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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 : 2026-03-01 Epub 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
Unveiling the long-term cascading effects of the 2018 Baige landslide and subsequent outburst flood with satellite radar observations 利用卫星雷达观测揭示2018年白葛山滑坡及其溃决洪水的长期级联效应
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2026-01-10 DOI: 10.1016/j.rse.2026.115231
Bo Chen , Zhenhong Li , Chuang Song , Roberto Tomás , Chen Yu , Wu Zhu , Jianbing Peng
Landslide-dammed lakes (LDL) and landslide lake outburst flood (LLOF) can significantly alter the kinematic behavior of upstream and downstream landslides, posing severe threats to human life and infrastructure. However, the long-term impacts of LDL and LLOF on surrounding landslide stability remain poorly understood. In this study, we systematically examine the cascading effects triggered by the 2018 Baige LDL and LLOF on adjacent landslides, based on time series interferometric synthetic aperture radar (InSAR) analysis of 1437 satellite radar images. Unlike previous studies that focused on individual landslides or localized areas, we developed an automated method to detect the onset of landslide acceleration, leading to the establishment of an inventory of 65 accelerated landslides (ALs) and a quantitative evaluation of their controlling factors. Our results show that approximately 30 % of the flood-affected active landslides changed their deformation mechanisms, which can be categorized into five distinct types. Among the landslides accelerated by the Baige event, 43 % exhibited persistent acceleration, whereas 57 % showed signs of self-recovery. For the latter, deformation velocity typically decayed by 90 % within an average of 9.3 years after the outburst, returning to near pre-event levels. Furthermore, compared to 378 flood-involved but non-ALs, ALs preferentially occur on gentler slopes and in areas with lower vegetation cover. More notably, those ALs generally experienced greater flood depth, higher flow velocity, and stronger flood power. This study is the first to assess the long-lasting cascading effects of LDL and LLOF on creep landslides. These findings advance our understanding of LDL and LLOF-induced landslide mechanisms and offer valuable insights for the long-term risk assessment and geohazard mitigation of landslide-prone regions affected by similar cascading processes.
滑坡堰塞湖(LDL)和滑坡湖溃决洪水(LLOF)可以显著改变上下游滑坡的运动行为,对人类生命和基础设施构成严重威胁。然而,低密度脂蛋白和低密度脂蛋白对周围滑坡稳定性的长期影响仍然知之甚少。基于时间序列干涉合成孔径雷达(InSAR)对1437张卫星雷达图像的分析,系统研究了2018年白格低密度脂蛋白和低密度脂蛋白对相邻滑坡的级联效应。与以往专注于单个滑坡或局部区域的研究不同,我们开发了一种自动检测滑坡加速开始的方法,从而建立了65个加速滑坡(al)的清单,并对其控制因素进行了定量评估。结果表明,约30%的受洪水影响的活动性滑坡发生了变形机制的改变,可分为5种不同的类型。在因白葛山事件加速的滑坡中,43%表现出持续加速,57%表现出自我恢复的迹象。对于后者,变形速度通常在突出后平均9.3年内衰减90%,恢复到接近事件前的水平。此外,与378种与洪水有关但非ALs相比,ALs优先发生在较平缓的斜坡和植被覆盖较低的地区。更值得注意的是,这些al普遍具有更大的洪水深度,更高的流速和更强的洪水功率。这项研究首次评估了LDL和LLOF对蠕变滑坡的长期级联效应。这些发现促进了我们对低密度脂蛋白和低密度脂蛋白诱发的滑坡机制的理解,并为受类似级联过程影响的滑坡易发地区的长期风险评估和地质灾害缓解提供了有价值的见解。
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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 : 2026-03-01 Epub 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。
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引用次数: 0
