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A hybrid physics-informed and data-driven model for estimating ocean internal wave phase speeds from remote sensing imagery 从遥感图像估计海洋内波相速的混合物理信息和数据驱动模型
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-29 DOI: 10.1016/j.rse.2026.115247
Guangxi Cui , Zhongya Cai , Zhiqiang Liu
The propagation speed of internal waves is a fundamental parameter for understanding their physical mechanisms, dynamic behavior, and environmental impact. However, traditional estimation methods are typically based on numerical simulations or sparse in-situ observations, which limit their accuracy and scalability, and results in a significant scarcity of available phase speed datasets. To overcome these challenges, we propose a physics-informed and data-driven model for estimating internal wave phase speed from satellite imagery. The proposed model incorporates three key innovations: (1) the integration of theoretical equations (KdV, BO, and eKdV equations) as physical constraints to ensure consistency with real-world ocean dynamics; (2) the adoption of an adaptive ensemble learning framework that fuses data-driven and physical-informed features to improve model robustness and prediction accuracy; and (3) the introduction of a transfer learning strategy to mitigate discrepancies between theoretical predictions and observational real-world internal wave results. Experimental results demonstrate that the model achieves superior performance across varying water depths, with an average RMSE of 0.04 m/s, MRE of 2.5%, and R2 of 98.8% on the testing set. Additionally, the model was applied to the South China Sea, revealing a distinct propagation pattern: average phase speed initially increased (from 2.427 m/s to 2.53 m/s), then decreased (to 1.464 m/s), and subsequently increased again (to 1.703 m/s) as internal waves propagated westward across the Dongsha Islands and Hainan Island. The model was further validated on a global scale, achieving an average percentage error of 4.95%, confirming its scalability and generalization capability. This study presents an efficient and automated approach for accurately retrieving internal wave phase speed.
内波的传播速度是了解其物理机制、动态行为和环境影响的基本参数。然而,传统的估计方法通常基于数值模拟或稀疏的原位观测,这限制了它们的准确性和可扩展性,并且导致可用的相位速度数据集严重缺乏。为了克服这些挑战,我们提出了一个物理信息和数据驱动的模型,用于从卫星图像估计内波相速度。提出的模型包含三个关键创新:(1)将理论方程(KdV、BO和eKdV方程)作为物理约束的集成,以确保与真实海洋动力学的一致性;(2)采用融合数据驱动和物理信息特征的自适应集成学习框架,提高模型的鲁棒性和预测精度;(3)引入迁移学习策略来缓解理论预测与实际观测结果之间的差异。实验结果表明,该模型在不同水深下均取得了较好的性能,在测试集上平均RMSE为0.04 m/s, MRE为2.5%,R2为98.8%。此外,将该模型应用于南海,显示出明显的传播模式:内波在东沙群岛和海南岛向西传播时,平均相速先增加(从2.427 m/s到2.53 m/s),然后减小(到1.464 m/s),随后又增加(到1.703 m/s)。进一步在全球尺度上对模型进行了验证,平均百分比误差为4.95%,验证了模型的可扩展性和泛化能力。本研究提出了一种高效、自动化的内波相速精确检索方法。
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引用次数: 0
TIDA-SR: A time-conditioned deformable attention network for DEM super-resolution in cloud-covered mountainous regions 云覆盖山区DEM超分辨率的时间条件形变关注网络
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-29 DOI: 10.1016/j.rse.2026.115254
Kai Chen , Fayuan Li , Sijin Li , Haoyu Cao , Wen Dai , Guoan Tang
The complex terrain and variable climatic conditions in mountainous regions often cause cloud and fog occlusions, which hinder the generation of high-resolution Digital Elevation Models (DEMs) (below 10 m) using optical satellite photogrammetry. To address the issues of insufficient accuracy and data gaps in cloud-affected DEM areas, this study proposes a Time-Conditioned Deformable Convolution Attention Super-Resolution Network (TIDA-SR). The network performs super-resolution reconstruction using open-source DEMs and integrates multiple DEM sources through a feathered blending strategy to achieve high-accuracy results. Its architecture incorporates a diffusion process, deformable convolutions, and a Convolutional Block Attention Module (CBAM), combined with a composite loss function, to enhance the recovery of complex terrain details. TIDA-SR network, combined with the cloud-affected 5 m DEMs generated from GF-7 stereo imagery and open-source 30 m DEMs, is employed to reconstruct and fuse cloud-affected regions with 5 m resolution. The experimental results in the Loess Plateau and the Rocky Mountains demonstrate that, compared with traditional interpolation methods and existing deep learning approaches, TIDA-SR reduces RMSE and MAE by approximately 5%–78% on the validation dataset and by 3%–25% on the open-source DEM dataset. Slope accuracy improvements of approximately 3%–42% on the validation dataset and 3%–8% on the open-source DEM dataset are observed. The feathered blending strategy effectively mitigates stitching artifacts between cloud and noncloud areas, enhancing overall spatial continuity. TIDA-SR exhibits superior performance in high-resolution DEM reconstruction for cloud-affected mountainous regions and shows strong potential for practical applications, including surface process simulations, mountain hydrological modeling, geomorphological analysis, and other terrain-driven geoscience tasks.
