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Comparative analysis of bias correction techniques for future climate assessment using CMIP6 hydrological variables for the Indian subcontinent 利用 CMIP6 水文变量对印度次大陆未来气候评估进行偏差修正技术比较分析
IF 2.3 4区 地球科学 Pub Date : 2024-06-28 DOI: 10.1007/s11600-024-01378-4
Meghal Shah, Amit Thakkar, Hiteshri Shastri

The study focuses on the bias correction of Coupled Model Intercomparison Project Phase 6 (CMIP6) hydrologic variables for the Indian region. The performance of two widely accepted bias correction methodologies, namely Quantile Mapping (QM) and Bias Correction Spatial Disaggregation (BCSD), is compared. The study undertakes to evaluate the application of these popular bias correction methodologies on four important hydrologic variables viz. precipitation, temperature, and surface wind. The QM methodology is employed and compared with BCSD based bias corrected variables obtained from NEX-GDDP-CMIP6 dataset. The selected GCM historical bias corrected climate variables using QM are compared with the NCEP reanalysis variables. The objective is to improve the reliability and accuracy of climate projections by minimizing biases present in the GCM outputs. Through a comprehensive comparative analysis, it is determined that QM exhibits superior performance in reducing biases when compared to BCSD. Thus, use of QM demonstrates higher efficacy by effectively capturing the statistical distribution characteristics of observed data and transferring them to the GCM outputs. The future climate change over the Indian region is observed for both QM and BCSD algorithms for SSP5-8.5, SSP2-4.5, and SSP1-2.6. The result emphasizes the importance of selecting an appropriate bias correction methodology to enhance the reliability of climate projections in the Indian region. Ultimately, the findings of this study contribute to the broader field of climate modeling and impact assessment, providing valuable insights into the selection and application of bias correction techniques for CMIP6 datasets in the Indian subcontinent region.

Graphical abstract

研究重点是印度地区耦合模式相互比较项目第 6 阶段(CMIP6)水文变量的偏差校正。研究比较了两种广为接受的偏差校正方法,即量子绘图法(QM)和偏差校正空间分解法(BCSD)。研究评估了这些流行的偏差校正方法在四个重要水文变量(即降水、温度和地表风)上的应用。采用了 QM 方法,并与从 NEX-GDDP-CMIP6 数据集获得的基于 BCSD 的偏差校正变量进行了比较。利用 QM 方法对选定的 GCM 历史偏差校正气候变量与 NCEP 再分析变量进行了比较。目的是通过尽量减少 GCM 输出中存在的偏差,提高气候预测的可靠性和准确性。通过综合比较分析,确定与 BCSD 相比,QM 在减少偏差方面表现出更优越的性能。因此,通过有效捕捉观测数据的统计分布特征并将其转移到 GCM 输出中,使用 QM 展示了更高的功效。在 SSP5-8.5、SSP2-4.5 和 SSP1-2.6 中,QM 算法和 BCSD 算法都能观测到印度地区未来的气候变化。该结果强调了选择适当的偏差校正方法对提高印度地区气候预测可靠性的重要性。最终,本研究的结果将为更广泛的气候建模和影响评估领域做出贡献,为印度次大陆地区 CMIP6 数据集的偏差校正技术的选择和应用提供有价值的见解。
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引用次数: 0
Scale effects and spatial distribution characteristics of 3D roughness of natural rock fracture surfaces: statistical analysis 天然岩石断裂面三维粗糙度的尺度效应和空间分布特征:统计分析
IF 2.3 4区 地球科学 Pub Date : 2024-06-25 DOI: 10.1007/s11600-024-01397-1
Jiuyang Huan, Mingming He, Zhiwen Wan, Meishu Li, Hengfei Pan, Mengdie Hu

