the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 05 Feb 2024
Evaluating L-band InSAR Snow Water Equivalent Retrievals with Repeat Ground-Penetrating Radar and Terrestrial Lidar Surveys in Northern Colorado
Abstract. Snow provides critical water resources for billions of people, making the remote sensing of snow water equivalent (SWE) a highly prioritized endeavor, particularly given current and projected climate change impacts. Synthetic Aperture Radar (SAR) is a promising method for remote sensing of SWE because radar penetrates snow and SAR interferometry (InSAR) can be used to estimate changes in SWE (ΔSWE) between SAR acquisitions. We calculated ΔSWE retrievals from 10 NASA L-band Uninhabited Aerial Vehicle SAR (UAVSAR) acquisitions in northern Colorado during the winters of 2020 and 2021 and evaluated the retrievals against measurements of SWE from ground-penetrating radar (GPR) and terrestrial lidar scans (TLS) collected as part of the NASA SnowEx 2020 and 2021 Time Series Campaigns. Next, we evaluated the full UAVSAR time series at the northern Colorado sites using SWE measured at seven automated stations and ascertained whether coherence can be used as an accuracy metric for ΔSWE retrievals. For single InSAR pairs, UAVSAR ΔSWE retrievals displayed high correlation with TLS and GPR ΔSWE retrievals (overall r = 0.72–0.79) and yielded an RMSE of 19–22 mm. When compared to SWE at seven automated stations, cumulative SWE from UAVSAR retrievals exhibited poor agreement in 2020, but high agreement in 2021. We found that SWE can be reliably retrieved, even for lower coherences, as RMSE values ranged by <10 mm from coherences of 0.10 to 0.90. The upcoming NASA-ISRO SAR satellite mission, with a 12-day revisit period, offers an exciting opportunity to apply this methodology globally, but further quantification of limitations is necessary, particularly in forested environments and as the snowpack begins to melt.
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CC1: 'Comment on egusphere-2024-236', Giacomo Medici, 12 Feb 2024
General comments
Paper of large impact that can be highly cited in the future. Indeed, lots of research is focusing these days on remote sensing and the role of the snowpack in hydrology. See below my specific comments for the Discussion.
Specific comments
Abstract
- Lines 30-40. Specify in the abstract the spatial scale. How much is the area large? The idea is to provide the observation scale in the abstract to enhance clarity.
Introduction
- Lines 42. “In snow-dominated watersheds, melt from seasonal snowpacks drives streamflow and groundwater recharge”. Add recent papers that show the importance of snowmelt on aquifer recharge in snow-dominated watersheds worldwide:
- Tracking flowpaths in a complex karst system through tracer test and hydrogeochemical monitoring: Implications for groundwater protection (Gran Sasso, Italy). Heliyon, https://doi.org/10.1016/j.heliyon.2024.e24663
- Snowpack aging, water isotope evolution, and runoff isotope signals, Palouse Range, Idaho, USA. Hydrology, 9(6), 94, https://doi.org/10.3390/hydrology9060094
- Line 50. Summarize the scenario of snow decline in other mountain belts. What about Andes? See below:
- Rapid decline of snow and ice in the tropical Andes–Impacts, uncertainties and challenges ahead. Earth-science Reviews, 176, 195-213, https://doi.org/10.1016/j.earscirev.2017.09.019.
Line 116. I suggest adding the three to four specific objectives of the research by using numbers (e.g., i, ii, iii).
Methods.
- Line 174. “Along a ~40–60 km stretch with a 16 km swath width”. I suggest inserting the link with Figure 1a.
- Line 221. I suggest “key in situ measurements included in this research are:...”
- Line 271. “3×3 pixel grid”. Please, specify the size.
Results
- Line 305. “RMSE”, specify the acronym “Root Mean Squared Error” earlier in the manuscript.
Discussion and Conclusion
- Lines 503-518. Recall the wider implications of your paper that are part of your discussion. Please, do not simply summarize your results in the Conclusion.
