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Seismic Petrophysical Inversion Guided by Rock Physics Modeling for Quantitative Estimation of Permeability and Gas Saturation in Volcanic Reservoirs 以岩石物理建模为指导的地震岩石物理反演定量估计火山岩储层渗透率和含气饱和度
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-14 DOI: 10.1007/s10712-026-09930-1
Yuedong Li, Zhiqi Guo, Cai Liu
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引用次数: 0
Recent Advances in 2D Frequency-Domain Marine Controlled-Source EM Inversion Using Adjoint Approximate Sensitivities 基于伴随近似灵敏度的二维频域海洋可控源电磁反演研究进展
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-14 DOI: 10.1007/s10712-025-09925-4
Gang Li, Yutao Liu, Octavio Castillo-Reyes
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引用次数: 0
Filtering Unevenly Spaced Geophysical Time Series as an Ill-Posed Problem 非均匀间隔地球物理时间序列的不适定问题滤波
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-13 DOI: 10.1007/s10712-025-09924-5
Kunpu Ji, Lin Zhang, Fengwei Wang
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引用次数: 0
Slabs and Plumes Beneath South America Revealed by Whole-Mantle Tomography 全地幔层析成像揭示的南美洲板块和地幔柱
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-13 DOI: 10.1007/s10712-025-09926-3
Genti Toyokuni, Dapeng Zhao
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引用次数: 0
A Unified Framework for Trend Uncertainty Assessment in Climate Data Records: Demonstration on Global Mean Sea Level 气候资料记录趋势不确定性评估的统一框架:全球平均海平面的论证
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-12 DOI: 10.1007/s10712-025-09922-7
Kevin Gobron, Roland Hohensinn, Xavier Loizeau, Claire E. Bulgin, Christopher J. Merchant, Emma R. Woolliams, Maurice G. Cox, Wouter Dorigo, Thomas Howard, Mary Langsdale, Adam C. Povey, Michaël Ablain, Janusz Bogusz, Alexander Gruber, Anna Klos, Jonathan Mittaz
{"title":"A Unified Framework for Trend Uncertainty Assessment in Climate Data Records: Demonstration on Global Mean Sea Level","authors":"Kevin Gobron, Roland Hohensinn, Xavier Loizeau, Claire E. Bulgin, Christopher J. Merchant, Emma R. Woolliams, Maurice G. Cox, Wouter Dorigo, Thomas Howard, Mary Langsdale, Adam C. Povey, Michaël Ablain, Janusz Bogusz, Alexander Gruber, Anna Klos, Jonathan Mittaz","doi":"10.1007/s10712-025-09922-7","DOIUrl":"https://doi.org/10.1007/s10712-025-09922-7","url":null,"abstract":"","PeriodicalId":49458,"journal":{"name":"Surveys in Geophysics","volume":"54 1","pages":""},"PeriodicalIF":4.6,"publicationDate":"2026-01-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145955810","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Error Covariance Structure Caused by Uncertainties in Atmospheric Correction for Optical Sensors 光学传感器大气校正中不确定性引起的误差协方差结构
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-12 DOI: 10.1007/s10712-025-09921-8
Simon Blessing, Ralf Giering
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引用次数: 0
Unconventional Three-Dimensional Active Seismic Tomography Applied in the Lousal Mine (Iberian Pyrite Belt, Portugal) 非常规三维活动地震层析成像在葡萄牙伊比利亚黄铁矿带Lousal矿中的应用
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-25 DOI: 10.1007/s10712-025-09920-9
Ines Hamak, Pedro Teixeira, José Borges, Ivan Koulakov, Rui Oliveira, Bento Caldeira, Mourad Bezzeghoud, João X. Matos, Sofia Andringa
The Lousal Mine (Iberian Pyrite Belt, Portugal) was operated from 1900 to 1988 for the extraction of massive sulphides and was later rehabilitated as a science museum. It was selected as a test site for underground muon tomography applied to geophysical surveys, as part of the LouMu project. This study focuses on seismic tomography to analyse the subsurface above the mine gallery, primarily surveyed by a muography telescope, which was developed specifically for this site by the Laboratory of Instrumentation and Experimental Particle Physics. To validate the muon tomography results, an initial approach using conventional 2D seismic refraction failed to reach the Waldemar gallery depth, due to limited seismic ray coverage. Therefore, an innovative setup using surface shots and in-gallery geophones was implemented, providing full ray coverage. A 3D velocity model was then produced using the ATOM3D code, which enabled the integration of this configuration and performed travel-time inversion for velocity calculation. A regional dextral strike-slip fault, the Corona Fault (CF), crosses the surveyed area, and served as the main focus of this investigation. The 3D velocity model successfully detected this structure, that corresponded to the boundary between positive anomalies of the Volcano-Sedimentary Complex (VSC) and negative anomalies of the Phyllite-Quartzite Group (PQG). The absolute velocity distribution showed a distinct offset around the Corona Fault (CF), indicating a dextral strike-slip mechanism. A subvertical extension of secondary faults was observed, reflecting deformation similar to that of the main tectonic context. Previous data from the gallery confirmed that these results are consistent with the known geology and can serve as a reference for the muon tomography interpretations.