The roughness feature of a natural rock fracture surface is an important factor affecting the shear and poromechanical behavior of rock. The scale effect and spatial distribution characteristics of the fracture surface roughness are notable challenges at rock engineering sites. In this article, morphological data of a large-scale field rock fracture surface were collected using a 3D scanner. Then, the original surface was divided into several small fracture surfaces. With the use of a 2D roughness statistical index, the 2D roughness (JRC2D) of the fracture profile was evaluated. The 3D roughness (JRC3D) of the fracture surface along different directions was obtained via the weighted averaging method. Based on four oblique analysis schemes, the elevation statistical trend and roughness scale effect of fracture surfaces with different widths were examined. With increasing fracture size, the average elevation ((mu)) and the standard deviation of elevation ((sigma)) showed different typical change patterns. The impact of size variation on the fracture surface roughness includes four types and exhibits significant anisotropy. Based on small fissure surfaces without mutual coverage, the spatial distribution characteristics of the fracture roughness were analyzed and were proven to exhibit high dispersion and anisotropy. With increasing width of the analyzed small fracture, the roughest position on the fracture surface basically remained the same, but there was a significant change in roughness anisotropy.

天然岩石断裂面的粗糙度特征是影响岩石剪切和孔隙力学行为的重要因素。断裂面粗糙度的尺度效应和空间分布特征是岩石工程现场面临的显著挑战。本文使用三维扫描仪采集了大规模野外岩石断裂面的形态数据。然后,将原始表面划分为多个小型断裂面。利用二维粗糙度统计指数,评估了断裂剖面的二维粗糙度(JRC2D)。通过加权平均法获得了断裂面沿不同方向的三维粗糙度(JRC3D)。基于四种斜面分析方案,研究了不同宽度断裂面的高程统计趋势和粗糙度尺度效应。随着断裂尺寸的增大,平均高程((mu))和高程标准偏差((sigma))呈现出不同的典型变化规律。尺寸变化对裂缝表面粗糙度的影响包括四种类型,并表现出明显的各向异性。基于无相互覆盖的小裂隙表面,分析了断裂粗糙度的空间分布特征,证明其具有较高的分散性和各向异性。随着所分析的小型断裂宽度的增加,断裂表面最粗糙的位置基本保持不变,但粗糙度各向异性发生了显著变化。
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引用次数: 0
Estimation of water saturation based on optimized models in tight gas sandstone reservoirs: a case study of Triassic Xujiahe Formation in northwestern Sichuan Basin 基于优化模型的致密气砂岩储层含水饱和度估算:四川盆地西北部三叠系徐家河地层案例研究
IF 2.3 4区 地球科学 Pub Date : 2024-06-25 DOI: 10.1007/s11600-024-01393-5
Xiaoyong Xia, Bing Han, Bing Xie, Qiang Lai, Yuexiang Wang, Shaowu Zhu

Water saturation estimation faced a great challenge in tight gas sandstone reservoirs because of the effect of pore structure and strong heterogeneity. The classic Archie’s equation cannot be always well used. To quantify the effect of pore structure to rock resistivity in tight gas sandstones, taking Triassic Xujiahe Formation of northwestern Sichuan Basin as an example, 35 core samples were recovered and applied for resistivity experiments in laboratory under the simulated formation temperature and pressure environment, and 18 of them were simultaneously applied for nuclear magnetic resonance (NMR) and high-pressure mercury injection experimental measurements. Relationships between pore structure and resistivity parameters were analyzed. The results clearly illustrated that cementation exponent (m) and saturation exponent (n) were heavily affected by pore structure. Rocks with superior pore structure contained relatively higher cementation exponent and lower saturation exponent, and vice versa. Afterward, we raised a parameter of pore size index, which was defined as the ratio of macropore and micro-pore percentage contents, to characterize rock pore structure, and established a model to calculate optimal saturation exponent from NMR data. Meanwhile, cementation exponent prediction model was also raised by combining with porosity and irreducible water saturation (Swirr). Combining with calculated cementation exponent and saturation exponent, we optimized the Archie’s equation to predict water saturation in our target tight gas sands. Field examples illustrated that the predicted cementation exponent and saturation exponent matched well with core-derived results. The absolute errors between predicted cementation exponent and saturation exponent with core-derived results were lower than 0.05 and 0.07, separately. By using optimized Archie’s equation, water saturations were precisely predicted from well logging data in our target tight gas sandstone reservoirs; whereas, the classic Archie’s equation underestimated formation water saturation.

