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A large-scale framework for deriving tidal flat topography from SWOT data 从SWOT数据推导潮滩地形的大尺度框架
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-10 DOI: 10.1016/j.rse.2026.115237
Hao Xu , Nan Xu , Wenyu Li , Kai Tan , Chunpeng Chen , Huan Li , Lucheng Zhan , Pei Xin , Jiaqi Yao , Peng Li , Zhen Zhang , Haipeng Zhao , Bolin Fu , Yifei Zhao , Yufeng Li , Qi Wang , Fan Zhao , Xiaojuan Liu , Zhongwen Hu , Guofeng Wu , Qingquan Li
Tidal flat topography is a fundamental attribute affecting inundation dynamics, sediment transport, and ecosystem functioning, yet accurate and spatially consistent large-scale monitoring remains challenging. Here, we leveraged satellite altimetry from the Surface Water and Ocean Topography (SWOT) mission to develop a novel, large-scale framework for deriving tidal flat topography from SWOT data, and demonstrated its capability by generating a high-accuracy, national-scale elevation dataset for China. By combining a percentile-based aggregation of multi-temporal water-surface elevation observations with a tide-constrained, adaptive best-quantile (best-q) reconstruction strategy, followed by linear interpolation for gap filling, we improved both vertical accuracy and spatial completeness. Validation against airborne LiDAR, GNSS-RTK surveys, and ICESat-2 photon data demonstrates robust performance across diverse coastal settings, achieving RMSE = 0.34–0.47 m and R2 = 0.81–0.88 at a horizontal resolution of 100 m. Compared with existing large-scale digital elevation models (DEMs), the SWOT-derived topography not only improves vertical accuracy by over 80% but also providing substantially more complete spatial coverage of tidal flat elevations. Spatial analyses reveal pronounced latitudinal gradients, with higher tidal flats concentrated in low-latitude regions and extensive low-lying flats dominating northern estuarine and deltaic systems. This study establishes a scalable framework for tidal-flat elevation retrieval and provides a foundational dataset to support coastal monitoring and sustainable management.
潮滩地形是影响淹没动态、泥沙输运和生态系统功能的基本属性,但精确和空间一致的大规模监测仍然具有挑战性。在这里,我们利用来自地表水和海洋地形(SWOT)任务的卫星测高数据,开发了一个新的、大规模的框架,用于从SWOT数据中获取潮滩地形,并通过生成中国高精度的国家尺度高程数据集来证明其能力。通过将基于百分位的多时间点水面高程观测集合与潮汐约束的自适应最佳分位数(best-q)重建策略相结合,然后采用线性插值进行间隙填充,我们提高了垂直精度和空间完整性。针对机载LiDAR、GNSS-RTK调查和ICESat-2光子数据的验证表明,在不同的沿海环境下,该方法具有强大的性能,在100米的水平分辨率下,RMSE = 0.34-0.47 m, R2 = 0.81-0.88。与现有的大尺度数字高程模型(dem)相比,swot衍生的地形不仅垂直精度提高了80%以上,而且提供了更完整的潮滩高程空间覆盖。空间分析显示了明显的纬度梯度,高纬度潮滩集中在低纬度地区,北部河口和三角洲系统主要是广泛的低洼滩。本研究建立了一个可扩展的潮坪高程检索框架,为支持沿海监测和可持续管理提供了基础数据集。
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引用次数: 0
Enhancing cloud detection across multiple satellite sensors using a combined Swin Transformer and UPerNet deep learning model 使用Swin Transformer和UPerNet深度学习模型的组合增强跨多个卫星传感器的云检测
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-09 DOI: 10.1016/j.rse.2025.115206
Shulin Pang , Zhanqing Li , Lin Sun , Biao Cao , Zhihui Wang , Xinyuan Xi , Xiaohang Shi , Jing Xu , Jing Wei
Cloud detection is crucial in many applications of satellite remote sensing data. Traditional cloud detection methods typically operate at the pixel level, relying on empirically tuned thresholds or, more recently, machine learning classification schemes based on training datasets. Motivated by the success of the Transformer with its self-attention mechanism and convolutional neural networks for enhanced feature extraction, we propose a new encoder-decoder method that captures global and regional contexts with multi-scale features. This new model takes advantage of two advanced deep-learning techniques, the Swin Transformer and UPerNet (named STUPmask), demonstrating improved cloud detection accuracy and strong adaptability to diverse imagery types, spanning spectral bands from visible to thermal infrared and spatial resolutions from meters to kilometers, across a wide range of surface types, including bright scenes such as ice and desert, globally. Training and validation of the STUPmask model are conducted using data obtained from the Landsat 8 and Sentinel-2 Manually Cloud Validation Mask datasets on a global scale. STUPmask accurately estimates cloud amount with a marginal difference against reference masks (0.27 % for Landsat 8 and −0.81 % for Sentinel-2). Additionally, the model captures cloud distribution with a high overall classification accuracy (97.51 % for Landsat 8 and 96.27 % for Sentinel-2). Notably, it excels in detecting broken, thin, and semi-transparent clouds across diverse surfaces, including bright surfaces like urban and barren lands, especially with acceptable accuracy over snow and ice. These encompass the majority of challenging scenes encountered by cloud identification methods. It also adapts to cross-sensor satellite data with varying spatial resolutions (4 m–2 km) from both Low-Earth-Orbit (LEO) and Geostationary-Earth-Orbit (GEO) platforms (including GaoFen-2, MODIS, and Himawari-8), with an overall accuracy of 94.21–97.11 %. The demonstrated successes in the automatic identification of clouds with a variety of satellite imagery of different spectral channels and spatial resolutions render the method versatile for a wide range of remote sensing studies.
