Sea Ice Thickness Estimation Based on Regression Neural Networks Using L-Band Microwave Radiometry Data from the FSSCat Mission

被引:15
作者
Herbert, Christoph [1 ,2 ,3 ,5 ]
Munoz-Martin, Joan Francesc [1 ,2 ]
Llaveria, David [1 ,2 ]
Pablos, Miriam [3 ,4 ]
Camps, Adriano [1 ,2 ,3 ]
机构
[1] Univ Politecn Catalunya UPC, CommSensLab, Jordi Girona 1-3, Barcelona 08034, Spain
[2] Inst Estudis Espacials Catalunya IEEC CTE UPC, Jordi Girona 1-3, Barcelona 08034, Spain
[3] Barcelona Expert Ctr BEC, Passeig Maritim Barceloneta 37-49, Barcelona 08003, Spain
[4] CSIC, Inst Ciencies Mar ICM, Passeig Maritim Barceloneta 37-49, Barcelona 08003, Spain
[5] Dept Signal Theory & Commun TSC, Bldg D3,1st Floor,Room 114,Jordi Girona 1-3, Barcelona 08034, Spain
关键词
predictive regression neural networks; sea ice thickness; microwave radiometry; CubeSats; SNOW DEPTH; RETRIEVAL; CRYOSAT-2; FREEBOARD;
D O I
10.3390/rs13071366
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Several methods have been developed to provide polar maps of sea ice thickness (SIT) from L-band brightness temperature (TB) and altimetry data. Current process-based inversion methods to yield SIT fail to address the complex surface characteristics because sea ice is subject to strong seasonal dynamics and ice-physical properties are often non-linearly related. Neural networks can be trained to find hidden links among large datasets and often perform better on convoluted problems for which traditional approaches miss out important relationships between the observations. The FSSCat mission launched on 3 September 2020, carries the Flexible Microwave Payload-2 (FMPL-2), which contains the first Reflected Global Navigation Satellite System (GNSS-R) and L-band radiometer on board a CubeSat-designed to provide TB data on global coverage for soil moisture retrieval, and sea ice applications. This work investigates a predictive regression neural network approach with the goal to infer SIT using FMPL-2 TB and ancillary data (sea ice concentration, surface temperature, and sea ice freeboard). Two models-covering thin ice up to 0.6 m and full-range thickness-were separately trained on Arctic data in a two-month period from mid-October to the beginning of December 2020, while using ground truth data derived from the Soil Moisture and Ocean Salinity (SMOS) and Cryosat-2 missions. The thin ice and the full-range models resulted in a mean absolute error of 6.5 cm and 23 cm, respectively. Both of the models allowed for one to produce weekly composites of Arctic maps, and monthly composites of Antarctic SIT were predicted based on the Arctic full-range model. This work presents the first results of the FSSCat mission over the polar regions. It reveals the benefits of neural networks for sea ice retrievals and demonstrates that moderate-cost CubeSat missions can provide valuable data for applications in Earth observation.
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页数:20
相关论文
共 55 条
[1]  
[Anonymous], 2016, NAT METHODS, DOI DOI 10.1038/nmeth.3707
[2]   Fluctuating arctic sea ice thickness changes estimated by an in situ learned and empirically forced neural network model [J].
Belchansky, G. I. ;
Douglas, D. C. ;
Platonov, N. G. .
JOURNAL OF CLIMATE, 2008, 21 (04) :716-729
[3]   MULTIDIMENSIONAL BINARY SEARCH TREES USED FOR ASSOCIATIVE SEARCHING [J].
BENTLEY, JL .
COMMUNICATIONS OF THE ACM, 1975, 18 (09) :509-517
[4]   Estimating snow depth on Arctic sea ice using satellite microwave radiometry and a neural network [J].
Braakmann-Folgmann, Anne ;
Donlon, Craig .
CRYOSPHERE, 2019, 13 (09) :2421-2438
[5]  
Camps A, 2018, INT GEOSCI REMOTE SE, P8285, DOI 10.1109/IGARSS.2018.8518405
[6]  
Camps A., 2019, SATELLITES INNOVATIV
[7]   Prediction of Arctic Sea Ice Concentration Using a Fully Data Driven Deep Neural Network [J].
Chi, Junhwa ;
Kim, Hyun-choel .
REMOTE SENSING, 2017, 9 (12)
[8]  
Chong E. K., 2004, An introduction to optimization
[9]   Passive microwave algorithms for sea ice concentration: A comparison of two techniques [J].
Comiso, JC ;
Cavalieri, DJ ;
Parkinson, CL ;
Gloersen, P .
REMOTE SENSING OF ENVIRONMENT, 1997, 60 (03) :357-384
[10]  
De Roo RD, 2004, AEROSP CONF PROC, P1015