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DOI | 10.1016/j.rse.2020.112111 |
On the impact of C-band in place of L-band radar for SMAP downscaling | |
Ghafari E.; Walker J.P.; Das N.N.; Davary K.; Faridhosseini A.; Wu X.; Zhu L. | |
发表日期 | 2020 |
ISSN | 00344257 |
卷号 | 251 |
英文摘要 | The National Aeronautics and Space Administration (NASA) Soil Moisture Active Passive (SMAP) mission was launched on 31st January 2015, with the aim of providing global soil moisture maps at 9 km spatial resolution by combining L-band radar and radiometer observations. However, after the SMAP radar became inoperable, NASA decided to utilize the Sentinel 1A/1B C-band SAR data in its place. The new version of baseline brightness temperature (Tb) downscaling algorithm for SMAP is tested using L-band airborne data to evaluate the capabilities of the C-band Sentinel-1A SAR relative to L-band radar data in downscaling the SMAP Tb for achieving high resolution brightness temperature. In this study, the downscaling algorithm used L-band airborne Synthetic Aperture Radar (SAR) backscatter (σ) collected from the fifth Soil Moisture Active Passive Experiment (SMAPEx-5) in south-eastern Australia to downscale 36 km L-band SMAP radiometer Tb pixels to 3 km and 9 km. The downscaling results were then compared with the published results using Sentinel-1A C-band backscatter, and evaluated against airborne 1 km resolution L-band passive microwave brightness temperature collected from SMAPEx-5. The results show that for vertical polarization the average Root Mean Square Error (RMSE) of downscaled Tb when compared with reference airborne Tb across 4 days at 9 km resolution were 4.9 K for L-band and 6.0 K for C-band, and increased to 9.3 K for L-band and 9.6 K for C-band at 3 km spatial resolution. Moreover, the correlation coefficient (R) of downscaled and reference Tb across the 4 days was 0.92 for L-band and 0.88 for C-band at 9 km, decreasing to 0.75 for L-band and 0.72 for C-band at 3 km spatial resolution. Accordingly, the RMSE increased and the correlation coefficient decreased when using C-band radar data in place of that at L-band. However, overall there is expected to be only a slight decrease in performance of the downscaling algorithm by using the Sentinel 1A data in place of the SMAP radar. © 2020 |
英文关键词 | Backscatter; Brightness temperature; C-band; Downscaling; L-band; Sentinel-1A; SMAP; SMAPEx |
语种 | 英语 |
scopus关键词 | Backscattering; Image resolution; Luminance; Mean square error; NASA; Radiometers; Soil moisture; Temperature; Airborne synthetic aperture radars; Brightness temperatures; Correlation coefficient; Passive microwave brightness temperatures; Root mean square errors; Soil moisture active passive (SMAP); South-eastern Australia; Vertical polarization; Synthetic aperture radar; algorithm; backscatter; brightness temperature; downscaling; radar; radiometer; satellite data; satellite mission; soil moisture; spatial resolution; spatiotemporal analysis; synthetic aperture radar; Australia |
来源期刊 | Remote Sensing of Environment |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/179107 |
作者单位 | Department of Civil Engineering, Monash University, Melbourne, Australia; Department of Water Engineering, Ferdowsi University, Mashhad, Iran; Jet Propulsion Laboratory, NASA, California Institute of Technology, Pasadena, CA 91109, United States; Centre for Water Systems, College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom |
推荐引用方式 GB/T 7714 | Ghafari E.,Walker J.P.,Das N.N.,et al. On the impact of C-band in place of L-band radar for SMAP downscaling[J],2020,251. |
APA | Ghafari E..,Walker J.P..,Das N.N..,Davary K..,Faridhosseini A..,...&Zhu L..(2020).On the impact of C-band in place of L-band radar for SMAP downscaling.Remote Sensing of Environment,251. |
MLA | Ghafari E.,et al."On the impact of C-band in place of L-band radar for SMAP downscaling".Remote Sensing of Environment 251(2020). |
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