云探测在卫星遥感数据的许多应用中是至关重要的。传统的云检测方法通常在像素级运行,依赖于经验调整的阈值,或者最近基于训练数据集的机器学习分类方案。由于Transformer的自关注机制和卷积神经网络在增强特征提取方面的成功,我们提出了一种新的编码器-解码器方法,该方法可以捕获具有多尺度特征的全局和区域上下文。这种新模型利用了两种先进的深度学习技术,Swin Transformer和UPerNet(名为STUPmask),展示了改进的云检测精度和对不同图像类型的强大适应性,涵盖了从可见光到热红外的光谱波段和从米到公里的空间分辨率,涵盖了广泛的表面类型,包括全球范围内的明亮场景,如冰和沙漠。使用全球范围内Landsat 8和Sentinel-2手动云验证掩码数据集的数据进行STUPmask模型的训练和验证。与参考掩模相比,STUPmask准确地估计了云量,差异很小(Landsat 8为0.27%,Sentinel-2为- 0.81%)。此外,该模型以较高的总体分类精度捕获云分布(Landsat 8为97.51%,Sentinel-2为96.27%)。值得注意的是,它在探测不同表面(包括城市和贫瘠土地等明亮表面)上的碎云、薄云和半透明云方面表现出色,特别是在冰雪上的精度可以接受。这些包含了云识别方法遇到的大多数具有挑战性的场景。它还适应来自低地球轨道(LEO)和地球静止轨道(GEO)平台(包括高分2号、MODIS和Himawari-8)的不同空间分辨率(4 m-2 km)的跨传感器卫星数据,总体精度为94.21 - 97.11%。在使用不同光谱通道和空间分辨率的各种卫星图像自动识别云方面所取得的成功,使该方法适用于广泛的遥感研究。
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引用次数: 0
AgriFM: A multi-source temporal remote sensing foundation model for Agriculture mapping AgriFM:农业制图的多源时序遥感基础模型
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-09 DOI: 10.1016/j.rse.2026.115234
Wenyuan Li , Shunlin Liang , Keyan Chen , Yongzhe Chen , Han Ma , Jianglei Xu , Yichuan Ma , Yuxiang Zhang , Shikang Guan , Husheng Fang , Zhenwei Shi
Climate change and population growth intensify the demand for precise agriculture mapping to enhance food security. Such mapping tasks require robust modeling of multi-scale spatiotemporal patterns from fine field textures to landscape context, and from short-term phenology to full growing-season dynamics. Existing methods often process spatial and temporal features separately, limiting their ability to capture essential agricultural dynamics. While transformer-based remote sensing foundation models (RSFMs) offer unified spatiotemporal modeling ability, most of them remain suboptimal: they either use fixed windows that ignore multi-scale crop characteristics or neglect temporal information entirely. To address these gaps, we propose AgriFM, a multi-source, multi-temporal foundation model for agriculture mapping. AgriFM introduces a synchronized spatiotemporal downsampling strategy within a Video Swin Transformer backbone, enabling efficient handling of long and variable-length satellite time series while preserving multi-scale spatial and phenological information. It is pre-trained on a globally representative dataset comprising over 25 million samples from MODIS, Landsat-8/9, and Sentinel-2 with land cover fractions as pre-training supervision. AgriFM further integrates a versatile decoder specifically designed to dynamically fuse multi-source features from different stages of backbone and accommodate varying temporal lengths, thereby supporting consistent and scalable agriculture mapping across diverse satellite sources and task requirements. It supports diverse tasks including agricultural land mapping, field boundary delineation, agricultural land use/land cover mapping, and specific crop mapping (e.g., winter wheat and paddy rice) with different data sources. Comprehensive evaluations show that AgriFM consistently outperforms existing deep learning models and general-purpose RSFMs across multiple agriculture mapping tasks. Codes and models are available at https://github.com/flyakon/AgriFM and https://glass.hku.hk
气候变化和人口增长加剧了对精确农业制图以加强粮食安全的需求。这样的测绘任务需要多尺度时空模式的强大建模,从精细的田野纹理到景观背景,从短期物候到整个生长季节动态。现有的方法往往分别处理空间和时间特征,限制了它们捕捉基本农业动态的能力。虽然基于变压器的遥感基础模型(RSFMs)提供了统一的时空建模能力,但大多数模型仍然不是最优的:它们要么使用固定窗口,忽略多尺度作物特征,要么完全忽略时间信息。为了解决这些差距,我们提出了一个多源、多时间的农业制图基础模型AgriFM。AgriFM在Video Swin Transformer主干中引入了同步的时空下采样策略,能够有效处理长时间和变长度的卫星时间序列,同时保留多尺度空间和物候信息。它是在一个具有全球代表性的数据集上进行预训练的,该数据集包括来自MODIS、Landsat-8/9和Sentinel-2的超过2500万个样本,土地覆盖分数作为预训练监督。AgriFM进一步集成了一个多功能解码器,专门设计用于动态融合来自不同主干网阶段的多源特征,并适应不同的时间长度,从而支持跨不同卫星源和任务需求的一致和可扩展的农业制图。它支持多种任务,包括农业用地制图、田间边界划定、农业用地利用/土地覆盖制图以及使用不同数据源的特定作物制图(如冬小麦和水稻)。综合评估表明,AgriFM在多个农业制图任务中始终优于现有的深度学习模型和通用rsfm。代码和模型可在https://github.com/flyakon/AgriFM和https://glass.hku.hk上获得