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 : 2026-03-01 Epub 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
Annotation-free cloud masking for PlanetScope images in the Arctic via cross-platform ability transfer using deep learning and foundation models 利用深度学习和基础模型进行跨平台能力转移,对北极地区PlanetScope图像进行无注释云掩蔽
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2025-12-05 DOI: 10.1016/j.rse.2025.115138
Zhili Li , Yiqun Xie , Sergii Skakun , Xiaowei Jia , Gengchen Mai , William Lu , Matthew Tong , Zhihao Wang
Cloud masking is an essential task for satellite-based Earth monitoring, and the quality of cloud masks can directly impact the solutions of the downstream Earth monitoring tasks. While significant progress has been made especially for data with desired bands (e.g., thermal bands in Landsat-8), the masking quality on small satellites with higher resolution but fewer spectral bands is still unreliable at high latitudes, where confusion with snow and ice makes the task significantly more challenging. We propose a novel learning-enabled cross-platform ability transfer paradigm that offers a scalable and effective solution to tackle this challenge through a case study using PlanetScope images in the Arctic. A unique characteristic of the new paradigm is that it does not require manual annotations to be collected for PlanetScope images, which is often the bottleneck and the most time-consuming part of machine learning-based cloud masking, especially given the similarity between clouds and snow/ice. To realize this, our approach first designs and creates a new training dataset, Co-Clouds, which contains around 45,000 coincident pairs of PlanetScope and Landsat-8 image patches collected within a nearly simultaneous temporal window. This coincident dataset offers a way to generate large volumes of training data and builds a bridge to transfer Landsat-8’s stronger cloud masking skills in the Arctic to PlanetScope images via data-driven learning. We also show the feasibility of the ability transfer from spectral signatures (e.g., thermal bands) to spatial signatures (e.g., textures). Using our Co-Clouds dataset, we train several deep learning models including both regular-size deep learning models and large foundation models. To validate the quality of the masks, we further create a manually labeled cloud mask dataset for PlanetScope images in the Arctic. Both the quantitative and qualitative results show significant improvements over the current operational cloud masks by PlanetScope. For example, the large foundation models such as SegFormer achieve approximately 20 % higher overall accuracy and 28 % higher producer’s accuracy than the operational cloud masks, while maintaining comparable or better user’s accuracy exceeding 90 %. The new approach is also very easy to implement and extend to other platforms, opening new opportunities for broadcasting advanced skills from one platform to others.