山区复杂的地形和多变的气候条件经常造成云雾遮挡,阻碍了利用光学卫星摄影测量技术生成高分辨率数字高程模型(dem)(低于10 m)。为了解决受云影响的DEM区域精度不足和数据缺口的问题,本研究提出了一种时间条件形变卷积注意超分辨率网络(TIDA-SR)。该网络使用开源DEM进行超分辨率重建,并通过羽状混合策略集成多个DEM源,以获得高精度结果。其架构包含扩散过程、可变形卷积和卷积块注意模块(CBAM),并结合复合损失函数,以增强复杂地形细节的恢复。利用TIDA-SR网络,结合GF-7立体影像生成的受云影响的5 m dem和开源的30 m dem,对5 m分辨率的云影响区域进行重建和融合。在黄土高原和落基山脉的实验结果表明,与传统插值方法和现有深度学习方法相比,在验证数据集上,TIDA-SR的RMSE和MAE降低了约5% ~ 78%,在开源DEM数据集上降低了3% ~ 25%。在验证数据集上,坡度精度提高了约3%-42%,在开源DEM数据集上,坡度精度提高了3%-8%。羽状混合策略有效地减轻了云和非云区域之间的拼接伪影,增强了整体空间的连续性。TIDA-SR在云影响山区的高分辨率DEM重建中表现出优异的性能,并显示出强大的实际应用潜力,包括地表过程模拟、山地水文建模、地貌分析和其他地形驱动的地球科学任务。
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引用次数: 0
InSAR analysis using both co- and cross-polarized data at Death Valley, California from 2017–2025 2017-2025年加利福尼亚死亡谷共极化和交叉极化数据的InSAR分析
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-29 DOI: 10.1016/j.rse.2026.115265
Olivia Paschall, Rowena Benfer Lohman
The Sentinel-1 satellite mission has been key to the achievement of interferometric synthetic aperture radar (InSAR)-based displacement rates that approach mm/yr precision, particularly in regions without significant vegetation and where long time series of observations exist. However, for more subtle displacement signals, separating the effects of surface processes from deformation due to deeper sources is still challenging. Here, we present a new method based on combinations of co-polarized (VV) and cross-polarized (VH) InSAR data. Cross-polarized data is typically noisier than the co-polarized data and are not widely used for InSAR. However, comparisons of co- and cross-polarized phase data can allow separation of the contributions from different processes. Signals due to deeper sources, such as slip along faults, should appear the same in both data types, while differences can be due to changes in surface characteristics. We examine full-resolution, unfiltered, VV and VH Sentinel-1 data covering Death Valley, California between January 2017 and March 2025. We find that displacement rates derived from VV and VH data differ by several mm/yr in some areas. We also show that rates based only on the VV imagery differ by a few mm/yr between subsets of pixels where the VV-VH differences are large or small, suggesting that VV-VH combinations can help researchers reliably identify pixels that are the least impacted by surface processes. While our work focuses on Death Valley, similar mm/yr-scale biases could impact endorheic basins around the world and influence analyses of interseismic motion, hazard estimates, and groundwater studies.