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引用次数: 0
Estimating the upper depth of subsurface water on the Greenland Ice Sheet using multi-frequency passive microwave remote sensing, radiative transfer modeling, and machine learning 利用多频被动微波遥感、辐射传输模型和机器学习估算格陵兰冰盖地下水上层深度
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-09 DOI: 10.1016/j.rse.2025.115197
Baptiste Vandecrux , Ghislain Picard , Pierre Zeiger , Marion Leduc-Leballeur , Andreas Colliander , Alamgir Hossan , Andreas Ahlstrøm
As the Arctic warms, surface melt extends into the Greenland Ice Sheet's accumulation zone, where much of the water infiltrates into the snowpack. This makes monitoring the subsurface water depth and spatial extent important for accurate ice sheet runoff estimations. Subsurface water can be detected using remotely sensed microwave brightness temperatures (TB). We use vertically polarized TB at 1.4 GHz from Soil Moisture and Ocean Salinity satellite (SMOS) and at 6.9, 10.7, and 18.7 GHz from the Advanced Microwave Scanning Radiometers (AMSR-E/2) to estimate the upper depth of liquid water (UDLW) on the ice sheet accumulation area. We build a catalogue of simulated UDLW and TB: realistic UDLW are modeled by the Geological Survey of Denmark and Greenland (GEUS) snow model, forced by the Copernicus Arctic Regional Reanalysis (CARRA), and the corresponding TB are calculated by the Snow Microwave Radiative Transfer (SMRT) model at 19 sites. We train on this catalogue an ensemble of cross-validated Random Forest (RF) models to predict UDLW and its uncertainty from TB at four frequencies. On hold-out modeled data and for water within 5 m of the surface, the RF ensemble achieves a median RMSE of 0.68 m and mean error of −0.09 m. Our retrieval, when applied to observed TB, matches within 2 m UDLW inferred from subsurface temperature profiles down to 4–6 m depth. Performances decrease beyond 5 m depth and for low liquid water amounts. Our retrieval produces daily UDLW maps over the ice sheet's accumulation area during 2010–2023 which reveal the seasonal evolution of UDLW, deliver the first quantitative estimates of subsurface liquid water depth on the ice sheet and offer new insights into meltwater infiltration and storage processes.
随着北极变暖,表面融化延伸到格陵兰冰盖的积累区,在那里,大部分水渗透到积雪中。这使得监测地下水深度和空间范围对于准确估计冰盖径流非常重要。利用遥感微波亮度温度(TB)可以探测地下水。利用土壤水分和海洋盐度卫星(SMOS)的1.4 GHz垂直极化TB和高级微波扫描辐射计(AMSR-E/2)的6.9、10.7和18.7 GHz垂直极化TB,估算了冰盖堆积区液态水(UDLW)的上层深度。基于哥白尼北极区域再分析(CARRA)强迫的丹麦和格陵兰地质调查局(GEUS)雪模式模拟了真实的UDLW,并利用SMRT雪微波辐射传输(SMRT)模式计算了19个站点的实际UDLW。我们在这个目录上训练了一个交叉验证的随机森林(RF)模型集合,以预测结核在四个频率下的UDLW及其不确定性。在保留模型数据和距离地表5米以内的水上,RF集合的中位数RMSE为0.68 m,平均误差为- 0.09 m。当应用于观测到的结核时,我们的检索结果匹配从4-6米深度的地下温度剖面推断的2米UDLW。深度超过5米及液态水含量低时,性能下降。我们的检索生成了2010-2023年期间冰盖积累区的每日UDLW图,揭示了UDLW的季节性演变,提供了冰盖地下液态水深度的第一个定量估计,并为融水渗透和储存过程提供了新的见解。
{"title":"Estimating the upper depth of subsurface water on the Greenland Ice Sheet using multi-frequency passive microwave remote sensing, radiative transfer modeling, and machine learning","authors":"Baptiste Vandecrux ,&nbsp;Ghislain Picard ,&nbsp;Pierre Zeiger ,&nbsp;Marion Leduc-Leballeur ,&nbsp;Andreas Colliander ,&nbsp;Alamgir Hossan ,&nbsp;Andreas Ahlstrøm","doi":"10.1016/j.rse.2025.115197","DOIUrl":"10.1016/j.rse.2025.115197","url":null,"abstract":"<div><div>As the Arctic warms, surface melt extends into the Greenland Ice Sheet's accumulation zone, where much of the water infiltrates into the snowpack. This makes monitoring