云掩模是星载地球监测的重要任务,云掩模的质量直接影响下游地球监测任务的解决方案。虽然已经取得了重大进展,特别是对于具有所需波段的数据(例如Landsat-8的热波段),但在高纬度地区,具有更高分辨率但较少光谱波段的小卫星的掩面质量仍然不可靠,在高纬度地区,与雪和冰的混淆使任务更具挑战性。我们提出了一种新的支持学习的跨平台能力转移范式,该范式通过使用PlanetScope在北极的图像进行案例研究,为解决这一挑战提供了可扩展和有效的解决方案。新范式的一个独特之处在于,它不需要为PlanetScope图像收集手动注释,这通常是基于机器学习的云掩蔽的瓶颈和最耗时的部分,特别是考虑到云和雪/冰之间的相似性。为了实现这一点,我们的方法首先设计并创建了一个新的训练数据集,Co-Clouds,其中包含了在几乎同时的时间窗口内收集的大约45,000对重合的PlanetScope和Landsat-8图像补丁。这个同步数据集提供了一种生成大量训练数据的方法,并建立了一座桥梁,通过数据驱动的学习,将Landsat-8在北极更强大的云掩蔽技能转化为PlanetScope图像。我们还展示了从光谱特征(例如,热波段)到空间特征(例如,纹理)的能力转移的可行性。使用我们的Co-Clouds数据集,我们训练了几个深度学习模型,包括常规大小的深度学习模型和大型基础模型。为了验证掩模的质量,我们进一步为PlanetScope在北极的图像创建了一个手动标记的云掩模数据集。定量和定性结果都显示了PlanetScope在当前操作云掩模上的重大改进。例如,SegFormer等大型基础模型的总体精度比操作云掩模高约20%,生产者精度比操作云掩模高28%,同时保持相当或更好的用户精度超过90%。新方法也很容易实现并扩展到其他平台,为从一个平台向另一个平台传播高级技能提供了新的机会。
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引用次数: 0
Comparing the performance of different hyperspectral satellite imaging spectroscopy in mapping methane point-source emissions 比较不同高光谱卫星成像光谱在甲烷点源排放制图中的性能
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2026-01-03 DOI: 10.1016/j.rse.2025.115224
Fei Li , Keer Lin , Yingqi Yan , Shengxi Bai , Qidan Huang , Chenxi Feng , Shiwei Sun , Shaohua Zhao , Wei Zhou , Chunyan Zhou , Jun Lin , Xinwei Zhang , Yongguang Zhang
Accurate detection and quantification of methane point sources are critical for climate change mitigation. Recent advances in spaceborne hyperspectral imaging spectrometers offer new opportunities for global monitoring, yet systematic evaluation across missions remains limited. Here, we assess the spectral and radiometric performance of six operational hyperspectral satellites for methane plume detection. Results show that EMIT, EnMAP, and the GF5 series provide superior capabilities. EMIT achieved the best retrieval precision (σ = 18 ppb), followed by GF5–02-AHSI (σ = 31 ppb), EnMAP (σ = 33 ppb), and GF5-01 A-AHSI (σ = 47 ppb), outperforming PRISMA (σ = 84 ppb) and ZY1-02E-AHSI (σ = 71 ppb). These differences arise from finer spectral sampling distances (SSD: 7.4–8.4 nm), higher signal-to-noise ratios (SNR: 170–250), and more stable central wavelength shifts (0.3–1.3 nm) within the 2300 nm methane absorption region, which collectively enhance plume discrimination against surface backgrounds. In contrast, PRISMA and ZY1-02E-AHSI exhibit lower sensitivity due to larger wavelength shifts (up to 2.8 nm) and lower SNRs (140–150). Case studies illustrate successful detection of methane plumes from diverse sources, including oil and gas (O&G) infrastructure, coal mines, and a landfill site, highlighting both straightforward and challenging retrieval scenarios. This cross-sensor comparison underscores the importance of spectral fidelity and radiometric performance for methane monitoring. The findings provide a quantitative basis for prioritizing existing assets and guiding the design of future missions, emphasizing that high SNR and stable spectral calibration are key for advancing global detection of point-source methane emissions.
甲烷点源的准确探测和量化对于减缓气候变化至关重要。星载高光谱成像光谱仪的最新进展为全球监测提供了新的机会,但跨任务的系统评估仍然有限。在这里,我们评估了六颗用于甲烷羽流探测的高光谱卫星的光谱和辐射性能。结果表明,EMIT、EnMAP和GF5系列提供了优越的性能。EMIT的检索精度最高(σ = 18 ppb),其次是GF5-02-AHSI (σ = 31 ppb)、EnMAP (σ = 33 ppb)和GF5-01 A-AHSI (σ = 47 ppb),优于PRISMA (σ = 84 ppb)和ZY1-02E-AHSI (σ = 71 ppb)。这些差异源于更精细的光谱采样距离(SSD: 7.4-8.4 nm),更高的信噪比(SNR: 170-250),以及2300 nm甲烷吸收区内更稳定的中心波长偏移(0.3-1.3 nm),这些共同增强了对地表背景的羽流识别。相比之下,PRISMA和ZY1-02E-AHSI的灵敏度较低,因为波长位移较大(高达2.8 nm),信噪比较低(140-150)。案例研究成功地检测了来自不同来源的甲烷羽流,包括石油和天然气基础设施、煤矿和垃圾填埋场,突出了简单和具有挑战性的回收方案。这种跨传感器的比较强调了光谱保真度和辐射测量性能对甲烷监测的重要性。研究结果为现有资产的优先排序和指导未来任务的设计提供了定量基础,强调了高信噪比和稳定的光谱校准是推进全球点源甲烷排放检测的关键。
