Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry (InSAR) phase variations. Eppler, J., Rabus, B., & Morse, P. The Cryosphere, 16(4):1497–1521, April, 2022. ![Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry (InSAR) phase variations [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex Abstract. Area-based measurements of snow water equivalent (SWE) are important for understanding earth system processes such as glacier mass balance, winter hydrological storage in drainage basins, and ground thermal regimes. Remote sensing techniques are ideally suited for wide-scale area-based mapping with the most commonly used technique to measure SWE being passive microwave, which is limited to coarse spatial resolutions of 25 km or greater and to areas without significant topographic variation. Passive microwave also has a negative bias for large SWE. Another method is repeat-pass synthetic aperture radar interferometry (InSAR) that allows measurement of SWE change at much higher spatial resolution. However, it has not been widely adopted because (1) the phase unwrapping problem has not been robustly addressed, especially for interferograms with poor coherence, and (2) SWE change maps scaled directly from repeat-pass interferograms are not an absolute measurement but contain unknown offsets for each contiguous coherent area. We develop and test a novel method for repeat-pass InSAR-based dry-snow SWE estimation that exploits the sensitivity of the dry-snow refraction-induced InSAR phase to topographic variations. The method robustly estimates absolute SWE change at spatial resolutions of \textless 1 km without the need for phase unwrapping. We derive a quantitative signal model for this new SWE change estimator and identify the relevant sources of bias. The method is demonstrated using both simulated SWE distributions and a 9-year RADARSAT-2 (C-band, 5.405 GHz) spotlight-mode dataset near Inuvik, Northwest Territories (NWT), Canada. SWE results are compared to in situ snow survey measurements and estimates from ERA5 reanalysis. Our method performs well in high-relief areas, thus providing complementary coverage to passive-microwave-based SWE estimation. Further, our method has the advantage of requiring only a single wavelength band and thus can utilize existing spaceborne synthetic aperture radar systems.
@article{eppler_snow_2022,
title = {Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry ({InSAR}) phase variations},
volume = {16},
issn = {1994-0424},
url = {https://tc.copernicus.org/articles/16/1497/2022/},
doi = {10.5194/tc-16-1497-2022},
abstract = {Abstract. Area-based measurements of snow water equivalent (SWE) are important for understanding earth system processes such as glacier mass balance, winter
hydrological storage in drainage basins, and ground thermal regimes. Remote sensing techniques are ideally suited for wide-scale area-based mapping
with the most commonly used technique to measure SWE being passive microwave, which is limited to coarse spatial resolutions of 25 km or
greater and to areas without significant topographic variation. Passive microwave also has a negative bias for large SWE. Another method is
repeat-pass synthetic aperture radar interferometry (InSAR) that allows measurement of SWE change at much higher spatial resolution. However, it
has not been widely adopted because (1) the phase unwrapping problem has not been robustly addressed, especially for interferograms with poor
coherence, and (2) SWE change maps scaled directly from repeat-pass interferograms are not an absolute measurement but contain unknown offsets for
each contiguous coherent area. We develop and test a novel method for repeat-pass InSAR-based dry-snow SWE estimation that exploits the sensitivity
of the dry-snow refraction-induced InSAR phase to topographic variations. The method robustly estimates absolute SWE change at spatial resolutions
of {\textless} 1 km without the need for phase unwrapping. We derive a quantitative signal model for this new SWE change estimator and identify
the relevant sources of bias. The method is demonstrated using both simulated SWE distributions and a 9-year RADARSAT-2 (C-band,
5.405 GHz) spotlight-mode dataset near Inuvik, Northwest Territories (NWT), Canada. SWE results are compared to in situ snow survey measurements and estimates from
ERA5 reanalysis. Our method performs well in high-relief areas, thus providing complementary coverage to passive-microwave-based SWE
estimation. Further, our method has the advantage of requiring only a single wavelength band and thus can utilize existing spaceborne synthetic
aperture radar systems.},
language = {en},
number = {4},
urldate = {2023-06-15},
journal = {The Cryosphere},
author = {Eppler, Jayson and Rabus, Bernhard and Morse, Peter},
month = apr,
year = {2022},
keywords = {NALCMS},
pages = {1497--1521},
}
Downloads: 0