Figures and tables
- Figure 2. I suggest to make either the boxes for GPR and TLS workflows lighter. The green in the GPR Workflow is too dark for letters in black.
- Figure 8. Not very conceptual. Is it necessary in the manuscript? Possible to insert in the Supplementary Material?
References
- Lines 644-870. Add the relevant references suggested above on the importance of the snowpack in the hydrological cycle.
Citation: https://doi.org/10.5194/egusphere-2024-236-CC1 - AC1: 'Reply on CC1', Randall Bonnell, 18 May 2024
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RC1: 'Comment on egusphere-2024-236', Jeff Dozier, 01 Mar 2024
My comments include an equation and a figure, so also see the attached PDF.
This paper presents interesting results that offer both hope and caution for L-band InSAR and InSAR generally. The quality and extent of the field validation data are impressive, perhaps the best I’ve seen from a field snow experiment.
Three suggestions to improve the analysis and the presentation:
- My major critique is that the target audience has to know a lot about radar and radar remote sensing of snow properties to understand the paper’s implications. Craig Bohren has a pointed phrase about a subject being “well known to those that know it well,” and this paper unfortunately hits that spot especially in the Introduction. Some colleagues tell me that the coded vocabulary makes the radar remote sensing literature hard to penetrate.
- The approach for all the methods for SWE retrieval seems to combine a measurement of depth by some remotely sensed method, and then to multiply those depths by estimates of density. With snow depths retrieved from lidar or photogrammetry, this is the viable approach, but from InSAR data it’s feasible (and probably better) to directly retrieve SWE without estimating depth or density.
- The explanations for getting SWE from InSAR are scattered throughout: in the Introduction, Section 3 (Methods), or the Appendix. Perhaps consolidating might be the answer, or advise some readers to read the Appendix first.
Some line-by-line comments, but consider in the context of the three points above.
Line 30: maybe insert a short parenthetical definition of L-band (frequency 1-2 GHz).
Line 35: I tend to avoid adjectives (“high” here) to describe statistical measures like correlation. In some spectroscopic retrievals I work on, r<0.9 is awful. Present the values themselves.
Line 34: Is “coherence” the same as “correlation”? Without knowing that, some of the rest of the Abstract is hard to interpret. In general, this issue pervades the paper. Coherence is shown to be important but isn’t defined.
Line 36: poor in one year, good the next. Any explanation? I see on Line 420 that this may be an artifact of mis-registration between airborne and in situ data.
Line 37: The sentence “We found that …” seems incongruous with RMSE between 19-22 mm. It would also be useful to specify the ranges of SWE (total) and ΔSWE (between passes) in the experiment. This information does show up later in the paper.
Line 47: The Wrzesien 2018 paper covered North America but the sentence is global. Maybe cite the 2019 paper instead (DO10.1029/2019WR025350I) or clarify that the sentence applies to North America in the 2018 paper.
Line 54: SNOTEL stations are all on nearly flat terrain, hence interpolating between them misses effects of slope and orientation. This sampling bias, combined with the spatial and elevational extent of the snow pillow network, subjects interpolation to artifacts.
Line 56, let’s correct a misunderstanding: National Academies of Sciences, Engineering and Medicine are NOT a “government agency.”
Line 60: I don’t think SnowEx was a “mission.” The Durand et al. 2018 reference uses “campaign.”
Line 65: “is” not “are”.
Line 72: Need a short tutorial here explaining what backscatter, time-of-flight, and co-polar phase difference are. And then a sentence about why the paper focuses on InSAR (which indeed is defensible). The reference to Borah et al. 2023 perhaps distracts. If indeed we can measure SWE up to 800 mm based on backscattering at X- and Ku-band, why go to interferometry? Earlier work by Jiancheng Shi also got impressive results based on multifrequency multipolarization backscatter, albeit with validation by a only few snow pits.
