the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Validating Remote-Sensing Measures of Natural Hazards: Granular-Level Links to Insured Loss during a Cyclone
Abstract. Remote-sensing products are widely used after disasters as indicators of incurred damage, yet it remains uncertain which mapped surface-disturbance remote-sensing signals are most informative about residential damages. This study examines the damage from the 2023 Cyclone Gabrielle in New Zealand by linking four publicly available remote-sensing layers—SAR-detected standing water, post-event wetness, soil- or silt-related disturbance, and inferred slope-related disturbance—to residential insurance claims from the public insurer at a fine spatial scale. We construct claim-rate and insurance payout outcomes and estimate cross-sectional models, investigating their association with the data from remote-sensing products. The two insurance outcomes capture recorded claim intensity relative to local building stock and the monetary intensity of insured loss. Slope-related disturbance is most strongly associated with claim occurrence and loss variation in hazard-positive rural areas. Wetness-related disturbance becomes the strongest predictor of loss severity once claims are observed. Standing-water and soil-related indicators provide smaller but more stable signals, and their composite index is positively associated with both claim rates and payouts. Urban areas show higher baseline loss levels, whereas rural areas show stronger marginal responses to additional physical disturbance. Our findings show that remote-sensing indicators are not interchangeable hazard proxies. Their value as proxies for disaster damage depends on the physical signal captured, the damage outcome measured, and the settlement context in which damage occurs.
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Status: open (until 02 Oct 2026)
- RC1: 'Review for egusphere-2026-3539', Anonymous Referee #1, 03 Sep 2026 reply
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RC2: 'Comment on egusphere-2026-3539', Anonymous Referee #2, 16 Sep 2026
reply
Validating remote-sensing measures of natural hazards: Granular-level links to insured loss during a cyclone
This paper examines the relationship between residential property insurance claims—specifically the proportion of claim counts and payout ratios—and remote sensing indicators in regions affected by the 2023 cyclone in New Zealand. As remote sensing indicators, the study employs flood extent estimated from SAR imagery (S-flood), alongside three indicators derived from optical sensors (D-wet, D-soil, and D-slope). Through statistical analysis, the paper reveals that both the claim count ratio and the payout ratio show relatively higher correlations with S-flood and D-soil, and that the performance of these indicators varies between urban and suburban/rural areas. Based on these findings, the paper concludes that estimating damage-related metrics from remote sensing indicators is still challenging.
The use of insurance loss data is invaluable for evaluating and estimating damage scale, and the study deserves credit for utilizing such a precious dataset. However, significant flaws remain regarding the remote sensing indicators selected. While S-flood measures inundated areas using SAR imagery—a metric clearly relevant to cyclone damage—the other three indicators are calculated from pre- and post-disaster changes in NDVI. Because these NDVI-based indicators inherently include seasonal vegetation fluctuations, they lack a direct connection to actual disaster damage. Performing statistical analyses with metrics that have such weak physical ties to actual losses makes it virtually impossible to infer meaningful relationships with monetary damage, leaving the validity of the selected remote sensing indicators questionable.
Furthermore, NDVI is primarily an index used to assess the condition of vegetation and green spaces. In contrast, residential properties (buildings and immediate lots) subject to insurance claims are predominantly non-vegetated, built environments. Asserting that a drop in NDVI in surrounding farmland or woodland directly correlates with physical destruction or inundation of residential structures represents a major leap in physical logic.
If the authors intend to conclude that estimating damage from remote sensing indicators is difficult, it is essential to explore indicators that directly represent cyclone-induced physical damage. A study that skips the critical step of evaluating indicator validity and simply fits basic statistical models remains insufficient. Linking data that fails to separate baseline background noise from true disaster damage directly to insurance claims yields extremely low academic validity and utility.
For these reasons, the reviewer concludes that the paper suffers from flawed methodological premises regarding the physical and disaster-related validity of the input data. As the reliability of its conclusions cannot be guaranteed, this manuscript is recommended for Reject.
Citation: https://doi.org/10.5194/egusphere-2026-3539-RC2 -
RC3: 'Comment on egusphere-2026-3539', Anonymous Referee #3, 16 Sep 2026
reply
Although the title presents the study as a validation exercise, the methodology describes an exploratory cross-sectional analysis. The study assesses correspondence with insurance outcomes but does not validate the accuracy of the remote-sensing measures against independent ground-truth hazard or damage observations.
The selection and construction of the variables requires clear justification. ClaimRate is calculated by dividing residential claims by the number of building footprints in each meshblock, but the building footprints may include garages, sheds and other roofed structures that are not equivalent to insured dwellings. The authors should explain why this is an appropriate denominator and assess the sensitivity of the results to this measurement mismatch. Similarly, hazard intensity is defined as the affected pixel area divided by the total land area of the meshblock. It is unclear why this represents residential hazard exposure, since affected pixels may cover areas without connection to a residential asset.
Re: the PCA discussion - Line 534, 541-543 highlights identical loading as something that supports the study but this is just a natural result of reducing the dimensions to two, you get sqrt(2)/2. A 2-variable PCA reveals 36.3% unexplained variance.
Citation: https://doi.org/10.5194/egusphere-2026-3539-RC3
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The study ‘Validating Remote-Sensing Measures of Natural Hazards: Granular-Level Links to Insured Loss during a Cyclone’ looks at the correlation between four different remote-sensing indicators and the occurrence and magnitude of residential losses represented through natural-hazard insurance claims following Cyclone Gabrielle, which hit the North Island of New Zealand in February 2023.
The study is an interesting and timely contribution to improvements in the validation of risk and hazard indices. While the results are interesting and worth publishing in NHESS, several key points made in the manuscript require further clarification. I would therefore recommend the manuscript for publication after major revisions.
General comments
I think the manuscript will do well in future reviews if the authors are able to address the following issues:
Specific comments:
L37ff: ‘This distinction matters for loss analysis because insurance claims better reflect realised damage rather than meteorological intensity alone. Remote-sensing indicators can therefore provide a more direct spatial link between physical disturbance and observed residential losses and damages.’ These two sentences confuse hazard, risk and vulnerability. Both the meteorological intensity and the used remote sensing indicators are just different ways to measure hazard intensity. Losses are a function of properties exposed to the measured hazard and how vulnerable these properties are to the hazard.
L164:’This “standing water” image has not been validated against ground observations of flood extent.’ That seems like a useful thing to do as I would assume that standing water can be the result of various processes including in-situ rainfall which is different from standing flood water from rivers. Is there a reason why the authors have not done that?
L188f: What is the rationale for normalising LogPayouts by the total number of buildings and not by the number of affected buildings in a mesh block? Normalising by the total number of buildings makes it difficult to distinguish between areas that have few buildings with high damages and areas with many buildings with low damages.
L288ff: It would be good to get at least a bit more detail about the remote sensing indicators used and how they were constructed. For example, for D-Wet, how was the threshold defined to distinguish between higher soil moisture levels following rainfall and higher soil moisture levels caused by flooding?
L423: ‘This sample’ repetition