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引用次数: 0
Estimation of sea surface foam coverage and effective foam layer thickness from satellite microwave measurements 卫星微波测量估算海面泡沫覆盖和有效泡沫层厚度
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2025-12-11 DOI: 10.1016/j.rse.2025.115176
Xuchen Jin , Xianqiang He , Palanisamy Shanmugam , Yan Bai , Jianyun Ying , Qiankun Zhu , Yaqi Zhao , Delu Pan
Sea surface foam commonly represents the accumulation of bubbles on the sea surface caused by breaking waves and plays a critical role in the air-sea interaction process and climate research. Both foam coverage and foam layer thickness have a profound effect on sea surface emissivity for moderate to high wind speeds due to the high emissivity of foam at microwave bands. However, there is a lack of models to estimate sea foam layer thickness due to the limited experimental data and constrained empirical formulations. To address this limitation, we propose a dual-channel (L- and Ka-bands) method that utilizes passive microwave satellite measurements to estimate sea surface foam coverage and effective foam layer thickness over the global ocean. This method uses microwave measurements from the Aquarius/SAC-D and Soil Moisture Active Passive (SMAP) missions, together with observations from the WindSat instrument, to convert the top-of-atmosphere (TOA) brightness temperature (TB) to sea surface TBs and then isolate the foam-induced emission component. Because sea surface emissivity is sensitive to foam distributions, a foam emissivity model was developed and implemented to derive the foam layer parameters (coverage and thickness) as functions of wind speed. The retrieved foam coverage shows strong agreement with independent observations, with root mean square differences (RMSDs) of 0.87 % against field measurements and 0.38 % against satellite data. In addition, the retrieved effective foam thickness also shows close consistency with hydrodynamic model expectations. The global distributions of foam coverage and effective layer thickness were further retrieved and analyzed in this study, which demonstrated high potential of the proposed models compared to the previous methods and suggested that the combined use of L- band and Ka-band measurements from a single platform could improve the accuracy of foam coverage and effective layer thickness over the global ocean.
海面泡沫通常代表着破碎波浪在海面上造成的气泡积聚,在海气相互作用过程和气候研究中起着至关重要的作用。由于泡沫在微波波段的高发射率,因此泡沫覆盖面积和泡沫层厚度对中至高风速下的海面发射率都有深远的影响。然而,由于实验数据的限制和经验公式的约束,目前还缺乏估算海泡沫层厚度的模型。为了解决这一限制,我们提出了一种双通道(L和ka波段)方法,利用被动微波卫星测量来估计全球海洋的海面泡沫覆盖率和有效泡沫层厚度。该方法利用来自Aquarius/SAC-D和土壤湿度主动式被动(SMAP)任务的微波测量数据,以及来自WindSat仪器的观测数据,将大气顶(TOA)亮度温度(TB)转换为海面温度,然后分离泡沫诱发发射分量。由于海面发射率对泡沫分布很敏感,建立并实现了泡沫发射率模型,推导了泡沫层参数(覆盖面积和厚度)随风速的变化规律。回收的泡沫覆盖度与独立观测值非常吻合,与现场测量值的均方根差(rmsd)为0.87%,与卫星数据的均方根差(rmsd)为0.38%。此外,回收的有效泡沫厚度也显示出与水动力模型预期的密切一致性。本研究对全球泡沫覆盖率和有效层厚度的分布进行了进一步的反演和分析,结果表明,与以往的方法相比,所提出的模型具有很高的潜力,并表明在单一平台上联合使用L波段和ka波段测量可以提高全球海洋泡沫覆盖率和有效层厚度的精度。
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引用次数: 0