由于孔隙结构和强烈异质性的影响,致密气砂岩储层的含水饱和度估算面临巨大挑战。经典的阿奇方程并不能一直很好地使用。为了量化孔隙结构对致密气砂岩岩石电阻率的影响,以四川盆地西北部三叠系徐家河地层为例,采集了 35 个岩心样品,在实验室模拟地层温度和压力环境下进行了电阻率实验,其中 18 个样品同时进行了核磁共振和高压注汞实验测量。分析了孔隙结构与电阻率参数之间的关系。结果清楚地表明,胶结指数(m)和饱和指数(n)受孔隙结构的影响很大。孔隙结构优越的岩石固结指数相对较高,饱和指数相对较低,反之亦然。随后,我们提高了孔隙度指数参数,将其定义为大孔隙与微孔的百分比含量之比,以表征岩石的孔隙结构,并建立了一个模型,根据核磁共振数据计算最佳饱和指数。同时,结合孔隙度和不可还原水饱和度(Swirr),提出了胶结指数预测模型。结合计算出的胶结指数和饱和指数,我们优化了阿奇方程,以预测目标致密气砂中的含水饱和度。现场实例表明,预测的胶结指数和饱和指数与岩心得出的结果非常吻合。预测的胶结指数和饱和指数与岩心衍生结果之间的绝对误差分别低于 0.05 和 0.07。通过使用优化的阿奇方程,可以根据测井数据精确预测目标致密气砂岩储层的含水饱和度;而传统的阿奇方程则低估了地层含水饱和度。
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引用次数: 0
Steady-state seepage through and below earthen dam under seismic condition: insights into hydrological mechanism 地震条件下土坝及其下方的稳态渗流:对水文机制的启示
IF 2.3 4区 地球科学 Pub Date : 2024-06-24 DOI: 10.1007/s11600-024-01391-7
Smita Tung, Sibapriya Mukherjee, Ankit Garg, Radha Tomar

Most of the studies in the literature focus on analyzing water flow within earthen dam under static condition. The objective of this study is to analyze water flow mechanisms within earthen dam under seismic condition. To achieve this purpose, a series of numerical simulations were conducted to model earthen embankment based on a real case scenario based on dam built in eastern province of India (i.e., South 24 Parganas in West Bengal). Further the effect of sheet pile as a seepage cutoff has been evaluated with variations in sheet pile length and location under steady-state settings for both static and seismic conditions. The study was carried out using FLAC2D version 5.0 and SEEP/W version 12.0 for a dam. The results show that pore pressure is high on the upstream side of the sheet pile during continuous seepage and quickly decreases along the sheet pile itself for all sheet pile positions. In seismic instances under steady-state conditions, when pore water pressure increases, the factor of safety decreases by 45% to 50% as compared to similar static cases. This is due to an increase in seepage force. As the sheet pile is cut off, the overall factor of safety increases as compared to the condition with no sheet pile. This study is though simplified; however, it provides insights into water flow pattern within earthen dam that need to be considered for preliminary design in regions, which are subjected to seismic loads.

文献中的大多数研究侧重于分析静态条件下土坝内的水流。本研究的目的是分析地震条件下土坝内的水流机制。为实现这一目的,我们进行了一系列数值模拟,以印度东部省份(即西孟加拉邦的南 24 Parganas)大坝的实际情况为基础,对土坝进行建模。此外,在静态和地震条件下的稳态设置中,随着钢板桩长度和位置的变化,还对钢板桩作为截渗层的效果进行了评估。这项研究是使用 FLAC2D 5.0 版和 SEEP/W 12.0 版对一座大坝进行的。结果表明,在连续渗流过程中,板桩上游侧的孔隙压力较高,而在所有板桩位置,孔隙压力都会沿着板桩本身迅速降低。在稳态条件下的地震实例中,当孔隙水压力增加时,安全系数与类似的静态情况相比会降低 45% 至 50%。这是由于渗流力增加所致。当钢板桩被切断时,与没有钢板桩的情况相比,整体安全系数会增加。这项研究虽然比较简单,但它提供了土坝内水流模式的见解,在承受地震荷载的地区进行初步设计时需要考虑这些见解。
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引用次数: 0
Interactive analysis of the results of NET-VISA, a Bayesian inference system, in CTBTO’s International Data Centre bulletin production 在禁核试组织国际数据中心的公报中对贝叶斯推理系统 NET-VISA 的结果进行互动分析
IF 2.3 4区 地球科学 Pub Date : 2024-06-22 DOI: 10.1007/s11600-024-01398-0
Sherif Mohamed Ali, Ehsan Qorbani, Ronan Le Bras, Gérard Rambolamanana