the subsurface water depth and spatial extent important for accurate ice sheet runoff estimations. Subsurface water can be detected using remotely sensed microwave brightness temperatures (T<sub>B</sub>). We use vertically polarized T<sub>B</sub> at 1.4 GHz from Soil Moisture and Ocean Salinity satellite (SMOS) and at 6.9, 10.7, and 18.7 GHz from the Advanced Microwave Scanning Radiometers (AMSR-E/2) to estimate the upper depth of liquid water (UDLW) on the ice sheet accumulation area. We build a catalogue of simulated UDLW and T<sub>B</sub>: realistic UDLW are modeled by the Geological Survey of Denmark and Greenland (GEUS) snow model, forced by the Copernicus Arctic Regional Reanalysis (CARRA), and the corresponding T<sub>B</sub> are calculated by the Snow Microwave Radiative Transfer (SMRT) model at 19 sites. We train on this catalogue an ensemble of cross-validated Random Forest (RF) models to predict UDLW and its uncertainty from T<sub>B</sub> at four frequencies. On hold-out modeled data and for water within 5 m of the surface, the RF ensemble achieves a median RMSE of 0.68 m and mean error of −0.09 m. Our retrieval, when applied to observed T<sub>B</sub>, matches within 2 m UDLW inferred from subsurface temperature profiles down to 4–6 m depth. Performances decrease beyond 5 m depth and for low liquid water amounts. Our retrieval produces daily UDLW maps over the ice sheet's accumulation area during 2010–2023 which reveal the seasonal evolution of UDLW, deliver the first quantitative estimates of subsurface liquid water depth on the ice sheet and offer new insights into meltwater infiltration and storage processes.</div></div>","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"334 ","pages":"Article 115197"},"PeriodicalIF":11.4,"publicationDate":"2026-01-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145938861","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"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
Remote sensing of the global cryosphere: Status, processes, and trends 全球冰冻圈遥感:现状、过程和趋势
IF 13.5 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-08 DOI: 10.1016/j.rse.2025.115220
Guoqing Zhang, Hongjie Xie, Alfonso Fernandez, Christophe Kinnard, Stef Lhermitte
Driven by rapid technological advances in cryospheric science and the emergence of new generations of remote sensing observations, this special issue of Remote Sensing of Environment, entitled “Remote sensing of the global cryosphere: status, processes, and trends”, brings together 23 studies published between 2023 and 2025. Collectively, these papers showcase how multi-sensor satellite observations, high-resolution digital elevation models (DEMs), and cutting-edge deep learning techniques are revolutionizing the monitoring of glaciers, snow, glacial lakes, permafrost, sea ice, and ice shelves across the Earth's three poles: the Arctic (including Greenland), Antarctica, and High Mountain Asia (the Third Pole). These studies integrate diverse datasets – including multisource DEMs, optical, thermal, and passive microwave imageries, as well as RADAR, LiDAR, and GRACE observations - to quantify glacier mass balance, map glacial lakes, assess permafrost thermal conditions, classify sea-ice types, and detect icebergs. We organize the publications by major cryospheric themes and their distribution across polar regions and summarize the dominant remote sensing datasets and methodologies employed. Finally, we outline future directions, emphasizing multi-sensor data fusion, physics-informed modeling, and AI-driven approaches to improve predictions of cryospheric change under a warming climate.