A novel SIF framework for decoupling hierarchical water stress impacts on winter wheat photosynthesis 一种解耦等级水分胁迫对冬小麦光合作用影响的SIF框架
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2025-12-24 DOI: 10.1016/j.rse.2025.115216
Kaiqi Du , Guilong Xiao , Xia Jing , Jie Zhang , Tingting Zhao , Xuecao Li , Yelu Zeng , Jianxi Huang
Drought has emerged as a critical constraint on sustainable agricultural development, particularly in water-scarce agroecosystems where multiscale hydrological stresses—such as rainfall deficits, soil moisture depletion, and groundwater exhaustion—interact to undermine crop productivity stability. However, current remote sensing frameworks lack the capacity to isolate and quantify the independent impacts of groundwater drought on crop photosynthesis and yield, leading to long-standing underestimation of deep-layer hydrological stress, especially in groundwater-dependent regions. To address this gap, we have proposed a dynamic monitoring framework based on solar-induced chlorophyll fluorescence (SIF) to assess the photosynthetic response characteristics of winter wheat across the Huang-Huai-Hai Plain under precipitation, surface moisture, and groundwater anomalies. This framework integrates dynamic time warping (DTW) for interannual phenological alignment and constructs a quantile-based dynamic baseline library that overcomes the limitations of traditional normality-based anomaly metrics. On this basis, we have developed a novel photosynthetic response anomaly index (PRAI) to characterize the spatiotemporal evolution of drought-induced photosynthetic stress. Results reveal that groundwater anomalies induce a significantly lagged crop response (mean lag ≈ +2.1 months, p < 0.01) and exert stronger influence on photosynthetic dynamics than soil surface moisture or rainfall. PRAI exhibits more concentrated and persistent negative anomalies during groundwater drought years, correlating more strongly with yield loss (R2 = 0.53) than during meteorological drought years (R2 = 0.30). Cross-validation using evapotranspiration (ET) and vegetation optical depth (VOD) further confirms PRAI reliability in capturing physiological stress. The proposed SIF-based dynamic monitoring framework not only deepens the understanding of crop eco-physiological response mechanisms to multiscale water stress, but also provides critical scientific support and methodological innovations for regional scale precision agriculture, crop model optimization, and sustainable water resource management.
干旱已成为可持续农业发展的关键制约因素,特别是在缺水的农业生态系统中,多尺度水文压力(如降雨不足、土壤水分枯竭和地下水枯竭)相互作用,破坏了作物生产力的稳定性。然而,目前的遥感框架缺乏分离和量化地下水干旱对作物光合作用和产量的独立影响的能力,导致长期低估深层水文应力,特别是在依赖地下水的地区。为了解决这一问题,我们提出了一个基于太阳诱导叶绿素荧光(SIF)的动态监测框架,以评估黄淮海平原冬小麦在降水、地表湿度和地下水异常下的光合响应特征。该框架集成了动态时间规整(DTW)用于年际物候比对,并构建了一个基于分位数的动态基线库,克服了传统基于正态的异常度量的局限性。在此基础上,我们建立了一个新的光合响应异常指数(PRAI)来表征干旱诱导的光合胁迫的时空演变。结果表明,地下水异常导致作物响应显著滞后(平均滞后≈+2.1个月,p < 0.01),对光合动态的影响强于土壤表面水分和降雨。PRAI在地下水干旱年表现出更集中和持续的负异常,与产量损失的相关性(R2 = 0.53)比气象干旱年更强(R2 = 0.30)。利用蒸散发(ET)和植被光学深度(VOD)进行交叉验证进一步证实了PRAI在捕捉生理胁迫方面的可靠性。基于sif的作物动态监测框架不仅深化了对作物多尺度水分胁迫生态生理响应机制的认识,而且为区域尺度精准农业、作物模式优化和水资源可持续管理提供了重要的科学支持和方法创新。
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引用次数: 0
Large-scale tree-level mapping of forest structure including species type with remote sensing data and ground measurements 基于遥感数据和地面测量的森林结构包括物种类型的大尺度树级制图