Sentinel-1卫星任务是实现基于干涉合成孔径雷达(InSAR)的位移率接近毫米/年精度的关键,特别是在没有显著植被和存在长时间观测序列的地区。然而,对于更细微的位移信号,将地表过程的影响与深层源引起的变形区分开来仍然具有挑战性。本文提出了一种基于共极化(VV)和交叉极化(VH) InSAR数据组合的新方法。交叉极化数据通常比共极化数据噪声更大,因此不广泛用于InSAR。然而,共极化和交叉极化相数据的比较可以允许从不同过程的贡献分离。深层来源(如断层滑动)产生的信号在两种数据类型中应该是相同的,而差异可能是由于地表特征的变化造成的。我们研究了2017年1月至2025年3月期间覆盖加州死亡谷的全分辨率、未过滤、VV和VH Sentinel-1数据。我们发现,在某些地区,由VV和VH数据得出的位移率相差几毫米/年。我们还表明,在VV- vh差异大或小的像素子集之间,仅基于VV图像的速率差异仅为几毫米/年,这表明VV- vh组合可以帮助研究人员可靠地识别受表面过程影响最小的像素。虽然我们的工作主要集中在死亡谷,但类似的毫米/年尺度偏差可能会影响世界各地的内河盆地,并影响地震间运动的分析、危害估计和地下水研究。
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引用次数: 0
Enhancing two-week live fuel moisture content forecasts through biophysical modelling and remote sensing data assimilation 通过生物物理建模和遥感数据同化增强两周活燃料水分含量预报
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-28 DOI: 10.1016/j.rse.2026.115267
Qinglong Jia , Xingwen Quan , Víctor Resco de Dios , Marta Yebra , Binbin He , Xing Li , Zhanmang Liao , Rodrigo Balaguer-Romano , Miquel De Cáceres
Live Fuel Moisture Content (LFMC) is a critical determinant of wildfire ignition and spread. Accurate forecasting of LFMC dynamics, particularly at a two-week timescale, is essential for early wildfire danger assessment. While satellite remote sensing provides valuable current and historical observations, it lacks the ability to predict future LFMC dynamics. Meanwhile, although weather forecasts are relatively reliable over short timescales (up to two weeks), LFMC models based solely on meteorological inputs often fall short, particularly when predicting conditions at the species level. To address these limitations, this study introduces a species-specific approach that integrates MODIS-derived LFMC data into the biophysical process-based MEDFATE model to optimize LFMC simulations and enable short-term forecasting based on daily weather projections. A global sensitivity analysis was conducted to identify key input parameters for different tree species within MEDFATE. These parameters guided the development of a cost function that quantifies discrepancies between model-simulated and field-measured LFMC, enabling species-specific model calibration. To enhance model optimization, the global optimal DEoptim algorithm was combined with four-dimensional variational data assimilation (4D-Var) to integrate MODIS-derived LFMC estimates into MEDFATE. Using weather projections, the optimized MEDFATE model produced LFMC forecasts at about a two-week timescale. Time-series measurements of LFMC dynamics for Quercus faginea, Quercus ilex, and Pinus halepensis in Spain, Pinus ponderosa in the USA, and Eucalyptus species in Australia demonstrated that model calibration improved daily LFMC estimates (R2 increased from 0.22 to 0.31; RMSE reduced from 18.71% to 16.04%). Further incorporation of MODIS-derived LFMC data significantly enhanced accuracy (R2 = 0.56; RMSE = 9.75%). Validation across seven wildfire events in Spain, Australia, and the USA confirmed the effectiveness and operational relevance of the approach for early fire warning. These findings underscore the potential of integrating satellite remote sensing and meteorological data into biophysical process-based models to improve tree species-specific LFMC prediction and support proactive fire management.
