signal strength indicator data to estimate soil moisture based on GNSS interference signal analysis. Remote Sens Lett 9(1):61–70
Wan W et al (2015) Initial results of China’s GNSS-R airborne campaign: soil moisture retrievals. Sci Bull 60(10):964–971
Larson KM et al (2009) Can we measure snow depth with GPS receivers? Geophys Res Lett 36(17):L17502
Fabra F et al (2010) Monitoring sea-ice and dry snow with GNSS reflections 38(5):3837–3840
Jin S, Komjathy A (2010) GNSS reflectometry and remote sensing: new objectives and results. Adv Space Res 46(2):111–117
Jin S, Feng GP, Gleason S (2011) Remote sensing using GNSS signals: current status and future directions. Adv Space Res 47(10):1645–1653
Larson KM et al (2008) Using GPS multipath to measure soil moisture fluctuations: initial results. GPS Solut 12(3):173–177
Ozeki M, Heki K (2012) GPS snow depth meter with geometry-free linear combinations of carrier phases. J Geodesy 86(3):209–219
Yu K et al (2015) Snow depth estimation based on multipath phase combination of GPS triple-frequency signals. IEEE Trans Geosci Remote Sens 53(9):5100–5109
Jin S, Qian X, Kutoglu H (2016) Snow depth variations estimated from GPS-reflectometry: a case study in Alaska from L2P SNR Data. Remote Sens 8(1):63
Huang DF et al (2001) Wavelet Filters Based Separation of GPS multi-path effects and engineering structure vibrations. Acta Geodaetica Et Cartographic Sinica 30(1):36–41
Acknowledgements
This work was sponsored by the National Natural Foundation of China (41704027; 41664002); the “Ba Gui Scholars” program of the provincial government of Guangxi; Guangxi Natural Science Foundation of China (2017GXNSFBA198139; 2017GXNSFDA198016); the Guangxi Key Laboratory of Spatial Information and Geomatics (16-380-25-01); and the basic ability promotion program for young and middle-aged teachers of Guangxi (KY2016YB189). The authors would like to thank the International GNSS Service Center (IGS) for providing the GPS observation and the National Climatic Data Center (NCDC) for providing the in situ snow depth data.
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Zhou, W., Liu, L., Huang, L., Chen, J., Li, S. (2018). Snow Depth Detection Based on L2 SNR of GLONASS Satellites and Multipath Reflectometry. In: Sun, J., Yang, C., Guo, S. (eds) China Satellite Navigation Conference (CSNC) 2018 Proceedings. CSNC 2018. Lecture Notes in Electrical Engineering, vol 497. Springer, Singapore. https://doi.org/10.1007/978-981-13-0005-9_19
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DOI: https://doi.org/10.1007/978-981-13-0005-9_19
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