在冰冻圈科学快速技术进步和新一代遥感观测出现的推动下,本期《环境遥感》特刊题为“全球冰冻圈遥感:现状、过程和趋势”,汇集了2023年至2025年间发表的23项研究。总的来说,这些论文展示了多传感器卫星观测、高分辨率数字高差模型(dem)和尖端深度学习技术如何彻底改变对地球三极冰川、雪、冰川湖、永久冻土、海冰和冰架的监测:北极(包括格陵兰岛)、南极洲和亚洲高山(第三极)。这些研究整合了不同的数据集,包括多源dem、光学、热和被动微波图像,以及雷达、激光雷达和GRACE观测,以量化冰川物质平衡,绘制冰川湖泊图,评估永久冻土热条件,对海冰类型进行分类,并探测冰山。我们根据主要的冰冻圈主题及其在极地地区的分布来组织出版物,并总结了主要的遥感数据集和采用的方法。最后,我们概述了未来的发展方向,强调多传感器数据融合、物理信息建模和人工智能驱动的方法,以改善气候变暖下冰冻圈变化的预测。
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引用次数: 0
Determinants of L-band backscatter in dry tropical ecosystems: Implications for biomass mapping 干燥热带生态系统l波段反向散射的决定因素:对生物量制图的影响
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-08 DOI: 10.1016/j.rse.2025.115213
João M.B. Carreiras , Thomas Higginbottom , John L. Godlee , Sam Harrison , Lorena Benitez , Penelope J. Mograbi , Aurora Levesley , Karina Melgaço , David Milodowski , Georgia Pickavance , Geoff Wells , Edmar Almeida de Oliveira , Luzmila Arroyo , Sam Bowers , Roel J.W. Brienen , Domingos Cardoso , António Alberto Jorge Farias Castro , Ezequiel Chavez , Ítalo A.C. Coutinho , Tomás F. Domingues , Casey M. Ryan
<div><div>Accurate characterization of the role of the dry tropics in the global carbon cycle requires precise estimation of woody biomass changes due to ecological and anthropogenic change, including deforestation, forest degradation, regrowth, mortality and enhanced tree growth due to climate change. L-band Synthetic Aperture Radar (SAR) backscatter observations offer a reliable option to consistently map these processes as they are (i) available globally since 2007 (JAXA ALOS-1, ALOS-2 and ALOS-4), and (ii) sensitive to woody structure, such as aboveground biomass density (<span><math><mi>AGBD</mi></math></span>) up to ∼100 t ha<sup>−1</sup>. However, we lack multi-site empirical understanding of the scattering processes that determine the relationship between L-band SAR and woody vegetation structure in the dry tropics, and how this is mediated by soil properties.</div><div>This study used observations from ground plots in Africa (<em>n</em> = 171), Australia (<em>n</em> = 6), and South America (<em>n</em> = 44) to understand the impact of vegetation structure and soil properties on spatially and temporally coincident fully-polarimetric L-band SAR data. Fully-polarimetric L-band SAR single-look complex data were converted to scattering mechanisms/parameters using van Zyl, Cloude-Pottier, and Freeman-Durden polarimetric decompositions to elucidate the physical mechanisms involved. Multivariate SAR-vegetation-soil relationships were analysed using a theory-informed structural equation modelling approach. The strongest positive effects on volume scattering come from stem density (stems ha<sup>−1</sup>) and mean stem biomass of trees, and soil water and sand content (standardized regression coefficients of 0.3, 0.1, 0.2 and 0.1, respectively). The only significant effect on surface scattering is from stem density (0.1). Significant effects on double bounce scattering are from stem density (0.3) and soil sand content (−0.2). Since <span><math><mi>AGBD</mi></math></span> is the product of stem density and mean stem biomass, this modelling framework points to a stronger effect from the number of trees rather than their size/biomass. Therefore, <span><math><mi>AGBD</mi></math></span> maps relying solely on radar intensity may not reflect significant changes when <span><math><mi>AGBD</mi></math></span> is increasing due to the growth of existing stems. Additionally, such maps might overestimate changes in <span><math><mi>AGBD</mi></math></span> when driven by the recruitment of new stems or loss of existing stems. Full-polarimetric observations allow the decomposition of the radar signal into volume scattering, surface scattering, and double bounce, enabling the inversion of structural equation models to retrieve both stem density and mean stem biomass. This provides a more comprehensive description of forest structure compared to retrieving only <span><math><mi>AGBD</mi></math></span>. As this approach depends on full-polarimetric data, its effective
要准确描述干燥热带地区在全球碳循环中的作用,就需要精确估计由于生态和人为变化造成的木质生物量变化,包括森林砍伐、森林退化、再生、死亡和气候变化导致的树木生长增强。l波段合成孔径雷达(SAR)后向散射观测提供了一种可靠的选择,可以一致地绘制这些过程,因为它们(i)自2007年以来在全球范围内可用(JAXA ALOS-1, ALOS-2和ALOS-4),并且(ii)对木质结构敏感,例如地上生物量密度(AGBD)高达~ 100 t ha -1。然而,我们缺乏对l波段SAR与干旱热带木本植被结构之间关系的散射过程的多站点经验理解,以及土壤性质如何介导这种关系。本研究利用非洲(n = 171)、澳大利亚(n = 6)和南美洲(n = 44)的地面样地观测资料,了解植被结构和土壤性质对时空重合全极化l波段SAR数据的影响。利用van Zyl、cloud - pottier和Freeman-Durden极化分解方法,将全极化l波段SAR单目复杂数据转换为散射机制/参数,以阐明所涉及的物理机制。利用结构方程建模方法分析了多变量sar -植被-土壤关系。对体积散射的正向影响最大的是树木的茎密度(茎ha−1)和平均茎生物量,以及土壤含水量和含沙量(标准化回归系数分别为0.3、0.1、0.2和0.1)。唯一对表面散射有显著影响的是茎密度(0.1)。茎密度(0.3)和土壤含沙量(−0.2)对双弹跳散射有显著影响。由于AGBD是茎密度和平均茎生物量的产物,该模型框架指出,树木数量的影响比它们的大小/生物量更强。因此,单纯依靠雷达强度的AGBD地图可能无法反映出由于现有系统的生长而增加的AGBD的显著变化。此外,这样的图谱可能会高估AGBD的变化,因为它是由新茎的吸收或现有茎的丧失所驱动的。全极化观测允许将雷达信号分解为体散射、表面散射和双反弹,从而实现结构方程模型的反演,从而获得茎密度和平均茎生物量。与仅检索AGBD相比,这提供了更全面的森林结构描述。由于这种方法依赖于全极化数据,其有效性与这种观测的可用性密切相关。我们的研究结果强调了ALOS-4、PALSAR-3、BIOMASS和ROSE-L等近期和即将开展的任务的价值,并强调了优先获取四极SAR数据以支持未来大规模植被结构属性检索的必要性。
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引用次数: 0
Probabilistic mapping of high-intensity forest fire potential via time series machine learning and remote sensing-informed fire spread simulations 基于时间序列机器学习和遥感信息的火灾蔓延模拟的高强度森林火灾潜力的概率映射
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-08 DOI: 10.1016/j.rse.2026.115233