活燃料含水率(LFMC)是野火着火和蔓延的关键决定因素。准确预测LFMC动态,特别是在两周的时间尺度上,对早期野火危险评估至关重要。虽然卫星遥感提供了有价值的当前和历史观测,但它缺乏预测未来LFMC动态的能力。与此同时,尽管天气预报在短时间尺度(最多两周)内相对可靠,但仅基于气象输入的LFMC模式往往不足,特别是在预测物种水平的条件时。为了解决这些局限性,本研究引入了一种物种特异性方法,将modis衍生的LFMC数据整合到基于生物物理过程的MEDFATE模型中,以优化LFMC模拟并实现基于日常天气预测的短期预报。通过全局敏感性分析,确定MEDFATE中不同树种的关键输入参数。这些参数指导成本函数的发展,量化模型模拟和现场测量的LFMC之间的差异,从而实现特定物种的模型校准。为了加强模型的优化,将全局最优DEoptim算法与四维变分数据同化(4D-Var)相结合,将modis导出的LFMC估计整合到MEDFATE中。利用天气预测,优化的MEDFATE模型在大约两周的时间尺度上产生了LFMC预测。对西班牙麻栎(Quercus faginea)、冬青栎(Quercus ilex)和halepensis、美国黄松(Pinus ponderosa)和澳大利亚桉树(Eucalyptus)的LFMC动态进行的时间序列测量表明,模型校准提高了LFMC的日估算值(R2从0.22增加到0.31,RMSE从18.71%降低到16.04%)。进一步纳入modis衍生的LFMC数据显著提高了准确性(R2 = 0.56; RMSE = 9.75%)。在西班牙、澳大利亚和美国的七个野火事件中进行的验证证实了该方法在早期火灾预警中的有效性和操作相关性。这些发现强调了将卫星遥感和气象数据整合到基于生物物理过程的模型中,以改进特定树种的LFMC预测并支持主动火灾管理的潜力。
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引用次数: 0
Characterizing diurnal variability in power plant carbon emissions in Asia: A top-down estimation approach constrained by geostationary NO2 and OCO-3 CO2 observations 亚洲电厂碳排放的日变化特征:受地球静止NO2和OCO-3 CO2观测约束的自上而下估算方法
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-27 DOI: 10.1016/j.rse.2026.115261
Tianyi Xu , Chengxin Zhang , Cheng Liu
Accurate quantification of carbon dioxide emissions is crucial for addressing climate change. However, traditional top-down CO2 estimates are limited by sparse satellite observations and coarse temporal resolution. Although NO2 data from polar-orbiting satellites can help constrain CO2 emissions, temporal mismatch with OCO-3 measurements introduce additional uncertainty. To address this, we estimate hourly CO2 emissions by combining OCO-3 XCO2 observations with high temporal resolution NO2 data from the GEMS instrument onboard the GEO-KOMPSAT-2B satellite. We developed an algorithm based on a Gaussian plume model and wind rotation techniques to estimate CO2 emissions and NOx/CO2 emission ratios from near-synchronous NO2/CO2 observations. Hourly CO2 emissions were further derived using GEMS-based NOx emissions estimated via the flux divergence method. A total of 59 power plant cases across six Asian countries were identified. For these cases, the estimated CO2 emissions exhibit distinct diurnal, seasonal, and interannual emission variability, primarily driven by heating demand, decarbonization measures, and pandemic-related industrial slowdowns. These top-down estimates, constrained by GEMS NO2 data, show strong consistency with bottom-up inventories (R = 0.89), supporting the validity of our optimization approach. Furthermore, comparisons with daytime mean estimates suggest that CO2 emission estimates constrained by polar-orbiting satellite observations can exhibit biases of approximately 60% relative to GEO-based approaches, underscoring the importance for high-temporal-resolution measurements. This study highlights the value of integrating geostationary NO2 and CO2 observations to capture the diurnal dynamics of power plant emissions and improve the accuracy of top-down CO2 emission monitoring.
准确量化二氧化碳排放量对于应对气候变化至关重要。然而,传统的自上而下的CO2估算受到稀疏的卫星观测和粗糙的时间分辨率的限制。虽然极轨卫星的二氧化氮数据有助于限制二氧化碳排放,但与OCO-3测量值的时间不匹配带来了额外的不确定性。为了解决这个问题,我们将OCO-3 XCO2观测数据与GEO-KOMPSAT-2B卫星上的GEMS仪器的高时间分辨率NO2数据结合起来估算每小时CO2排放量。我们开发了一种基于高斯羽流模型和风旋转技术的算法,从近同步的NO2/CO2观测数据中估计CO2排放量和NOx/CO2排放比。利用通量发散法估算的基于gems的氮氧化物排放量,进一步推导出每小时的二氧化碳排放量。在6个亚洲国家共发现了59个电厂病例。在这些情况下,估计的二氧化碳排放量表现出明显的日、季节和年际变化,主要由供暖需求、脱碳措施和与大流行相关的工业放缓驱动。这些自上而下的估计,在GEMS NO2数据的约束下,与自下而上的库存显示出很强的一致性(R = 0.89),支持我们的优化方法的有效性。此外,与日间平均估算值的比较表明,受极轨卫星观测约束的二氧化碳排放估算值相对于基于地理位置的方法可能显示出约60%的偏差,这突出了高时间分辨率测量的重要性。该研究强调了整合地球静止NO2和CO2观测数据的价值,以捕获发电厂排放的日动态,并提高自上而下的CO2排放监测的准确性。
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引用次数: 0
Active and passive co-observations from a spaceborne lidar: Retrieving surface reflectance and aerosol optical thickness using ICESat-2 signal and noise data 星载激光雷达的主动和被动联合观测:利用ICESat-2信号和噪声数据检索地表反射率和气溶胶光学厚度
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-24 DOI: 10.1016/j.rse.2026.115264
Jian Yang , Huiying Zheng , Yue Ma , Xinyuan Liu , Song Li , Xiao Hua Wang , Wei Gong
