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LiDAR-derived Lorenz-entropy metric for vertical structural complexity: A comparative study of tropical dry and moist forests 垂直结构复杂性的激光雷达衍生的lorenz -熵度量:热带干湿森林的比较研究
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-06 DOI: 10.1016/j.rse.2024.114545
Nooshin Mashhadi , Arturo Sanchez-Azofeifa , Ruben Valbuena
This study introduces an Entropy-based index: the Lorenz-entropy (LE) index, which we have developed by integrating Light Detection And Ranging (LiDAR), econometrics, and forest ecology. The main goal of the LE is to bridge the gap between theoretical entropy concepts and their practical applications in monitoring vertical structural complexity of tropical forest ecosystems. The LE index quantifies entropy by analyzing Relative Height (RH) metrics (representing a one-dimensional (1D) canopy structure metric) distributions from full-waveform LiDAR across successional stages in a tropical dry forest (TDF) and a tropical rainforest. To validate the LE trends derived from LiDAR, we extended the analysis using inventory-based two-dimensional (2D) and three-dimensional (3D) metrics, specifically basal area and biomass. The consistency of trends between the 1D LiDAR-derived LE and the inventory-based 2D and 3D metrics reinforces the LE's ability to capture and monitor structural complexity reliably across different measurement dimensions.
Our findings demonstrated that LE captures the changes in entropy as a function of successional stages, reflecting how canopy structure evolves towards homogeneity and complexity. Our statistical analysis revealed significant differences between successional stages (ANOVA, α = 0.05, p < 2e-16), with LE increasing substantially from early to late stages and plateauing at climax, where vertical structure (entropy) stabilizes. The mean LE increased by 1.70×102 between late and climax stages, with a small effect size (Cohen's d = 0.25), indicating minor differences in complexity. The LE index, calculated from biomass and basal area, confirming that as forests mature, entropy and vertical structural complexity increase. Furthermore, the sensitivity analysis showed that LE is most responsive to RHs variability during intermediate stages, suggesting that structural development is most dynamic during this phase. These results demonstrate the potential of the LE index as a tool for ecological analysis and monitoring forest dynamics.
本研究介绍了一种基于熵的指数:Lorenz-entropy (LE)指数,该指数是我们通过整合光探测与测距(LiDAR)、计量经济学和森林生态学而开发的。LE的主要目标是弥合理论熵概念与其在监测热带森林生态系统垂直结构复杂性方面的实际应用之间的差距。LE指数通过分析来自全波形激光雷达的相对高度(RH)指标(代表一维(1D)冠层结构指标)在热带干燥森林(TDF)和热带雨林连续阶段的分布来量化熵。为了验证激光雷达得出的LE趋势,我们使用基于库存的二维(2D)和三维(3D)指标扩展了分析,特别是基础面积和生物量。基于1D激光雷达的LE与基于库存的2D和3D指标之间趋势的一致性增强了LE在不同测量维度上可靠捕获和监测结构复杂性的能力。我们的研究结果表明,LE捕获了作为演替阶段函数的熵的变化,反映了冠层结构如何向同质性和复杂性演变。我们的统计分析显示,连续阶段之间存在显著差异(方差分析,α = 0.05, p <;e-16), LE从早期到后期大幅增加,在顶极处趋于稳定,垂直结构(熵)趋于稳定。在后期和高潮阶段,平均LE增加1.70×10−2×10−2,效应大小较小(Cohen’s d = 0.25),表明复杂性差异较小。从生物量和基面积计算的LE指数证实,随着森林的成熟,熵和垂直结构复杂性增加。此外,敏感性分析显示,LE在中间阶段对RHs变异性的响应最大,表明该阶段结构发育最动态。这些结果表明,LE指数具有作为生态分析和森林动态监测工具的潜力。
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引用次数: 0
Assessing and attributing flood potential in Brazil using GPS 3D deformation 利用GPS三维变形对巴西洪水潜力进行评估和归因
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-05 DOI: 10.1016/j.rse.2024.114535
Xinghai Yang , Linguo Yuan , Miao Tang , Zhongshan Jiang
Global Positioning System (GPS) instruments capture the daily crustal 3D deformation responding elastically to terrestrial water storage (TWS) variations, providing a powerful tool for hydrological studies. Here, we further expand the application of GPS in flood potential assessment. GPS vertical and horizontal crustal deformation are inverted into TWS variations using a 3D-Inversion model, and then a novel GPS-based modified flood potential index (GMFPI) is developed to assess and attribute the spatiotemporal patterns of flood potential in Brazil. The 3D-Inversion-derived TWS estimates show more spatial details compared to those derived from vertical deformation (1D-Inversion), with annual water thickness amplitudes of about 900 mm in the middle Amazon River, which is consistent with the Gravity Recovery and Climate Experiment Mascon solutions but is greater than the 1D-Inversion estimates. The comparison between in-situ discharge data and GMFPI indicates that GMFPI performs well in monitoring flood potential, showing Accuracy (ACC) values greater than 0.8 at basin scales. In four reported flood events, the spatial patterns of GMFPI and discharge show that the locations of those floods are accurately characterized by GMFPI. The attribution analysis of flood dynamics shows that precipitation in coastal regions can rapidly increase flood potential, while a large amount of precipitation in inland regions first replenishes unsaturated soil water and groundwater. Additionally, the daily GMFPI exhibits good consistency with daily discharge, demonstrating a capacity for monitoring floods at a sub-monthly scale. Our study highlights the improvement of 3D-Inversion to TWS estimates and the novel application of GPS in flood potential assessing with high spatiotemporal resolution, providing valuable insights for flood early warning and prevention.
