{"title":"A Simple Snowfall Retrieval Algorithm for the GPM Dual-Frequency Precipitation Radar: Development and Validation With OLYMPEX Campaign Observation","authors":"S. Akiyama, S. Shige, K. Aonashi, T. Iguchi","doi":"10.1029/2024EA003962","DOIUrl":"https://doi.org/10.1029/2024EA003962","url":null,"abstract":"<p>The current operational algorithm for the Ku- and Ka-band Dual-frequency Precipitation Radar (DPR) onboard the Global Precipitation Measurement (GPM) satellite, which does not effectively utilize Ka-band radar, underestimates snowfall amount. We developed a dual-frequency method (DF-method) that can be incorporated into the framework of the DPR operational algorithm. Estimates from the DF-method, as well as those from the operational algorithm, were validated against data nearly simultaneously measured by in situ airborne instruments and those from a ground-based radar during the Olympic Mountains Experiment (OLYMPEX). The results showed the DF-method produced high correlation, but some bias dependent on an assumed particle model. Both the operational algorithm and the DF-method using the scattering properties of the spheroid model equivalent to the best aggregate model yielded unsatisfactory results, indicating that it is important to use realistic snow scattering properties in the DF-method, rather than relying on the Mie or T-matrix scattering.</p>","PeriodicalId":54286,"journal":{"name":"Earth and Space Science","volume":"12 6","pages":""},"PeriodicalIF":2.9,"publicationDate":"2025-06-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024EA003962","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144256418","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Robert Popescu, Nantheera Anantrasirichai, Juliet Biggs
{"title":"Unsupervised Anomaly Detection for Volcanic Deformation in InSAR Imagery","authors":"Robert Popescu, Nantheera Anantrasirichai, Juliet Biggs","doi":"10.1029/2024EA003892","DOIUrl":"https://doi.org/10.1029/2024EA003892","url":null,"abstract":"<p>Satellite-based Interferometric Synthetic Aperture Radar (InSAR) images have the potential to detect volcanic deformation prior to eruptions, but while a vast number of images are routinely acquired, only a small percentage contain volcanic deformation events. Manual inspection could miss these anomalies, and an automatic system modeled with supervised learning requires suitably labeled data sets. To tackle these issues, this paper explores the use of unsupervised deep learning on InSAR images for the purpose of identifying volcanic deformation as anomalies. We test three different state-of-the-art architectures, one convolutional neural network Patch Distribution Modeling (PaDiM) and two generative models (GANomaly and Denoising diffusion probabilistic models (DDPM)). We propose a preprocessing approach to deal with noisy and incomplete data points. We further improve the performance of PaDiM by using a weighted distance, assigning greater importance to features from deeper layers. The final framework was tested with five different volcanoes, which have different characteristics and its performance was compared against an existing supervised learning method for volcanic deformation detection. The experiments show that our final anomaly detection outperforms the supervised learning method, particularly where the characteristics of deformation are unknown. Our framework can thus be used to identify deformation at volcanoes without needing prior knowledge about the deformation patterns present there.</p>","PeriodicalId":54286,"journal":{"name":"Earth and Space Science","volume":"12 6","pages":""},"PeriodicalIF":2.9,"publicationDate":"2025-06-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024EA003892","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144256419","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
C. Godano, G. Petrillo, A. Tramelli, V. Convertito
{"title":"The \u0000 \u0000 \u0000 b\u0000 \u0000 $b$\u0000 -Value Tomography of the Calabrian Arc","authors":"C. Godano, G. Petrillo, A. Tramelli, V. Convertito","doi":"10.1029/2024EA004065","DOIUrl":"https://doi.org/10.1029/2024EA004065","url":null,"abstract":"<p>In the Calabrian Arc subduction zone, the notable lack of seismicity at depths near 100 km strongly suggests the presence of slab detachment. Contrary to typical patterns, where <span></span><math>\u0000 <semantics>\u0000 <mrow>\u0000 <mi>b</mi>\u0000 </mrow>\u0000 <annotation> $b$</annotation>\u0000 </semantics></math>-values decrease with depth, our b-value mapping reveals unexpectedly high <span></span><math>\u0000 <semantics>\u0000 <mrow>\u0000 <mi>b</mi>\u0000 </mrow>\u0000 <annotation> $b$</annotation>\u0000 </semantics></math>-values at these depths. Within the 100–150 km depth interval, the gradient of the <span></span><math>\u0000 <semantics>\u0000 <mrow>\u0000 <mi>b</mi>\u0000 </mrow>\u0000 <annotation> $b$</annotation>\u0000 </semantics></math>-value reaches its peak, indicating a significant reduction in stress. We propose four potential interpretations for these observations: (a) fluid-induced weakening due to dehydration processes, (b) heterogeneity at the slab tip reducing rupture propagation, (c) creeping zone behavior at the detachment tip, and (d) post-detachment damage to the rocks, leaving them unable to support stress. These hypotheses remain beyond experimental verification at present. This study underscores the complex interplay of geological processes at depth and their implications for seismic hazard assessment in subduction zones.</p>","PeriodicalId":54286,"journal":{"name":"Earth and Space Science","volume":"12 6","pages":""},"PeriodicalIF":2.9,"publicationDate":"2025-06-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024EA004065","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144244183","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}