卢萨尔矿(葡萄牙伊比利亚黄铁矿带)于1900年至1988年开采块状硫化物,后来恢复为科学博物馆。作为楼木工程的一部分,它被选为地下介子层析成像应用于地球物理调查的试验场。这项研究的重点是地震层析成像,以分析矿廊上方的地下,主要是通过仪器和实验粒子物理实验室专门为该地点开发的摄影望远镜进行调查。为了验证介子层析成像结果,由于地震射线覆盖范围有限,使用传统的二维地震折射的初始方法未能达到Waldemar走廊深度。因此,采用了表面拍摄和画廊内检波器的创新设置,提供了全射线覆盖。然后使用ATOM3D代码生成三维速度模型,该模型可以集成该配置,并对速度计算进行走时反演。一个区域右走滑断层,电晕断层(CF)穿过调查区域,成为本次调查的主要焦点。三维速度模型成功探测到该构造,该构造对应于火山-沉积杂岩(VSC)的正异常和千层岩-石英岩群(PQG)的负异常之间的边界。绝对速度分布在冕状断层周围有明显的偏移,表明其为右向走滑机制。观察到次级断裂的亚垂向伸展,反映了与主构造背景相似的变形。先前从画廊获得的数据证实,这些结果与已知的地质情况一致,可以作为介子断层扫描解释的参考。
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引用次数: 0
Challenges and Gaps in Understanding and Monitoring Low-Latitude F-region Plasma Irregularities 了解和监测低纬度f区等离子体不规则性的挑战和差距
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-10 DOI: 10.1007/s10712-025-09917-4
Astrid Maute, Tibor Durgonics, Joe Huba, Rayan Imam, Hanli Liu, Garima Malhotra, John Retterer, Claudia C. Stephan, Claudia Stolle, Endawoke Yizengaw
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引用次数: 0
Next-Generation Data Assimilation Methods for Polar Ionospheric Electrodynamics 极地电离层电动力学的下一代数据同化方法
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-09 DOI: 10.1007/s10712-025-09918-3
Karl M. Laundal, Aurélie Marchaudon, Astrid Maute, Spencer M. Hatch, Florine Enengl, Tomoko Matsuo, Margot Decotte, Michael Madelaire, Viacheslav G. Merkin, Anthony Sciola, Veronika Haberle, Andreas S. Skeidsvoll
Accurately specifying polar ionospheric electrodynamics is essential for understanding energy and momentum exchange between space and the upper atmosphere and for improving simulations of the ionosphere and the thermosphere. Statistical models are commonly used to provide input for global circulation models (GCMs). However, maps derived from simultaneous multi-instrument observations better represent the actual state of the system. Such maps integrate measurements from ground-based magnetometers and radars, in situ plasma and magnetic field sensors at low-Earth orbit, and optical and particle observations of auroral precipitation. However, ionospheric data assimilation remains in its early stages. Current methods rely on restrictive assumptions to simplify equations and stabilize inverse problems, but these constraints limit applicability beyond polar regions, hinder the inclusion of time-dependent processes, and prevent independent estimation of ionospheric conductance. This review examines the physical foundations of ionospheric data assimilation, evaluates the limitations of existing approaches, and explores pathways toward more accurate and flexible techniques. Specifically, we discuss approaches to: (1) use a common dataset to estimate conductance and fields in a single inversion; (2) incorporate neutral winds instead of assuming they are zero; (3) account for a realistic main magnetic field geometry instead of assuming radial field lines; (4) eliminate a sharp boundary between polar and low-latitude regions; (5) use F-region density measurements to capture the history of ionospheric conductance and plasma transport; (6) account for the magnetic field of ground-induced currents in a more realistic way; (7) include ionospheric induction effects to stabilize time-dependent inversions; and (8) couple ionospheric electrodynamics with global magnetosphere simulations to model the physics of time variations.
准确地确定极性电离层电动力学对于理解空间和高层大气之间的能量和动量交换以及改进电离层和热层的模拟至关重要。统计模式通常用于为全球环流模式(GCMs)提供输入。然而,由多仪器同时观测得到的地图更好地代表了系统的实际状态。这些地图综合了地面磁力计和雷达、近地轨道上的原位等离子体和磁场传感器以及极光降水的光学和粒子观测的测量结果。然而,电离层资料同化仍处于早期阶段。目前的方法依赖于限制性假设来简化方程和稳定反问题,但这些约束限制了极地以外地区的适用性,阻碍了时间相关过程的包含,并阻碍了电离层电导的独立估计。本文综述了电离层数据同化的物理基础,评估了现有方法的局限性,并探索了更准确和灵活的技术途径。具体来说,我们讨论了以下方法:(1)使用一个公共数据集来估计单次反演中的电导和场;(2)纳入中性风,而不是假设它们为零;(3)考虑真实的主磁场几何形状,而不是假设径向磁场线;(4)消除极地和低纬度地区之间的明显界限;(5)利用f区密度测量来捕捉电离层电导和等离子体输运的历史;(6)更真实地考虑地感应电流的磁场;(7)包括电离层感应效应,以稳定随时间变化的反演;(8)将电离层电动力学与全球磁层模拟相结合,模拟时间变化的物理特性。
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引用次数: 0
Perspectives and Challenges in High-Resolution Whole-Atmosphere Modeling 高分辨率全大气建模的前景与挑战
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-11-27 DOI: 10.1007/s10712-025-09915-6
Claudia Christine Stephan, Han-Li Liu, Huixin Liu, Xian Lu, Astrid Maute, Nicholas M. Pedatella, Valery A. Yudin
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引用次数: 0
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