全球定位系统(GPS)仪器捕获了地壳每日三维变形对陆地储水量变化的弹性响应,为水文研究提供了有力的工具。本文进一步拓展了GPS在洪水潜力评价中的应用。利用三维反演模型将GPS地壳垂直和水平变形转化为TWS变化,建立了基于GPS的修正洪水潜力指数(GMFPI),对巴西洪水潜力的时空格局进行了评价和属性化。基于3d反演的TWS估算结果比基于垂直形变(1d反演)的TWS估算结果显示出更多的空间细节,亚马逊河中部的年水厚度振幅约为900 mm,这与重力恢复和气候实验Mascon解决方案一致,但大于一维反演估算结果。实测流量数据与GMFPI的对比表明,GMFPI在流域尺度上的精度(ACC)大于0.8,具有较好的监测洪水潜力的效果。在4个已报道的洪水事件中,GMFPI和流量的空间格局表明GMFPI能准确表征洪水发生的位置。洪水动力学归因分析表明,沿海地区降水可迅速增加洪水潜力,而内陆地区大量降水首先补充非饱和土壤水和地下水。日GMFPI与日流量具有较好的一致性,具有分月尺度的洪水监测能力。我们的研究强调了3d反演对TWS估算的改进,以及GPS在高时空分辨率洪水潜力评估中的新应用,为洪水预警和预防提供了有价值的见解。
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引用次数: 0
Corrigendum to “HIDYM: A high-resolution gross primary productivity and dynamic harvest index based crop yield mapper” [Remote Sensing of Environment, 2024, 114301] “HIDYM:基于总初级生产力和动态收获指数的高分辨率作物产量制图器”的勘误表[遥感环境,2024,114301]
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-04 DOI: 10.1016/j.rse.2024.114548
Weiguo Yu , Dong Li , Hengbiao Zheng , Xia Yao , Yan Zhu , Weixing Cao , Lin Qiu , Tao Cheng , Yongguang Zhang , Yanlian Zhou
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引用次数: 0
A text-based, generative deep learning model for soil reflectance spectrum simulation in the solar range (400–2499 nm) 400-2499 nm太阳范围土壤反射率光谱模拟的文本生成深度学习模型
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-03 DOI: 10.1016/j.rse.2024.114527
Tong Lei, Brian N. Bailey
Soil spectral reflectance is a necessary input for land surface and radiative transfer models, and can be used to infer soil properties. Numerous soil reflectance inversion models have been developed based on mechanistic approaches, each with their own limitations. Mechanistic models based on radiative transfer theory are usually based on only a few input soil properties, whereas data-driven approaches are limited by high non-uniformity of available published datasets that severely limits the amount of data usable for model calibration. To address these limitations, a fully data-driven soil optics generative model (SOGM) for simulation of soil reflectance spectra from soil property inputs was developed based on the denoising diffusion probabilistic model (DDPM). The model was trained on an extensive dataset comprising nearly 180,000 soil spectra-property set pairs from 17 published datasets. The model generates soil reflectance spectra from text-based inputs describing soil properties and their values rather than only numerical values and labels in binary vector format, which means the model can handle variable formats for property reporting. Because the model is generative, it can simulate reasonable output spectra based on an incomplete set of available input properties, which becomes more reliable as the input property set becomes more complete. Two additional sub-models were also built to complement the SOGM: a spectral padding model that can fill in the gaps for spectra shorter than the target solar range (400 to 2499 nm), and a wet soil spectra model that can estimate the effects of water content on soil reflectance spectra given the dry spectrum predicted by the SOGM. It can also be easily integrated with other soil–plant radiation models used for remote sensing research such as PROSAIL and Helios 3D plant modeling software. The testing results of the SOGM on new datasets not included in model training demonstrated that the model can generate reasonable soil reflectance spectra based on available property inputs. Results also show soil clay/sand/silt fraction, organic carbon content, nitrogen content, and iron content tended to be important properties for spectra simulation. Inclusion of some trace minerals like nickel as model inputs decreased model performance because of their low concentrations and large propensity for ground-truth measurement error.