The Global Association model is a crucial tool in seismic data analysis at the International Data Centre (IDC) of the Comprehensive Nuclear-Test-Ban Treaty Organization. However, it faces challenges due to its limitations in accurately associating seismic events on a global scale. Over the past years, attempts have been undertaken to tackle these issues by introducing the Network Processing Vertically Integrated Seismic Analysis (NET-VISA) algorithm, specifically designed to enhance seismic event association across the globe. NET-VISA uses a machine learning Bayesian approach to solve the automatic association problem. NET-VISA has been implemented in operation as an additional automatic event scanner tool since January 2018. In this study, we assess the effect of the NET-VISA automatic scanner on the IDC output REB and LEB bulletins. We used three distinct time periods to evaluate the NET-VISA performance. The results show a 4.6% increase in the number of LEB events after including the NET-VISA scanner in operation, with an average of 7 additional events per day, and an increase of 17.90% in the number of scanned events. A comparison between the different bulletins in distinct periods shows NET-VISA is beneficial to build more valid events, providing opportunities to improve nuclear-test-ban monitoring. However, NET-VISA exhibits slightly reduced performance for events occurring at depths exceeding 300 km.

全球关联模型是全面禁止核试验条约组织国际数据中心(IDC)进行地震数据分析的重要工具。然而,由于其在全球范围内准确关联地震事件方面的局限性,它面临着挑战。在过去几年中,为解决这些问题,人们尝试引入网络处理垂直整合地震分析(NET-VISA)算法,该算法专门用于加强全球范围内的地震事件关联。NET-VISA 采用机器学习贝叶斯方法解决自动关联问题。自 2018 年 1 月起,NET-VISA 已作为额外的自动事件扫描工具投入使用。在本研究中,我们评估了 NET-VISA 自动扫描仪对 IDC 输出 REB 和 LEB 公告的影响。我们使用了三个不同的时间段来评估 NET-VISA 的性能。结果显示,加入 NET-VISA 扫描仪后,LEB 事件的数量增加了 4.6%,平均每天增加 7 个事件,扫描事件的数量增加了 17.90%。不同时期不同公告之间的比较显示,NET-VISA 有利于建立更多的有效事件,为改进核试验禁令监测提供了机会。不过,对于发生在深度超过 300 公里的事件,NET-VISA 的性能略有下降。
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引用次数: 0
Application of pseudo-3D sub-bottom profile imaging technology in small submarine target detection 伪三维海底剖面成像技术在小型潜艇目标探测中的应用
IF 2.3 4区 地球科学 Pub Date : 2024-06-22 DOI: 10.1007/s11600-024-01343-1
Tianguang Li, Zhiqing Huang, Xiaobo Zhang, Fansheng Meng, Yifan Pei, Jiali Guo

The sub-bottom profiler is a valuable tool for obtaining high-resolution shallow stratigraphic data in marine geological and geophysical surveys. To detect and acquire the structural characteristics of small submarine objects, we developed a data processing method that utilizes 2D data to construct a 3D structural model. We conducted application experiments using sub-bottom profile detection data from Chuanshan Islands, which were explored using China’s most advanced unmanned exploration platform and commercial shallow formation profiling system. To create high-resolution 3D seafloor structure models from recorded 2D sub-bottom profile datasets, an optimized data processing sequence was devised, comprising two stages: 2D data processing and 3D data processing. The 2D data processing stage involved spectrum analysis, band-pass filtering, matching filtering, time-varying gain, and surge correction. The subsequent 3D data processing stage encompassed ping location reallocation, static correction, and extraction of feature layer information. Notably, the final pseudo-3D sub-bottom profile time slice exhibited significant amplitude variations near the target body. This methodology represents an extension of the application of 2D sub-bottom profile data, enhancing the target recognition capabilities of such data. To further improve the precision of target body characterization, we used ArcScene 10.0 to create a 3D sub-bottom profile formation model spatial database. We constructed a submarine 3D formation structure model to show the 3D structural characteristics of the target body in detail and identified a seabed target body measuring 6.4 × 9.2 × 10 m.