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2026-01-05 DOI: 10.1016/j.rse.2025.115223
J. Kostensalo , P. Packalen , M. Kuronen , L. Mehtätalo , S. Tuominen , M. Myllymäki
Remote-sensing based tree maps can be used to calculate various diversity indices, but the detection probability of trees depends on size and species. We propose a novel approach combining individual tree detection (ITD) with resampling corrections (+R) which aims to simultaneously correct the size, species, and spatial distribution of trees using scalable algorithms. Using airborne laser scanning, optical data, and ground measurements, we demonstrate the compatibility of ITD+R with two different types of forests and ITD algorithms, as well as its scalability to areas exceeding 3000 km2. The tree maps were evaluated using plot-level variables and benchmarked against area-based k nearest neighbors (k-NN). The ITD+R improved ITD results for most studied metrics, with the Shannon index being an exception, and even outperformed k-NN in predicting dominant height in managed stands, though k-NN still outperformed for stem density and volume. The ITD+R approach was shown to be adaptable to various diversity indices which it has not been specifically trained on, with 254 m2 plot-level predictions correlating at r=0.42–0.91. While ITD trees could be classified with OA=82.0%–86.6% to pine, spruce, and deciduous, further research is needed to account for rare tree species, as low prevalence results in a large number of false detections which cannot be sufficiently addressed with classification alone.
基于遥感的树图可用于计算各种多样性指数,但树木的检测概率取决于大小和种类。我们提出了一种结合单个树检测(ITD)和重采样校正(+R)的新方法,该方法旨在使用可扩展算法同时校正树木的大小、种类和空间分布。利用机载激光扫描、光学数据和地面测量,我们证明了ITD+R与两种不同类型森林和ITD算法的兼容性,以及它在超过3000平方公里的区域内的可扩展性。使用plot-level变量对树图进行评估,并以基于区域的kk近邻(kk- nn)为基准。除Shannon指数外,ITD+R在大多数研究指标上都改善了ITD结果,在预测管理林分的优势高度方面甚至优于kk-NN,尽管kk-NN在树干密度和体积方面仍然优于kk-NN。研究表明,过渡段+R方法适用于尚未专门训练的各种多样性指数,254 m2的样点水平预测的相关系数为0.42-0.91。虽然过渡段乔木的OA值为82.0% ~ 86.6%,可分类为松树、云杉和落叶乔木,但由于低流行率导致大量误检,单靠分类无法充分解决,因此需要进一步研究以解释稀有树种。
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引用次数: 0
Space-based assessment of NOx emissions from global oil and gas fields: Bridging the gap in current emission inventories 全球油气田氮氧化物排放的天基评估:弥合当前排放清单的差距
IF 11.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2026-03-01 Epub Date: 2026-01-03 DOI: 10.1016/j.rse.2025.115229
Piyushkumar N. Patel , Ritesh Gautam , Mark Omara
<div><div>Identifying air pollutant sources and quantifying related emissions provides crucial information towards improving global air quality and public health. However, emission inventories for oil and gas (OG) activities inadequately represent nitrogen oxide (NO<sub>x</sub>) emissions—a key precursor to tropospheric ozone and secondary aerosols—with notable discrepancies identified. Satellite remote sensing provides a unique vantage point to map and quantify these emissions consistently on a global scale. Here, we quantify annual NO<sub>x</sub> emissions from 44 major OG basins distributed globally, utilizing TROPOspheric Monitoring Instrument (TROPOMI) nitrogen dioxide (NO<sub>2</sub>) observations with the divergence flux method. In addition, we