Consider this comment in the context of data processing. Then the details of how you measure coherence, time delay, phase angle, etc. (now Lines 85-107) can be covered in Section 3 or in the Appendix (but make the forward reference).Line 74 et seq. At the first introduction of “frequency,” it would be useful to include a short table that translates between “Q”-band, frequency, and wavelength. I hope that this paper will be read by people who have no idea what X-band is, or whether X-band’s frequency is greater than or less than P-band’s.
Line 85: Maybe a sketch here to explain what a phase change and a coherent reflection are, or cite where one can find an explanation, or refer to Section 3 or the Appendix. In the current version, it’s difficult to figure out how one goes from measurement to estimate of phase change.
Line 86: “The technique was first established at C-band . . .” First established to do what? Does this remark refer especially to snow, or to interferometric retrievals of elevation?
Line 88: “interferogram” indeed well known to a small community, possibly obtuse to other readers.
Line 98: Not sure what “only two of these studies have not considered atmospheric signal delays” means. Does it imply that signal delays are important, but seemingly well covered?
Line 100-108: This paragraph has information, but not enough to know how one gets a measurement of phase difference between an interferometric pair. Also, is coherence the same as a product-moment correlation? Or something related but different?
Line 170: I suggest expanding section 3.1 with material from the Introduction (line 85-107) For the less informed reader, the relationship between coherence and phase is arcane. In particular, the snow properties that degrade coherence are important and affect the need for frequent image acquisition. How is the interferometric phase angle determined from the correlated (cohered?) pairs?
Line 177: And then we have to worry about “phase unwrapping,” but this text doesn’t tell us what that is. Also, is phase unwrapping a problem generally with SAR at L-band and higher frequency? Perhaps interpret the equations in Leinss et al. 2015 to explain? (Later I see phase unwrapping at ~100 mm)
Figure 2 and Line 196: Calculations of Incidence Angles from the Copernicus DEM lead to an uncertainty in cosine(incidence) of ~0.1 (from my own work, DOI 10.1029/2022JG007147), but are you able to overcome this problem because repeated images get you the right incidence geometry? Otherwise this is a source of uncertainty, even with the best available global DEM.
Line 215: Can you include a equation that defines Coherence? Or is it just Pearson product-moment correlation?
Line 235: Maybe include a citation to Reflex W? I may not need to know what a “de-wow” filter is, but I’d like to know that I could find out.
Line 248: The title of Section 3.2.3 is “TLS” but the section also covers the UAV lidar.
Line 283: “phase cycle” appears here for the first time. The cognoscenti know what this is but some readers may not.
Line 424: “phase unwrapping” is mentioned here and elsewhere. In processing the interferometric phase values, how do you decide when you’ve gone through a phase cycle? Or more than one?
ESTIMATING SWE DIRECTLY FROM InSAR (instead of estimating depth and multiplying by density)
[Check the attached PDF, as this section includes an equation and a figure]
A compelling argument for InSAR is its lack of dependence on density, in contrast to lidar for example where the biggest uncertainty is that in density.
- AC2: 'Reply on RC1', Randall Bonnell, 18 May 2024
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RC2: 'Comment on egusphere-2024-236', Anonymous Referee #2, 21 Mar 2024
Review
General Comment
The article ‚Evaluating L-band InSAR Snow Water Equivalent Retrievals with Repeat Ground-Penetrating Radar and Terrestrial Lidar Surveys in Northern Colorado’ compares SWE change retrievals from airborne interferometric SAR data, ground penetrating radar, terrestrial lidar scans, automated measurement stations and in-situ measurements. The paper provides an extensive data analysis for two winters (2020 and 2021) over different test sites in Colorado. The authors also analyze the impact of low coherence on the SWE change retrieval, providing valuable insights for future space borne L-band SAR missions.
Specific Comments
Line 37: Maybe you can add half a sentence why the agreement was poor in 2020.
Line 98: The meaning of this sentence is hard to understand. Maybe you could rephrase it.