The ICESat-2 (Ice, Cloud, and land Elevation Satellite-2) carries a revolutionary photon-counting lidar and diverse studies have demonstrated its great observational capabilities on Earth observations. However, it is still difficult to obtain high quality land surface reflectance in that a single measurement (e.g., the laser signal derived apparent surface reflectance) is characterized by two main unknowns, i.e., the SR (surface reflectance) and atmospheric transmission. As the radiative properties of ICESat-2 laser signal and solar noise are simultaneously obtained, we combine signal and noise information to achieve the co-observations, which show how two measurements help to decouple the reflectivity of atmosphere from surfaces and thus resolve this inherent ill-posed problem. Specifically, we propose the theoretical laser signal and solar noise models for spaceborne lidars that link the two measurements (the signal count and background rate) to the two unknowns. Then, a method and workflow applied for ICESat-2 is designed to retrieve the AOTs (aerosol optical thickness) and SRs. The performance is validated against the MODIS (Moderate-resolution Imaging Spectroradiometer) and AERONET (Aerosol Robotic NETwork) product with the average MAPE (mean absolute percentage errors) of less than 30% for AOTs and the average MAPE of less than 15% for SRs in different land cover types. In addition, the ability of this method to identify snow-covered or cloud-covered areas is explored and validated. This study provides a reference for the active and passive co-observations. In the future, satellites carrying both lidar and multispectral cameras could enable higher quality Earth observations, with the lidar enabling more accurate isolation of atmospheric and surface contributions.
ICESat-2(冰、云和陆地高程卫星-2)携带了革命性的光子计数激光雷达,各种研究已经证明了它在地球观测方面的巨大观测能力。然而,由于单次测量(如激光信号导出的地表表观反射率)存在两个主要未知数,即地表反射率(SR)和大气透射率,因此仍然难以获得高质量的地表反射率。由于ICESat-2激光信号和太阳噪声的辐射特性是同时获得的,我们将信号和噪声信息结合起来实现了共同观测,这表明了两次测量如何有助于将大气反射率与地表解耦,从而解决了这一固有的不适定问题。具体来说,我们提出了星载激光雷达的理论激光信号和太阳噪声模型,该模型将两个测量值(信号计数和背景速率)与两个未知数联系起来。然后,设计了适用于ICESat-2的AOTs(气溶胶光学厚度)和sr的检索方法和工作流程。通过MODIS(中分辨率成像光谱仪)和AERONET(气溶胶机器人网络)产品验证了该性能,不同土地覆盖类型的aot的平均MAPE(平均绝对百分比误差)小于30%,sr的平均MAPE小于15%。此外,还对该方法识别积雪或云层覆盖区域的能力进行了探索和验证。本研究为主动和被动共同观测提供了参考。未来,携带激光雷达和多光谱相机的卫星可以实现更高质量的地球观测,激光雷达可以更准确地分离大气和地表的贡献。
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引用次数: 0
Daily 4D landslide movements monitoring via InSAR: A fusion framework integrating physics-based and data-driven models 通过InSAR进行每日四维滑坡运动监测:一个融合了基于物理和数据驱动模型的融合框架
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-24 DOI: 10.1016/j.rse.2026.115263
Wanji Zheng , Min Zhao , Bo Huang , Aoqing Guo , Jun Hu
Continuous monitoring of deep-seated slow-moving landslides is a critical measure to mitigate risks posed by catastrophic events, especially under increasing extreme weather conditions. As a non-contact, high-resolution measurement technique, space-borne interferometric synthetic aperture radar (InSAR) has been widely applied in landslide monitoring. However, when used for continuous monitoring, challenges remain, including incomplete monitoring dimensions, slow update efficiency, and insufficient temporal resolution. To address these, this paper proposes a fusion framework of physics-based and data-driven models, built on a Kalman Filter, to rapidly obtain daily 4D (spatial 3D with time) landslide movements based on movement characteristics and dependence on hydrometeorological factors. The method's performance was evaluated using both synthetic and real datasets. On synthetic data, RMSEs in the east, north, and vertical directions were 9.6 mm, 3.8 mm, and 1.4 mm, respectively. For real data, the daily 4D movements were projected onto the Line-of-Sight (LOS) directions of Sentinel-1 Track 11 and ALOS2 PALSAR2 for comparison, achieving sub-centimeter Root Mean Square Errors (RMSEs). These results confirm the accuracy of the estimated movements and demonstrate enhanced update efficiency enabled by the Kalman Filter, which allows rapid assimilation of new data without reprocessing the full historical archive. Additionally, by incorporating geophysical and geodynamic methods, we leveraged daily 4D movements to derive various landslide parameters to analyze the kinematics of the Chuwangjing landslide during 2016–2024. The findings indicate that daily 4D movements not only enhance InSAR's performance in continuous landslide monitoring but also provide additional derivative products, deepening the understanding of deep-seated landslide kinematics.