Rui Chen , Yiru Zhang , Yanxi Li , Marta Yebra , Chunquan Fan , Hongguo Zhang , Binbin He
High-intensity forest fires have significant destructive impacts on ecosystems and society, and are an increasing concern worldwide. Accurate probabilistic risk assessment of these fires can effectively enhance the ability to guide wildfire management, particularly for large and extreme fires. However, forecasting large-scale fire behavior characteristics remains challenging, limiting the effectiveness of spatial estimations of high-intensity forest fire potential (HIFFP). This study aims to integrate fire spread simulations and machine learning (ML) algorithms to enhance HIFFP estimations through multi-step time-series forecasting on fire rate of spread and fireline intensity at regional scales. We first established a high-intensity forest fire dataset based on remote sensing-informed fire spread simulations from the Weather Research and Forecasting coupled fire-spread model (WRF-SFIRE), incorporating explanatory variables on fuel, weather, climate, and topography. Then, the knowledge-guided framework (multi-step time series-based ML, MTS-ML) was designed to estimate HIFFP within different hours after fires occur, integrating with Bayesian Network (BN), Random Forest (RF), and copula models. Results indicate that MTS-ML improved HIFFP modeling compared with ML-based methods, achieving AUC (the area under the receiver operating characteristic curve) > 0.95 (with ∼0.04 increments), F1 score > 0.85 (with ∼0.08 increments), and MAE < 0.15. Topographic index, foliage fuel load, and wind speed are identified as primary contributors to HIFFP. Probabilistic mapping of HIFFP represents wildfire danger, which is closely linked to burn severity and fire-induced carbon emissions. This study presents a novel framework for enhancing regional risk assessment of high-intensity forest fires, providing valuable guidance in wildfire control and management.
高强度森林火灾对生态系统和社会具有重大的破坏性影响,并日益受到全世界的关注。对这些火灾进行准确的概率风险评估可以有效地提高指导野火管理的能力,特别是对于大型和极端火灾。然而,预测大尺度火灾行为特征仍然具有挑战性,限制了高强度森林火灾潜力(HIFFP)空间估计的有效性。本研究旨在结合火灾蔓延模拟和机器学习(ML)算法,通过在区域尺度上对火灾蔓延速度和火线强度进行多步时间序列预测,增强HIFFP估计。我们首先基于天气研究与预报耦合火灾蔓延模型(WRF-SFIRE)的遥感信息火灾蔓延模拟建立了一个高强度森林火灾数据集,并纳入了燃料、天气、气候和地形等解释变量。然后,结合贝叶斯网络(BN)、随机森林(RF)和copula模型,设计了知识引导框架(基于多步时间序列的ML, MTS-ML)来估计火灾发生后不同小时内的HIFFP。结果表明,与基于ml的方法相比,MTS-ML改进了HIFFP建模,实现了AUC(受试者工作特征曲线下面积)> 0.95(增量为~ 0.04),F1评分>; 0.85(增量为~ 0.08),MAE < 0.15。地形指数,叶片燃料负荷和风速被确定为HIFFP的主要贡献者。HIFFP的概率图表示野火危险,这与烧伤严重程度和火灾引起的碳排放密切相关。本研究为加强区域高强度森林火灾风险评估提供了一个新的框架,为森林火灾的控制和管理提供了有价值的指导。
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引用次数: 0
High-resolution annual desertification mapping in northern China using a novel comprehensive desertification index and unsupervised algorithm 基于新型综合沙漠化指数和无监督算法的中国北方高分辨率沙漠化年制图
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-08 DOI: 10.1016/j.rse.2025.115230
Yaqing Dou , Huaiqing Zhang , Hua Sun , Hui Lin , Yang Liu , Meng Zhang
Desertification is a global ecological and environmental problem, dynamic monitoring and accurate assessment of desertification are essential for restoring regional ecology and achieving sustainable development. Current desertification monitoring methods face dual challenges including unclear remote sensing mechanisms, non-robust extraction methods and the absence of high-resolution large-scale desertification products. This study constructs a comprehensive desertification index (CDI) by integrating multisource remote sensing data (Sentinel-1/2), incorporating three features —phenomenal indices (vegetation cover), cause indices (soil moisture) and essence indices (soil roughness)—on the basis of the multidimensional driving mechanisms of desertification physical processes. The Gaussian mixture model (GMM) was then applied to the CDI to automate desertification mapping for yielding the first 10 m-resolution annual desertification dataset in northern China (NCDMD, 2016–2024). The results demonstrated that the CDI-GMM based method achieves superior performance in mapping desertification scope across northern China in 2019, with an overall accuracy of 93.5 % and an overall accuracy of 86.4 % for desertification degree according to field survey data. In comparison, traditional approaches showed significantly lower accuracy, with the pixel dichotomy model (FVC-based) achieving 82.2 % in scope extraction and 50.3 % in degree classification, while the DDI feature space method reached 86.1 % and 64.2 %, respectively. Comparative experiments with five unsupervised classification methods (GMM, K-Means, MiniBatch K-Means, Jenks natural breaks, and Weka LVQ algorithms) indicated that the CDI combined with the GMM clustering algorithm can optimize the extraction of desertification and maintain stable performance, with an overall classification accuracy of over 93 %. Moreover, the NCDMD achieved consistent desertification mapping accuracies above 83 % throughout the 2016–2024 period, further demonstrating the robust spatiotemporal reliability of the proposed product. In summary, as a nationally significant high-resolution base dataset, the NCDMD not only fills the gap in high-precision desertification monitoring in China but also provides scientific support for ecological restoration assessment and land management policy-making.