{"_id":"ZXNbmvGc8HLQrhWd6","bibbaseid":"eppler-rabus-morse-snowwaterequivalentchangemappingfromslopecorrelatedsyntheticapertureradarinterferometryinsarphasevariations-2022","author_short":["Eppler, J.","Rabus, B.","Morse, P."],"bibdata":{"bibtype":"article","type":"article","title":"Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry (InSAR) phase variations","volume":"16","issn":"1994-0424","url":"https://tc.copernicus.org/articles/16/1497/2022/","doi":"10.5194/tc-16-1497-2022","abstract":"Abstract. Area-based measurements of snow water equivalent (SWE) are important for understanding earth system processes such as glacier mass balance, winter hydrological storage in drainage basins, and ground thermal regimes. Remote sensing techniques are ideally suited for wide-scale area-based mapping with the most commonly used technique to measure SWE being passive microwave, which is limited to coarse spatial resolutions of 25 km or greater and to areas without significant topographic variation. Passive microwave also has a negative bias for large SWE. Another method is repeat-pass synthetic aperture radar interferometry (InSAR) that allows measurement of SWE change at much higher spatial resolution. However, it has not been widely adopted because (1) the phase unwrapping problem has not been robustly addressed, especially for interferograms with poor coherence, and (2) SWE change maps scaled directly from repeat-pass interferograms are not an absolute measurement but contain unknown offsets for each contiguous coherent area. We develop and test a novel method for repeat-pass InSAR-based dry-snow SWE estimation that exploits the sensitivity of the dry-snow refraction-induced InSAR phase to topographic variations. The method robustly estimates absolute SWE change at spatial resolutions of \\textless 1 km without the need for phase unwrapping. We derive a quantitative signal model for this new SWE change estimator and identify the relevant sources of bias. The method is demonstrated using both simulated SWE distributions and a 9-year RADARSAT-2 (C-band, 5.405 GHz) spotlight-mode dataset near Inuvik, Northwest Territories (NWT), Canada. SWE results are compared to in situ snow survey measurements and estimates from ERA5 reanalysis. Our method performs well in high-relief areas, thus providing complementary coverage to passive-microwave-based SWE estimation. Further, our method has the advantage of requiring only a single wavelength band and thus can utilize existing spaceborne synthetic aperture radar systems.","language":"en","number":"4","urldate":"2023-06-15","journal":"The Cryosphere","author":[{"propositions":[],"lastnames":["Eppler"],"firstnames":["Jayson"],"suffixes":[]},{"propositions":[],"lastnames":["Rabus"],"firstnames":["Bernhard"],"suffixes":[]},{"propositions":[],"lastnames":["Morse"],"firstnames":["Peter"],"suffixes":[]}],"month":"April","year":"2022","keywords":"NALCMS","pages":"1497–1521","bibtex":"@article{eppler_snow_2022,\n\ttitle = {Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry ({InSAR}) phase variations},\n\tvolume = {16},\n\tissn = {1994-0424},\n\turl = {https://tc.copernicus.org/articles/16/1497/2022/},\n\tdoi = {10.5194/tc-16-1497-2022},\n\tabstract = {Abstract. Area-based measurements of snow water equivalent (SWE) are important for understanding earth system processes such as glacier mass balance, winter\nhydrological storage in drainage basins, and ground thermal regimes. Remote sensing techniques are ideally suited for wide-scale area-based mapping\nwith the most commonly used technique to measure SWE being passive microwave, which is limited to coarse spatial resolutions of 25 km or\ngreater and to areas without significant topographic variation. Passive microwave also has a negative bias for large SWE. Another method is\nrepeat-pass synthetic aperture radar interferometry (InSAR) that allows measurement of SWE change at much higher spatial resolution. However, it\nhas not been widely adopted because (1) the phase unwrapping problem has not been robustly addressed, especially for interferograms with poor\ncoherence, and (2) SWE change maps scaled directly from repeat-pass interferograms are not an absolute measurement but contain unknown offsets for\neach contiguous coherent area. We develop and test a novel method for repeat-pass InSAR-based dry-snow SWE estimation that exploits the sensitivity\nof the dry-snow refraction-induced InSAR phase to topographic variations. The method robustly estimates absolute SWE change at spatial resolutions\nof {\\textless} 1 km without the need for phase unwrapping. We derive a quantitative signal model for this new SWE change estimator and identify\nthe relevant sources of bias. The method is demonstrated using both simulated SWE distributions and a 9-year RADARSAT-2 (C-band,\n5.405 GHz) spotlight-mode dataset near Inuvik, Northwest Territories (NWT), Canada. SWE results are compared to in situ snow survey measurements and estimates from\nERA5 reanalysis. Our method performs well in high-relief areas, thus providing complementary coverage to passive-microwave-based SWE\nestimation. Further, our method has the advantage of requiring only a single wavelength band and thus can utilize existing spaceborne synthetic\naperture radar systems.},\n\tlanguage = {en},\n\tnumber = {4},\n\turldate = {2023-06-15},\n\tjournal = {The Cryosphere},\n\tauthor = {Eppler, Jayson and Rabus, Bernhard and Morse, Peter},\n\tmonth = apr,\n\tyear = {2022},\n\tkeywords = {NALCMS},\n\tpages = {1497--1521},\n}\n\n\n\n","author_short":["Eppler, J.","Rabus, B.","Morse, P."],"key":"eppler_snow_2022","id":"eppler_snow_2022","bibbaseid":"eppler-rabus-morse-snowwaterequivalentchangemappingfromslopecorrelatedsyntheticapertureradarinterferometryinsarphasevariations-2022","role":"author","urls":{"Paper":"https://tc.copernicus.org/articles/16/1497/2022/"},"keyword":["NALCMS"],"metadata":{"authorlinks":{}}},"bibtype":"article","biburl":"https://bibbase.org/zotero/NAAtlas2024","dataSources":["qLjf8q88GSLZ5dAmC"],"keywords":["nalcms"],"search_terms":["snow","water","equivalent","change","mapping","slope","correlated","synthetic","aperture","radar","interferometry","insar","phase","variations","eppler","rabus","morse"],"title":"Snow water equivalent change mapping from slope-correlated synthetic aperture radar interferometry (InSAR) phase variations","year":2022}