持续监测深层缓慢移动的山体滑坡是减轻灾难性事件带来的风险的关键措施,特别是在极端天气条件日益增加的情况下。星载干涉合成孔径雷达(InSAR)作为一种非接触式、高分辨率的测量技术,在滑坡监测中得到了广泛应用。然而,当用于连续监视时,仍然存在挑战,包括监视维度不完整、更新效率缓慢和时间分辨率不足。为了解决这些问题,本文提出了一个基于卡尔曼滤波的物理和数据驱动模型的融合框架,基于运动特征和对水文气象因子的依赖,快速获得滑坡的每日4D(随时间的空间3D)运动。用合成数据集和真实数据集对该方法的性能进行了评价。在合成数据上,东、北、垂直方向的均方根误差分别为9.6 mm、3.8 mm和1.4 mm。对于真实数据,将每日4D运动投影到Sentinel-1 Track 11和ALOS2 PALSAR2的视距(LOS)方向进行比较,获得亚厘米的均方根误差(rmse)。这些结果证实了估计运动的准确性,并证明了卡尔曼滤波器增强的更新效率,它允许快速同化新数据而无需重新处理完整的历史档案。此外,通过结合地球物理和地球动力学方法,利用每日四维运动获得各种滑坡参数,分析了2016-2024年楚王京滑坡的运动学。研究结果表明,每天的4D运动不仅提高了InSAR在滑坡连续监测中的性能,而且提供了额外的衍生产品,加深了对深层滑坡运动学的理解。
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引用次数: 0
Centimeter-resolution 4D dynamics of retrogressive thaw slumps from repeat UAV photogrammetry on the Tibetan Plateau 基于重复无人机摄影测量的青藏高原退行性融化滑坡的厘米分辨率4D动态
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-24 DOI: 10.1016/j.rse.2026.115262
Siru Gao , Yushuo Liu , Xinyu Men , Hongting Zhao , Luyang Wang , Ziteng Fu , Zhongqiong Zhang , Yuzhong Yang , Guanli Jiang , Qingbai Wu
Retrogressive thaw slumps (RTSs) are critical indicators of permafrost degradation, with significant implications for ecosystems, infrastructure, and carbon cycling. However, their evolutionary processes remain poorly understood due to limited high-resolution observations. Here, centimeter-scale UAV surveys were conducted from 2019 to 2024 to track eight RTSs on the Tibetan Plateau, with site-specific monitoring frequencies ranging from one to six surveys per year. These RTSs displayed tongue-, trumpet-, or funnel-shaped elongated morphologies with an average aspect ratio of 3.0 and were predominantly north-facing. Their areas, volumes, and headwall heights ranged from 1688.4 to 38,991.9 m2, 594.1 to 51,961.1 m3, and 0.9 to 4.6 m, respectively. Most RTSs featured a three-part structure—rear-edge slumping, mid-slope sliding, and front-edge accumulation—each with distinct deformation characteristics. Two evolutionary pathways of RTS expansion, immediate-triggered and threshold-delayed, were identified. RTS activity was observed from June to October, with the most intense activity occurred between September and late October. Annual and monthly expansion averaged 1182.9 m2 yr−1 and 505.7 m2 mo−1, while headwall retreat reached 14.5 m yr−1 and 6.2 m mo−1. Surface elevation exhibited rear-edge subsidence (mean 2.4 m), central uplift (mean 1.4 m), and stable front-edge, with net volume loss mainly due to subsidence (mean 81%). Surface movement decreased from the rear-edge to the front-edge, with maximum values at the rear-edge slumping zone. This study quantified the evolution of small-scale RTSs—including changes in area, headwall retreat, surface movement, elevation, and volume—particularly focusing on monthly dynamics, thereby enhancing understanding and impact assessment of RTS.