use the spaceborne Visible Infrared Imaging Radiometer Suite (VIIRS) natural gas flaring detections to further constrain satellite-derived NO<sub>x</sub> emissions. The divergence flux method, which addresses 3D topography corrections and chemical loss of NO<sub>x</sub> while accounting for wind-induced flux smearing, provides a robust approach for estimating NO<sub>x</sub> emissions. This top-down approach resolves emissions at the facility and basin scale (0.01° x 0.01°), enabling direct quantification of a major gap in current bottom-up inventories. Our findings reveal significant differences between satellite observations and established inventories, which systematically underestimate OG sector emissions. A direct comparison of our TROPOMI-derived NO<sub>x</sub> emissions against the existing inventories suggests that EDGARv6.1 underestimates onshore emissions by 61 % and offshore emissions by 26 %. The discrepancy is even more pronounced for the CAMS-GLOB-ANT_v5.3 inventory, which underestimates onshore and offshore emissions by 78 % and 92 %, respectively. These findings hold significance for global emission assessments, demonstrating that current inventories are missing a substantial source of NO<sub>x</sub> pollution, particularly from OG fields. Furthermore, our approach provides detailed spatial emission maps that enhance the granularity in depicting NO<sub>x</sub> distribution with error analysis (uncertainties: 32 %-54 %) supporting that inventory discrepancies are statistically significant, representing structural deficiencies rather than measurement error. We further explore the variations in the correlation between NO<sub>x</sub> emissions with OG production volumes and CH<sub>4</sub> concentrations across different OG basins in North America. The observed co-locations and correlations provide important insights into co-pollution emission characteristics of methane and NO<sub>x</sub>, that are respectively a potent greenhouse gas and a reactive air quality pollutant, linked to be originating from oil and gas activity. These findings have important implications for regulatory monitoring and verification, particularly for addressing emissions transparency requirements under internationa
确定空气污染源和量化相关排放为改善全球空气质量和公众健康提供了重要信息。然而,石油和天然气(OG)活动的排放清单不能充分代表氮氧化物(NOx)的排放,氮氧化物是对流层臭氧和二次气溶胶的关键前体,两者之间存在显著差异。卫星遥感提供了一个独特的优势,可以在全球范围内一致地绘制和量化这些排放。本文利用对流层监测仪器(TROPOMI)二氧化氮(NO2)的发散通量法观测数据,对分布在全球44个主要ogg盆地的年NOx排放量进行了量化。此外,我们使用星载可见光红外成像辐射计套件(VIIRS)进行天然气燃除检测,以进一步限制卫星产生的氮氧化物排放。散度通量方法解决了三维地形校正和氮氧化物的化学损失,同时考虑了风致通量涂布,为估计氮氧化物排放提供了一种可靠的方法。这种自上而下的方法解决了设施和流域尺度(0.01°x 0.01°)的排放问题,从而可以直接量化目前自下而上清单中的主要差距。我们的研究结果揭示了卫星观测与既定清单之间的显著差异,后者系统性地低估了OG部门的排放量。将tropomi衍生的氮氧化物排放量与现有清单进行直接比较表明,EDGARv6.1低估了陆上排放量61%,低估了海上排放量26%。CAMS-GLOB-ANT_v5.3清单的差异更为明显,它分别低估了78%和92%的陆上和海上排放量。这些发现对全球排放评估具有重要意义,表明目前的清单遗漏了氮氧化物污染的主要来源,特别是来自OG油田。此外,我们的方法提供了详细的空间排放图,通过误差分析(不确定性:32% - 54%)增强了描述氮氧化物分布的粒度,支持库存差异在统计上显着,代表结构缺陷而不是测量误差。我们进一步探讨了北美不同OG盆地中NOx排放量与OG产量和CH4浓度之间的相关性变化。观察到的共分布和相关性为甲烷和氮氧化物的共污染排放特征提供了重要的见解,这两种气体分别是一种强效温室气体和一种反应性空气质量污染物,与石油和天然气活动有关。这些发现对监管监测和核查具有重要意义,特别是对解决国际气候框架下的排放透明度要求。
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Remote Sensing of Environment
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