Line 100-108: You could think of adding this paragraph about the interferometric coherence to Appendix A.2., where you also describe the interferometric phase.
Line 124: Why have you used a different heading for the 27.01. /03.02. interferogram and not the 141° as well?
Line 177: Do you know why the coherence was low for that interferogram? Please elaborate briefly.
Line 183: Maybe you can point out that it is a SWE change retrieval, so you can just measure changes between the measurements, and not directly the total SWE.
Line 211: Were the 20% GPR SWE change retrievals used for estimating the absolute phase selected randomly? And why have you not used the In-Situ stations for absolute phase calibration?
Line 271: What is the resolution your 3x3 pixel grid?
Line 352: Why have you chosen HH and not VV? Since the RMSE is smaller for VV.
Line 492: In this paragraph you are discussing the influence of wet snow. Maybe you can also add that wet snow increases the absorption and decreases the penetration depth of the radar wave in the snow volume.
Line 520: In your Appendix A.1 you describe the L-Band transmissibility, which is very interesting, but you never refer to A.1.
Line 538: (Referring to comment on line 100-108). Maybe you could also add here an equation for the interferometric coherence, so it is easier to understand what it means and how you can obtain the interferometric phase.
Line 548: In A.2.2 you are describing the atmospheric correction for UAVSAR. I am not an expert in this field, but I understood that you are estimating a phase ramp due to the atmosphere and then are checking if the atmospheric correction is improving your SWE change estimates. You stated that it does not improve your results. But where does your calculated phase ramp then come from? Maybe you could explain this more.
Line 595: In (Leinss et al., 2015) an approach was presented, where a linear function between the SWE change and interferometric phase was derived. This has the advantage that you can directly derive the SWE change from the phase without the need of additional in-situ density measurements, which is the main advantage of the DInSAR approach compared to the GPR or LIDAR retrieval. Maybe you can think about it, since you also stated in line 66 that the need of in-situ density measurements adds uncertainty. Or state why you have chosen to use the approach with Equation (A5) and (A6).
Line 598: You maybe could point out that these are snow depth changes and SWE changes.
Technical Corrections
Line 53: Reference for the SNOTEL stations
Line 183: ...is outlined in Appendix A.2?
Line 236: The GPR Workflow in Figure 2 shows the Radargram processing and it has first the step (4) and then the step (3). Maybe you can make it more consistent.
Line 320, Line 333: It is hard to see the points in Figure 5 (i) and Figure 6 (i).
Line 352: Space after Figure missing.
Line 352: Parenthesis after HH.
Line 353: In the Table S4 the RMSE is 21mm and not 22mm.
Line 375, Line 378, Line 382: There is no Figure 8 (a-i).
Supplementary Material:
Line 62: There is only Figure 8 (a-b).
Citation: https://doi.org/10.5194/egusphere-2024-236-RC2 - AC3: 'Reply on RC2', Randall Bonnell, 18 May 2024
Interactive discussion
Status: closed
-
CC1: 'Comment on egusphere-2024-236', Giacomo Medici, 12 Feb 2024
General comments
Paper of large impact that can be highly cited in the future. Indeed, lots of research is focusing these days on remote sensing and the role of the snowpack in hydrology. See below my specific comments for the Discussion.
Specific comments
Abstract
- Lines 30-40. Specify in the abstract the spatial scale. How much is the area large? The idea is to provide the observation scale in the abstract to enhance clarity.
Introduction
- Lines 42. “In snow-dominated watersheds, melt from seasonal snowpacks drives streamflow and groundwater recharge”. Add recent papers that show the importance of snowmelt on aquifer recharge in snow-dominated watersheds worldwide:
- Tracking flowpaths in a complex karst system through tracer test and hydrogeochemical monitoring: Implications for groundwater protection (Gran Sasso, Italy). Heliyon, https://doi.org/10.1016/j.heliyon.2024.e24663
- Snowpack aging, water isotope evolution, and runoff isotope signals, Palouse Range, Idaho, USA. Hydrology, 9(6), 94, https://doi.org/10.3390/hydrology9060094
- Line 50. Summarize the scenario of snow decline in other mountain belts. What about Andes? See below:
- Rapid decline of snow and ice in the tropical Andes–Impacts, uncertainties and challenges ahead. Earth-science Reviews, 176, 195-213, https://doi.org/10.1016/j.earscirev.2017.09.019.