退行性融化滑坡(RTSs)是冻土退化的重要指标,对生态系统、基础设施和碳循环具有重要影响。然而,由于有限的高分辨率观测,它们的进化过程仍然知之甚少。在这里,从2019年到2024年,进行了厘米尺度的无人机调查,以跟踪青藏高原上的8个rts,特定地点的监测频率从每年1到6次不等。这些RTSs显示舌状、喇叭状或漏斗状的细长形态,平均长宽比为3.0,主要面向北。它们的面积、体积和井壁高度分别为1688.4 ~ 38991.9 m2、594.1 ~ 51961.1 m3和0.9 ~ 4.6 m。大多数RTSs具有后缘滑坡、中坡滑动和前缘堆积三部分结构,各部分具有不同的变形特征。确定了即时触发和阈值延迟两种RTS扩展的进化途径。RTS活动发生在6 - 10月,其中9月至10月下旬最为活跃。年和月平均扩张面积分别为1182.9平方米/年和505.7平方米/月,而井壁退缩面积分别为14.5平方米/年和6.2平方米/月。地表高程表现为后缘沉降(平均2.4 m)、中央隆起(平均1.4 m)和前缘稳定,净体积损失主要由沉降引起(平均81%)。地表运动由后缘向前缘递减,后缘滑塌区最大;本研究量化了小规模RTS的演变,包括面积、井壁后退、地表移动、海拔和体积的变化,特别关注月度动态,从而增强了对RTS的理解和影响评估。
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引用次数: 0
Airborne and spaceborne imaging spectroscopy capture belowground microbial communities and physicochemical characteristics in invaded grasslands 航空和星载成像光谱捕获入侵草原地下微生物群落和物理化学特征
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-23 DOI: 10.1016/j.rse.2026.115250
M. Ny Aina Rakotoarivony , Kianoosh Hassani , Samuel Fuhlendorf , Benedicte Bachelot , Robert Hamilton , Hamed Gholizadeh
Belowground properties, including belowground microbial communities and physicochemical characteristics, play a crucial role in ecosystem functioning. Developing scalable approaches to map these properties across large spatial domains is essential for advancing our understanding of ecosystem functioning. However, large-scale approaches for mapping belowground properties, particularly in vegetated ecosystems, have yet to be developed. In this study, we aimed to develop approaches to map belowground microbial communities (bacterial and fungal) and physicochemical characteristics in an extensive grassland ecosystem affected by invasive plants using airborne and spaceborne imaging spectroscopy (hyperspectral remote sensing). We focused on Lespedeza cuneata (L. cuneata), an invasive plant threatening grasslands of the U.S. Southern Great Plains. We developed structural equation models to determine aboveground-belowground linkages. We used airborne hyperspectral data to estimate aboveground characteristics from partial least squares regression and then mapped belowground properties using aboveground characteristics through generalized joint attribute models. We also assessed the capability of spaceborne data in mapping the spatial distribution of belowground properties through fusing coarse spatial resolution DLR's DESIS hyperspectral data with fine spatial resolution PlanetScope multispectral data. Our findings showed that there are linkages between percent cover of L. cuneata, aboveground characteristics, and belowground properties. Large-scale analysis using airborne hyperspectral data showed that belowground properties varied across increasing percent cover of L. cuneata. Similar results were observed when using fused spaceborne data. Our findings indicated that (1) spectral information can reveal belowground properties and (2) fusing spaceborne data can be an effective approach to mapping belowground properties in grassland ecosystems.