在海洋地质和地球物理勘测中,海底剖面仪是获取高分辨率浅地层数据的重要工具。为了探测和获取小型海底物体的结构特征,我们开发了一种利用二维数据构建三维结构模型的数据处理方法。我们利用川山列岛的海底剖面探测数据进行了应用实验,这些数据是利用中国最先进的无人勘探平台和商用浅层剖面探测系统进行探测的。为了从记录的二维海底剖面数据集创建高分辨率的三维海底结构模型,我们设计了一套优化的数据处理序列,包括两个阶段:二维数据处理和三维数据处理。二维数据处理阶段包括频谱分析、带通滤波、匹配滤波、时变增益和浪涌校正。随后的三维数据处理阶段包括 ping 位置重新分配、静态校正和提取特征层信息。值得注意的是,最终的伪三维海底剖面时间切片在目标体附近表现出明显的振幅变化。该方法是二维海底剖面数据应用的延伸,增强了此类数据的目标识别能力。为了进一步提高目标体特征描述的精度,我们使用 ArcScene 10.0 创建了三维海底剖面结构模型空间数据库。我们构建了海底三维地层结构模型,详细展示了目标体的三维结构特征,并识别出了一个面积为 6.4 × 9.2 × 10 米的海底目标体。
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引用次数: 0
Machine learning-based seismic characterization of deepwater turbidites in the Dangerous Grounds area, Northwest Sabah, offshore Malaysia 基于机器学习的马来西亚近海沙巴西北部危险地区深水浊积岩地震特征描述
IF 2.3 4区 地球科学 Pub Date : 2024-06-22 DOI: 10.1007/s11600-024-01396-2
Ismailalwali Babikir, Mohamed Elsaadany

Seismic interpretation is a critical aspect of hydrocarbon exploration, where geoscientists often struggle to accurately recognize patterns and anomalies in large datasets. Machine learning techniques offer a promising solution by allowing for the quick and accurate analysis of multiple and large-size seismic volumes. This study leverages seismic facies analysis, seismic attribute analysis, and supervised machine learning to identify and characterize turbidite deposits in the Dangerous Grounds region, an underexplored area recently revealed by high-resolution broadband seismic data. Through seismic stratigraphy, two distinct phases of turbidite deposition were identified: a lower unit showing higher amplitude and signs of faulting effect, and an upper, present-day unit characterized by lower amplitude and continuous reflectors. The attribute expression of these turbidites shows strong amplitude response, high relative acoustic impedance, and high gray-level co-occurrence matrix entropy emphasizing their distinctiveness from surrounding facies, with variations in reflector continuity and spectral decomposition providing further insight into their depositional processes and sediment characteristics. By applying nine machine learning classifiers with twenty seismic attributes as input, this study achieved over 99% accuracy in distinguishing turbidite facies from background, with the neural network, random forest, K-nearest neighbors, decision tree, and support vector machine exhibiting optimal performance. The study contributes significantly to the regional understanding of turbidite deposits through detailed machine learning-aided seismic characterization. It underscores the value of integrating domain knowledge with machine learning techniques in enhancing subsurface interpretations, offering a comprehensive methodology for seismic facies analysis in similarly complex and underexplored regions.

地震解释是碳氢化合物勘探的一个重要方面,地球科学家往往难以准确识别大型数据集中的模式和异常。机器学习技术能够快速准确地分析多个大型地震数据集,是一种很有前景的解决方案。本研究利用地震剖面分析、地震属性分析和有监督的机器学习来识别和描述危险地层地区的浊积岩矿床,这是最近由高分辨率宽带地震数据揭示的一个未充分勘探的地区。通过地震地层学,确定了浊积岩沉积的两个不同阶段:一个是振幅较高且有断层效应迹象的下部单元,另一个是振幅较低且有连续反射体的上部单元,即现在的单元。这些浊积岩的属性表达显示出较强的振幅响应、较高的相对声阻抗和较高的灰度共现矩阵熵,强调了它们与周围岩层的区别,而反射体连续性和频谱分解的变化则进一步揭示了它们的沉积过程和沉积特征。该研究以 20 个地震属性为输入,应用九种机器学习分类器,在区分浊积岩面与背景方面的准确率超过 99%,其中神经网络、随机森林、K-近邻、决策树和支持向量机表现最佳。这项研究通过详细的机器学习辅助地震特征描述,极大地促进了区域对浊积岩沉积的理解。该研究强调了将领域知识与机器学习技术相结合以增强地下解释的价值,为类似复杂和未充分勘探地区的地震剖面分析提供了一种全面的方法。
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引用次数: 0
Azimuthal crustal variations and their implications on the seismic impulse response in the Valley of Mexico 地壳方位角变化及其对墨西哥谷地震脉冲响应的影响
IF 2.3 4区 地球科学 Pub Date : 2024-06-19 DOI: 10.1007/s11600-024-01383-7
Manuel J. Aguilar-Velázquez, Xyoli Pérez-Campos, Josué Tago, Carlos Villafuerte