Line 116. I suggest adding the three to four specific objectives of the research by using numbers (e.g., i, ii, iii).
Methods.
- Line 174. “Along a ~40–60 km stretch with a 16 km swath width”. I suggest inserting the link with Figure 1a.
- Line 221. I suggest “key in situ measurements included in this research are:...”
- Line 271. “3×3 pixel grid”. Please, specify the size.
Results
- Line 305. “RMSE”, specify the acronym “Root Mean Squared Error” earlier in the manuscript.
Discussion and Conclusion
- Lines 503-518. Recall the wider implications of your paper that are part of your discussion. Please, do not simply summarize your results in the Conclusion.
Figures and tables
- Figure 2. I suggest to make either the boxes for GPR and TLS workflows lighter. The green in the GPR Workflow is too dark for letters in black.
- Figure 8. Not very conceptual. Is it necessary in the manuscript? Possible to insert in the Supplementary Material?
References
- Lines 644-870. Add the relevant references suggested above on the importance of the snowpack in the hydrological cycle.
Citation: https://doi.org/10.5194/egusphere-2024-236-CC1 - AC1: 'Reply on CC1', Randall Bonnell, 18 May 2024
-
RC1: 'Comment on egusphere-2024-236', Jeff Dozier, 01 Mar 2024
My comments include an equation and a figure, so also see the attached PDF.
This paper presents interesting results that offer both hope and caution for L-band InSAR and InSAR generally. The quality and extent of the field validation data are impressive, perhaps the best I’ve seen from a field snow experiment.
Three suggestions to improve the analysis and the presentation:
- My major critique is that the target audience has to know a lot about radar and radar remote sensing of snow properties to understand the paper’s implications. Craig Bohren has a pointed phrase about a subject being “well known to those that know it well,” and this paper unfortunately hits that spot especially in the Introduction. Some colleagues tell me that the coded vocabulary makes the radar remote sensing literature hard to penetrate.
- The approach for all the methods for SWE retrieval seems to combine a measurement of depth by some remotely sensed method, and then to multiply those depths by estimates of density. With snow depths retrieved from lidar or photogrammetry, this is the viable approach, but from InSAR data it’s feasible (and probably better) to directly retrieve SWE without estimating depth or density.
- The explanations for getting SWE from InSAR are scattered throughout: in the Introduction, Section 3 (Methods), or the Appendix. Perhaps consolidating might be the answer, or advise some readers to read the Appendix first.
Some line-by-line comments, but consider in the context of the three points above.
Line 30: maybe insert a short parenthetical definition of L-band (frequency 1-2 GHz).
Line 35: I tend to avoid adjectives (“high” here) to describe statistical measures like correlation. In some spectroscopic retrievals I work on, r<0.9 is awful. Present the values themselves.
Line 34: Is “coherence” the same as “correlation”? Without knowing that, some of the rest of the Abstract is hard to interpret. In general, this issue pervades the paper. Coherence is shown to be important but isn’t defined.
Line 36: poor in one year, good the next. Any explanation? I see on Line 420 that this may be an artifact of mis-registration between airborne and in situ data.
Line 37: The sentence “We found that …” seems incongruous with RMSE between 19-22 mm. It would also be useful to specify the ranges of SWE (total) and ΔSWE (between passes) in the experiment. This information does show up later in the paper.
Line 47: The Wrzesien 2018 paper covered North America but the sentence is global. Maybe cite the 2019 paper instead (DO10.1029/2019WR025350I) or clarify that the sentence applies to North America in the 2018 paper.