地下性质,包括地下微生物群落和物理化学特征,在生态系统功能中起着至关重要的作用。开发可扩展的方法来绘制跨大空间域的这些属性对于提高我们对生态系统功能的理解至关重要。然而,测绘地下属性的大规模方法,特别是在植被生态系统中,尚未开发出来。在这项研究中,我们旨在开发利用航空和星载成像光谱(高光谱遥感)绘制受入侵植物影响的广阔草原生态系统地下微生物群落(细菌和真菌)和物理化学特征的方法。本文研究了威胁美国南部大平原草原的入侵植物胡枝子(lepedeza cuneata)。我们开发了结构方程模型来确定地上-地下的联系。利用机载高光谱数据通过偏最小二乘回归估计地表特征,然后通过广义联合属性模型利用地表特征映射地表特征。我们还通过融合粗空间分辨率DLR的DESIS高光谱数据和精细空间分辨率PlanetScope多光谱数据,评估了星载数据映射地下属性空间分布的能力。研究结果表明,山羊草盖度、地上性状和地下性状之间存在一定的联系。利用航空高光谱数据进行的大尺度分析表明,随着覆盖面积的增加,山羊草地下性质也会发生变化。在使用融合的星载数据时观察到类似的结果。研究结果表明:(1)光谱信息可以揭示草地地下特征;(2)融合星载数据可以有效地映射草地生态系统地下特征。
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引用次数: 0
Physics-guided deep learning for geostationary satellite-based estimation of dead fuel moisture content in Southwest China 基于物理引导的深度学习方法估算西南地区乏燃料含水率
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-22 DOI: 10.1016/j.rse.2026.115259
Chunquan Fan , Yiru Zhang , Rui Chen , Hongguo Zhang , Jianpeng Yin , Yanxi Li , Binbin He , Xingwen Quan
Accurate large-scale estimation of forest surface Dead Fuel Moisture Content (DFMC) is critical for wildfire risk warning and scientific decision-making. While existing process-based and empirical models leveraging satellite data show utility at local scales, they exhibit inherent limitations: process-based models suffer from physical simplifications in numerical simulations, while empirical approaches lack mechanistic integration due to shallow learning architectures. This persistent gap necessitates—yet lacks—integrative frameworks that synergize physical realism with deep learning flexibility. To address this challenge, we propose a physics-guided deep learning framework that synergistically integrates geostationary meteorological satellite data and reanalysis data for regional-scale forest surface DFMC estimation. Our methodology fuses Long Short-Term Memory (LSTM) neural network features with physical features derived from the process-based Fuel Stick Moisture Model (FSMM). Critically, the physical feature fuel surface relative humidity (RHsurf) is incorporated into the loss function to constrain model weights, yielding our final Physics-guided LSTM (PyLSTM) model. Validation using single-site 3079 h DFMC data from Chengdu, Sichuan, China, demonstrated PyLSTM's superior temporal performance (R2 = 0.70, RMSE = 10.60%). Spatial validation across 241 sites in Xizang, Yunnan, Guizhou, and Sichuan provinces confirmed its robust spatial accuracy (R2 = 0.71, RMSE = 16.96%), outperforming both standalone FSMM and LSTM models. PyLSTM successfully captured the declining DFMC trend preceding the Yajiang fire event, with significantly lower estimated DFMC in the burned area compared to surrounding pixels in Yajiang County. These results demonstrate PyLSTM's capability to enhance wildfire risk early warning and identify high-risk areas. Therefore, this study serves as a foundational step toward estimating hourly regional-scale DFMC dynamics—a vital factor in assessing fire danger and behavior.
准确大尺度估算森林地表枯油含水率(DFMC)对森林火灾风险预警和科学决策具有重要意义。虽然利用卫星数据的现有基于过程的模型和经验模型在局部尺度上显示出效用,但它们存在固有的局限性:基于过程的模型在数值模拟中存在物理简化的问题,而经验方法由于学习架构浅薄而缺乏机制集成。这种持续的差距需要——但缺乏——将物理现实性与深度学习灵活性协同起来的综合框架。为了应对这一挑战,我们提出了一个物理指导的深度学习框架,该框架协同整合了地球静止气象卫星数据和再分析数据,用于区域尺度森林表面DFMC估算。我们的方法将长短期记忆(LSTM)神经网络特征与基于过程的燃料棒水分模型(FSMM)的物理特征融合在一起。关键是,物理特征燃料表面相对湿度(RHsurf)被纳入损失函数以约束模型权重,从而产生最终的物理引导LSTM (PyLSTM)模型。使用来自中国四川成都的单站点3079 h DFMC数据进行验证,证明PyLSTM具有优越的时间性能(R2 = 0.70, RMSE = 10.60%)。对西藏、云南、贵州和四川等省241个站点的空间验证证实了该模型的空间精度(R2 = 0.71, RMSE = 16.96%),优于独立FSMM和LSTM模型。PyLSTM成功捕获了雅江火灾发生前DFMC下降的趋势,与雅江县周围像元相比,被烧毁区域的DFMC估计值显著降低。这些结果证明了PyLSTM在加强野火风险预警和识别高风险地区方面的能力。因此,本研究是估计每小时区域尺度DFMC动态的基础步骤,这是评估火灾危险和行为的重要因素。
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引用次数: 0
期刊
Remote Sensing of Environment
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