Previous studies have suggested prominent variations in the seismic wave behavior at the 5 s period when traveling across the Valley of Mexico, associating them with the crustal structure and contributing to the anomalous seismic wave patterns observed each time an earthquake hits Mexico City. This article confirms the variations observed at 0.2 Hz by analyzing the Green tensor diagonal retrieved from empirical Green functions (EGF) calculated using seismic noise data cross-correlations of the vertical and horizontal components. We observe time and phase shifts between the east and north EGF components and show that they can be explained by the crustal structure from the surface up to 20 km depth; we also observe that the time and phase shifts are more significant if the distance between the source and the station increases. Additionally, the article presents an updated version of the velocity model from receiver functions and dispersion curves (VMRFDC v2.0) for the crustal structure under the Valley of Mexico. To validate this model, we compare the EGFs with synthetic Green functions determined numerically. To do so, we adaptatively meshed this model using an iterative algorithm to numerically simulate the impulse response up to 0.5 Hz. Finally, the comparisons between noise and synthetic EGF showed that the VMRFDC v2.0 model explains the time shifts and phase differences at 0.2 Hz, previously observed by independent studies, suggesting it correctly characterizes the crustal structure anomalies beneath the Valley of Mexico.

之前的研究表明,地震波在穿越墨西哥谷时,5 秒周期的地震波行为存在明显变化,这与地壳结构有关,也是每次墨西哥城地震时观测到的异常地震波模式的原因。本文通过分析利用地震噪声数据垂直和水平分量的交叉相关性计算出的经验格林函数(EGF)检索出的格林张量对角线,证实了在 0.2 Hz 处观察到的变化。我们观察到东面和北面 EGF 分量之间的时间和相位偏移,并表明它们可以用地表至 20 千米深度的地壳结构来解释;我们还观察到,如果震源和台站之间的距离增加,时间和相位偏移会更明显。此外,文章还介绍了针对墨西哥谷地下地壳结构的最新版接收函数和频散曲线速度模型(VMRFDC v2.0)。为了验证这一模型,我们将 EGF 与数值确定的合成格林函数进行了比较。为此,我们使用迭代算法对该模型进行了自适应网格划分,以数值模拟高达 0.5 Hz 的脉冲响应。最后,噪声与合成 EGF 的比较表明,VMRFDC v2.0 模型解释了之前独立研究观察到的 0.2 Hz 时移和相位差,表明它正确描述了墨西哥谷地下地壳结构异常的特征。
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引用次数: 0
Volcanic disaster scene classification of remote sensing image based on deep multi-instance network 基于深度多实例网络的遥感图像火山灾害场景分类
IF 2.3 4区 地球科学 Pub Date : 2024-06-18 DOI: 10.1007/s11600-024-01394-4
Chengfan Li, Jingxin Han, Chengzhi Wu, Lan Liu, Xuefeng Liu, Junjuan Zhao

Due to the varieties, random distributions, and rich visual characteristics of the volcanic disaster scene, traditional methods fail to fully express the complex features of volcanic disaster scenes in remote sensing images. To tackle this problem, a new multi-instance network framework with the Shift Windows Transformer (i.e., Swin-T) and attention mechanism is used to classify the volcanic disaster scene from remote sensing images (MI-STA). Firstly, via aggregating the global contextual information of remote sensing image features, the Swin-T extracts the multi-scale hierarchical features of volcano disaster scenes from remote sensing images. Secondly, the channel attention module and spatial attention module fuse to extract the features of volcanic disaster scene to enhance the description and representation for the local details and global information in volcanic disaster scenes. Last, the importance weight of different example characteristics is scored to calculate the attributive probabilities of each instance. This study elaborates an experiment on the xBD dataset and gives comparisons with the commonly used deep network models. The results show that the overall classification accuracy of the proposed method achieves 92.46% and has good performance on the test dataset. Then, we further utilize our model to classify the volcanic disaster scenes of the specific Hunga Tonga-Hunga Ha’apai on January 15, 2022, and the classification images have good consistency with the existing literature. It provides a new approach for volcanic disaster monitoring by means of remote sensing image and has broad application prospects.