Line 54: SNOTEL stations are all on nearly flat terrain, hence interpolating between them misses effects of slope and orientation. This sampling bias, combined with the spatial and elevational extent of the snow pillow network, subjects interpolation to artifacts.
Line 56, let’s correct a misunderstanding: National Academies of Sciences, Engineering and Medicine are NOT a “government agency.”
Line 60: I don’t think SnowEx was a “mission.” The Durand et al. 2018 reference uses “campaign.”
Line 65: “is” not “are”.
Line 72: Need a short tutorial here explaining what backscatter, time-of-flight, and co-polar phase difference are. And then a sentence about why the paper focuses on InSAR (which indeed is defensible). The reference to Borah et al. 2023 perhaps distracts. If indeed we can measure SWE up to 800 mm based on backscattering at X- and Ku-band, why go to interferometry? Earlier work by Jiancheng Shi also got impressive results based on multifrequency multipolarization backscatter, albeit with validation by a only few snow pits.
Consider this comment in the context of data processing. Then the details of how you measure coherence, time delay, phase angle, etc. (now Lines 85-107) can be covered in Section 3 or in the Appendix (but make the forward reference).Line 74 et seq. At the first introduction of “frequency,” it would be useful to include a short table that translates between “Q”-band, frequency, and wavelength. I hope that this paper will be read by people who have no idea what X-band is, or whether X-band’s frequency is greater than or less than P-band’s.
Line 85: Maybe a sketch here to explain what a phase change and a coherent reflection are, or cite where one can find an explanation, or refer to Section 3 or the Appendix. In the current version, it’s difficult to figure out how one goes from measurement to estimate of phase change.
Line 86: “The technique was first established at C-band . . .” First established to do what? Does this remark refer especially to snow, or to interferometric retrievals of elevation?
Line 88: “interferogram” indeed well known to a small community, possibly obtuse to other readers.
Line 98: Not sure what “only two of these studies have not considered atmospheric signal delays” means. Does it imply that signal delays are important, but seemingly well covered?
Line 100-108: This paragraph has information, but not enough to know how one gets a measurement of phase difference between an interferometric pair. Also, is coherence the same as a product-moment correlation? Or something related but different?
Line 170: I suggest expanding section 3.1 with material from the Introduction (line 85-107) For the less informed reader, the relationship between coherence and phase is arcane. In particular, the snow properties that degrade coherence are important and affect the need for frequent image acquisition. How is the interferometric phase angle determined from the correlated (cohered?) pairs?
Line 177: And then we have to worry about “phase unwrapping,” but this text doesn’t tell us what that is. Also, is phase unwrapping a problem generally with SAR at L-band and higher frequency? Perhaps interpret the equations in Leinss et al. 2015 to explain? (Later I see phase unwrapping at ~100 mm)
Figure 2 and Line 196: Calculations of Incidence Angles from the Copernicus DEM lead to an uncertainty in cosine(incidence) of ~0.1 (from my own work, DOI 10.1029/2022JG007147), but are you able to overcome this problem because repeated images get you the right incidence geometry? Otherwise this is a source of uncertainty, even with the best available global DEM.
Line 215: Can you include a equation that defines Coherence? Or is it just Pearson product-moment correlation?
Line 235: Maybe include a citation to Reflex W? I may not need to know what a “de-wow” filter is, but I’d like to know that I could find out.
Line 248: The title of Section 3.2.3 is “TLS” but the section also covers the UAV lidar.
Line 283: “phase cycle” appears here for the first time. The cognoscenti know what this is but some readers may not.
Line 424: “phase unwrapping” is mentioned here and elsewhere. In processing the interferometric phase values, how do you decide when you’ve gone through a phase cycle? Or more than one?
ESTIMATING SWE DIRECTLY FROM InSAR (instead of estimating depth and multiplying by density)
[Check the attached PDF, as this section includes an equation and a figure]
A compelling argument for InSAR is its lack of dependence on density, in contrast to lidar for example where the biggest uncertainty is that in density.