荒漠化是一个全球性的生态环境问题,对荒漠化进行动态监测和准确评价是恢复区域生态和实现可持续发展的关键。目前的荒漠化监测方法面临着遥感机制不明确、提取方法不稳健和缺乏高分辨率大尺度荒漠化产品的双重挑战。本研究基于沙漠化物理过程的多维驱动机制,整合多源遥感数据(Sentinel-1/2),结合现象指数(植被覆盖)、成因指数(土壤湿度)和本质指数(土壤粗糙度)三个特征,构建了综合沙漠化指数(CDI)。然后将高斯混合模型(GMM)应用于CDI,实现沙漠化制图自动化,生成了中国北方第一个10 m分辨率的沙漠化年度数据集(NCDMD, 2016-2024)。结果表明,基于CDI-GMM的方法在2019年中国北方地区沙漠化范围制图中取得了较好的效果,根据野外调查数据,沙漠化程度的总体精度为93.5%,总体精度为86.4%。相比之下,传统方法的准确率明显较低,基于像素二分法(fvc)的范围提取准确率为82.2%,程度分类准确率为50.3%,而DDI特征空间方法的范围提取准确率为86.1%,程度分类准确率为64.2%。与5种无监督分类方法(GMM、K-Means、MiniBatch K-Means、Jenks natural breaks和Weka LVQ算法)的对比实验表明,CDI结合GMM聚类算法可以优化提取沙漠化特征,并保持稳定的性能,总体分类准确率在93%以上。此外,在2016-2024年期间,NCDMD的沙漠化制图精度保持在83%以上,进一步证明了所提出产品的强大时空可靠性。综上所述,NCDMD作为全国重要的高分辨率基础数据集,不仅填补了中国沙漠化高精度监测的空白,而且为生态恢复评价和土地管理决策提供了科学支持。
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引用次数: 0
A transformer based multi-task deep learning model for urban livability evaluation by fusing remote sensing and textual geospatial data 基于遥感和文本地理空间数据融合的城市宜居性评价多任务深度学习模型
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-08 DOI: 10.1016/j.rse.2026.115232
Wen Zhou , Claudio Persello , Dongping Ming , Shaowen Wang , Alfred Stein
Livable cities enhance urban economic development, improve physical and mental health, foster well-being, and foster urban sustainability. Evaluating urban livability is therefore important for policymakers to develop urban planning and development strategies aimed at improving livability. Mainstream methods of evaluating urban livability assign different weights to diverse indicators extracted from survey data, statistical data, and geospatial data. To relieve such time-consuming and labor-intensive data collection, this study proposes a transformer-based multi-task multimodal regression (TMTMR) model for the simultaneous evaluation of urban livability focusing on five domain-specific scores. Pretrained state-of-the-art computer vision and natural language processing models serve as backbones to extract features from high spatial resolution remote sensing (RS) images, digital surface models (DSM), night light remote sensing (NLRS) images and point of interest (POI) data. An attention mechanism helps the TMTMR model to assign varying significance levels to features from different modalities, thus capturing both intrinsic information and interrelationships among modalities for livability evaluation. Focusing on 13 Dutch areas, our research demonstrates that the TMTMR model efficiently evaluates urban livability with correlation coefficients ranging from 0.605 to 0.779, and root mean square error values between 0.070 and 0.112 in four unseen test areas. Furthermore, we analyze the synergy between different modalities. We found that modalities of urban livability can be effectively evaluated by aligning, in a descending order, contributions from RS images, NLRS images, DSM, and POI data. We demonstrated that the proposed TMTMR model is capable of effectively evaluating urban livability directly from multimodal geospatial data.