由于火山灾害场景的多样性、随机分布和丰富的视觉特征,传统方法无法充分表达遥感图像中火山灾害场景的复杂特征。针对这一问题,我们采用了一种新的多实例网络框架,利用移窗变换器(即 Swin-T)和注意力机制对遥感图像中的火山灾害场景进行分类(MI-STA)。首先,Swin-T 通过聚合遥感图像特征的全局上下文信息,从遥感图像中提取火山灾害场景的多尺度分层特征。其次,融合通道关注模块和空间关注模块提取火山灾害场景特征,增强对火山灾害场景局部细节和全局信息的描述和表示。最后,对不同实例特征的重要性权重进行评分,计算出每个实例的归因概率。本研究详细阐述了在 xBD 数据集上进行的实验,并与常用的深度网络模型进行了比较。结果表明,所提方法的整体分类准确率达到了 92.46%,在测试数据集上具有良好的表现。随后,我们进一步利用模型对2022年1月15日洪加汤加-洪加哈帕伊特定火山灾害场景进行了分类,分类图像与现有文献具有良好的一致性。它为利用遥感图像进行火山灾害监测提供了一种新的方法,具有广阔的应用前景。
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引用次数: 0
Completeness and calibration of the Italian Seismological Instrumental and Parametric Database (ISIDe) before 16 April 2005 2005 年 4 月 16 日之前意大利地震仪器和参数数据库(ISIDe)的完整性和校准
IF 2.3 4区 地球科学 Pub Date : 2024-06-18 DOI: 10.1007/s11600-024-01395-3
Barbara Lolli, Gianfranco Vannucci, Paolo Gasperini

The Italian Seismological Instrumental and Parametric Database (ISIDe) is the recipient of earthquake data collected in real-time by the Istituto Nazionale di Geofisica e Vulcanologia (INGV), and used by the studies of earthquake forecasting and seismic hazard assessment in Italy in the last decade. When it went online, following a significant improvement of the seismic acquisition system of INGV, it was including only data since the second fortnight of April 2005. About ten years later, the data since the beginning of 1985 suddenly appeared without any prior notice than the updating of the starting date of the dataset. However, the characteristics of the added data appeared clearly different from the following period both in terms of the numbers of located earthquakes and of types of magnitudes provided. After having analyzed the numerical consistency and the calibration of magnitudes of ISIDe as a function of time from 1985 to 15 April 2005, we can say that such a dataset is incomplete and poorly calibrated compared to other catalogs of Italian seismicity (CSTI, CSI, and HORUS) available for the same period. Hence, we suggest not using it as is for statistical analyses of Italian seismicity. However, it provides some magnitudes that are missed by other catalogs and thus might be used for improving such catalogs.

意大利地震仪器和参数数据库(ISIDe)是意大利国家地球物理和火山研究所(INGV)实时收集的地震数据的接收者,在过去十年中被用于意大利的地震预报和地震灾害评估研究。随着 INGV 地震采集系统的重大改进,该系统上线时仅包括 2005 年 4 月第二个双周以来的数据。大约十年后,1985 年初以来的数据突然出现,除了更新数据集的起始日期外,没有任何事先通知。然而,新增数据的特征在地震定位数量和提供的震级类型方面都明显不同于随后的时期。在分析了从 1985 年到 2005 年 4 月 15 日 ISIDe 的数字一致性和震级校准随时间变化的函数之后,我们可以说,与同期的其他意大利地震目录(CSTI、CSI 和 HORUS)相比,该数据集是不完整的,校准也很差。因此,我们建议不要将其用于意大利地震的统计分析。不过,它提供了一些其他地震目录所遗漏的震级,因此可用于改进这些地震目录。
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Acta Geophysica
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