- AC2: 'Reply on RC1', Randall Bonnell, 18 May 2024
-
RC2: 'Comment on egusphere-2024-236', Anonymous Referee #2, 21 Mar 2024
Review
General Comment
The article ‚Evaluating L-band InSAR Snow Water Equivalent Retrievals with Repeat Ground-Penetrating Radar and Terrestrial Lidar Surveys in Northern Colorado’ compares SWE change retrievals from airborne interferometric SAR data, ground penetrating radar, terrestrial lidar scans, automated measurement stations and in-situ measurements. The paper provides an extensive data analysis for two winters (2020 and 2021) over different test sites in Colorado. The authors also analyze the impact of low coherence on the SWE change retrieval, providing valuable insights for future space borne L-band SAR missions.
Specific Comments
Line 37: Maybe you can add half a sentence why the agreement was poor in 2020.
Line 98: The meaning of this sentence is hard to understand. Maybe you could rephrase it.
Line 100-108: You could think of adding this paragraph about the interferometric coherence to Appendix A.2., where you also describe the interferometric phase.
Line 124: Why have you used a different heading for the 27.01. /03.02. interferogram and not the 141° as well?
Line 177: Do you know why the coherence was low for that interferogram? Please elaborate briefly.
Line 183: Maybe you can point out that it is a SWE change retrieval, so you can just measure changes between the measurements, and not directly the total SWE.
Line 211: Were the 20% GPR SWE change retrievals used for estimating the absolute phase selected randomly? And why have you not used the In-Situ stations for absolute phase calibration?
Line 271: What is the resolution your 3x3 pixel grid?
Line 352: Why have you chosen HH and not VV? Since the RMSE is smaller for VV.
Line 492: In this paragraph you are discussing the influence of wet snow. Maybe you can also add that wet snow increases the absorption and decreases the penetration depth of the radar wave in the snow volume.
Line 520: In your Appendix A.1 you describe the L-Band transmissibility, which is very interesting, but you never refer to A.1.
Line 538: (Referring to comment on line 100-108). Maybe you could also add here an equation for the interferometric coherence, so it is easier to understand what it means and how you can obtain the interferometric phase.
Line 548: In A.2.2 you are describing the atmospheric correction for UAVSAR. I am not an expert in this field, but I understood that you are estimating a phase ramp due to the atmosphere and then are checking if the atmospheric correction is improving your SWE change estimates. You stated that it does not improve your results. But where does your calculated phase ramp then come from? Maybe you could explain this more.
Line 595: In (Leinss et al., 2015) an approach was presented, where a linear function between the SWE change and interferometric phase was derived. This has the advantage that you can directly derive the SWE change from the phase without the need of additional in-situ density measurements, which is the main advantage of the DInSAR approach compared to the GPR or LIDAR retrieval. Maybe you can think about it, since you also stated in line 66 that the need of in-situ density measurements adds uncertainty. Or state why you have chosen to use the approach with Equation (A5) and (A6).
Line 598: You maybe could point out that these are snow depth changes and SWE changes.
Technical Corrections
Line 53: Reference for the SNOTEL stations
Line 183: ...is outlined in Appendix A.2?
Line 236: The GPR Workflow in Figure 2 shows the Radargram processing and it has first the step (4) and then the step (3). Maybe you can make it more consistent.
Line 320, Line 333: It is hard to see the points in Figure 5 (i) and Figure 6 (i).
Line 352: Space after Figure missing.
Line 352: Parenthesis after HH.
Line 353: In the Table S4 the RMSE is 21mm and not 22mm.
Line 375, Line 378, Line 382: There is no Figure 8 (a-i).
Supplementary Material:
Line 62: There is only Figure 8 (a-b).
Citation: https://doi.org/10.5194/egusphere-2024-236-RC2 - AC3: 'Reply on RC2', Randall Bonnell, 18 May 2024
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