宜居城市促进城市经济发展,改善身心健康,促进福祉,促进城市可持续发展。因此,评估城市宜居性对于决策者制定旨在改善宜居性的城市规划和发展战略至关重要。评价城市宜居性的主流方法对从调查数据、统计数据和地理空间数据中提取的不同指标赋予不同的权重。为了减轻这种耗时和劳动密集型的数据收集,本研究提出了一个基于转换器的多任务多模态回归(TMTMR)模型,用于同时评估城市宜居性,重点关注五个特定领域的分数。预训练的最先进的计算机视觉和自然语言处理模型作为从高空间分辨率遥感(RS)图像、数字表面模型(DSM)、夜间光遥感(NLRS)图像和兴趣点(POI)数据中提取特征的主干。注意机制有助于TMTMR模型为不同模式的特征分配不同的显著性水平,从而捕获可居性评估模式之间的内在信息和相互关系。以荷兰13个地区为研究对象,我们的研究表明,TMTMR模型有效地评估了城市宜居性,相关系数在0.605至0.779之间,均方根误差在0.070至0.112之间。此外,我们分析了不同模式之间的协同作用。我们发现,通过按降序排列RS图像、NLRS图像、DSM和POI数据的贡献,可以有效地评估城市宜居性的模式。我们证明了所提出的TMTMR模型能够直接从多模态地理空间数据中有效地评估城市宜居性。
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引用次数: 0
Multi-sensor (since 1997) global soil moisture mapping with enhanced Spatio-temporal coverage through machine learning framework fusion 多传感器(自1997年以来)全球土壤湿度制图,通过机器学习框架融合增强时空覆盖
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-01-07 DOI: 10.1016/j.rse.2025.115221
Haojie Zhang , Tianjie Zhao , Zhiqing Peng , Jingyao Zheng , Yu Bai , Nemesio Rodriguez-Fernadez , Donghai Zheng , Huazhu Xue , Zhanliang Yuan , Qian Cui , Peng Guo , Zushuai Wei , Peilin Song , Lixin Dong , Panpan Yao , Qiangqiang Yuan , Lingkui Meng , Jiancheng Shi
The successful deployment of multiple satellites equipped with passive microwave sensors has been pivotal for monitoring global soil moisture. Despite their importance, limitations including varying service durations, orbital scanning gaps, and differences in retrieval algorithms result in poor spatio-temporal consistency and coverage. This study introduces a two-stage paradigm to overcome the inconsistency of multi-sensors: Firstly, high-precision soil moisture is generated from SMAP L-band observations through the multi-channel collaborative algorithm (MCCA) as the physically anchored training target. Then, a long short-term memory (LSTM) network specifically designed for global gridded soil moisture dynamics is trained based on cross-calibrated brightness temperature observations (inclined orbit satellite sensors (TMI and GMI) and polar orbit satellite sensors (AMSR-E and AMSR2)) to obtain the high-quality retrieval accuracy of MCCA SMAP. Finally, the daily global soil moisture product (25 km resolution, 1997–2023) is provided by fusing the instantaneous soil moisture data of the four sensors from the model output. The study performed extensive validation with ground measurements and cross-validation with other datasets for both temporal and spatial consistency. The results indicate that the spatial distribution and seasonal variation patterns of MCCA-ML closely match those of MCCA SMAP, reflecting global climatic and geographic features. Verified by 24 dense global observation networks, the global r value of MCCA-ML SM is 0.76, the RMSE is 0.068 m3/m3, and the ubRMSE is 0.059 m3/m3, which well inherits the excellent performance of SMAP. During the service period of two or more satellites, the daily global land coverage of MCCA-ML SM usually exceeds 80 %, and it has a good ability to detect soil moisture.
成功部署装有无源微波传感器的多颗卫星对监测全球土壤湿度至关重要。尽管它们很重要,但包括不同的服务持续时间、轨道扫描间隙和检索算法差异在内的局限性导致了较差的时空一致性和覆盖范围。为了克服多传感器之间的不一致性,本研究引入了两阶段模式:首先,通过多通道协同算法(multi-channel collaborative algorithm, MCCA)将SMAP l波段观测数据作为物理锚定训练目标生成高精度土壤湿度;然后,利用倾斜轨道卫星传感器(TMI和GMI)和极轨道卫星传感器(AMSR-E和AMSR2)交叉标定的亮度温度观测数据,训练一个专为全球网格化土壤水分动态设计的长短期记忆(LSTM)网络,获得高质量的MCCA SMAP检索精度。最后,通过融合模型输出的4个传感器瞬时土壤湿度数据,得到全球土壤湿度日产品(25 km分辨率,1997-2023)。该研究对地面测量数据进行了广泛的验证,并与其他数据集进行了时间和空间一致性的交叉验证。结果表明,MCCA- ml的空间分布和季节变化特征与MCCA SMAP的空间分布和季节变化特征非常吻合,反映了全球气候和地理特征。经24个密集全球观测网验证,MCCA-ML SM的全局r值为0.76,RMSE为0.068 m3/m3, ubRMSE为0.059 m3/m3,很好地继承了SMAP的优良性能。在两颗或两颗以上卫星的服务期内,MCCA-ML SM的全球日土地覆盖率通常超过80% %,具有较好的土壤湿度探测能力。
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引用次数: 0
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Remote Sensing of Environment
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