土壤光谱反射率是陆地表面和辐射转移模型的必要输入,可用于推断土壤性质。许多基于机械方法的土壤反射率反演模型已经被开发出来,每个模型都有自己的局限性。基于辐射传输理论的机制模型通常仅基于少量输入土壤特性,而数据驱动的方法受到可用已发表数据集高度不均匀性的限制,这严重限制了可用于模型校准的数据量。为了解决这些限制,基于去噪扩散概率模型(DDPM),开发了一个完全数据驱动的土壤光学生成模型(SOGM),用于模拟土壤属性输入的土壤反射光谱。该模型是在一个广泛的数据集上进行训练的,该数据集包括来自17个已发表数据集的近18万个土壤光谱属性集对。该模型从描述土壤属性及其值的基于文本的输入生成土壤反射光谱,而不仅仅是二进制矢量格式的数值和标签,这意味着该模型可以处理属性报告的可变格式。由于该模型是生成式的,它可以基于一组不完整的可用输入属性来模拟合理的输出光谱,随着输入属性集的完备,该模型的可靠性越来越高。为了补充SOGM,我们还建立了两个额外的子模型:一个是光谱填充模型,它可以填补小于目标太阳距离(400 ~ 2499 nm)的光谱空白;一个是湿土壤光谱模型,它可以在SOGM预测的干光谱的基础上估计含水量对土壤反射光谱的影响。它还可以很容易地与用于遥感研究的其他土壤-植物辐射模型(如PROSAIL和Helios 3D植物建模软件)集成。SOGM在未纳入模型训练的新数据集上的测试结果表明,该模型可以根据可用的属性输入生成合理的土壤反射光谱。结果还表明,土壤粘土/砂/粉粒组分、有机碳含量、氮含量和铁含量往往是光谱模拟的重要性质。将一些微量矿物质(如镍)作为模型输入会降低模型的性能,因为它们的浓度低,并且容易产生地面真值测量误差。
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引用次数: 0
Estimating actual evapotranspiration across China by improving the PML algorithm with a shortwave infrared-based surface water stress constraint 基于短波红外地表水应力约束的改进PML算法估算中国实际蒸散发
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-03 DOI: 10.1016/j.rse.2024.114544
Yongmin Yang
Accurate estimation of evapotranspiration (ET) is essential for the precise quantification of energy and water budgets under climate change. Remote sensing ET models provide an effective way to map ET across different spatial and temporal scales. However, conductance-based ET models such as PML_V2 are associated with limited or no water stress constraints on soil evaporation and canopy transpiration that could cause significant bias for sparse vegetation in arid and semi-arid areas. To meet this challenge for using conductance-based ET models, we proposed to use shortwave infrared information to serve as a water stress constraint to vegetation transpiration and soil evaporation, and an improved ET model (PML_SWIR) was proposed. The PML_SWIR model was calibrated with ET measurements from 21 eddy covariance flux towers distributed across China, and showed good performance for estimating ET (R2 = 0.70 and RMSE = 0.72 mm/day) for the cross-validation dataset. PML_SWIR outperformed PML_V2 in estimating ET for arid and semi-arid areas, indicated by RMSE being 7.86 and 25.93 mm/year lower and bias being 4.74 and 16.63 % less compared with PML_V2(China) and PML_V2(Global) for ET estimation over Xinjiang Province. In addition, PML_SWIR was noticeably better than PML_V2 for depicting the ET patterns for these seasonal rivers in the arid areas. The ET values estimated by PML_SWIR were further compared with other ET products. The results indicated that PML_SWIR well characterized the ET pattern in arid and semi-arid areas, and the estimated ET values showed good agreement with the water balance-based ET (R2 = 0.87, RMSE = 91.37 mm/year) in major river basins of China. The PML_SWIR ET estimates indicated that 20.2 % of the area of China increased significantly in ET over the study period, mainly due to vegetation greening caused by cropland expansion and the large-scale afforestation program. Overall, our results demonstrated that the incorporation of SWIR-based water stress constraints into the conductance-based ET model was a very promising way for accurately mapping ET in arid and semi-arid areas, and that the PML_SWIR model was highly applicable to regional high spatiotemporal ET mapping.
准确估算蒸散发对气候变化条件下的能量和水收支的精确量化至关重要。遥感ET模型提供了在不同时空尺度上绘制ET地图的有效途径。然而,基于电导的蒸散发模型(如PML_V2)对土壤蒸发和冠层蒸腾的水分胁迫限制有限或没有限制,这可能导致干旱和半干旱地区稀疏植被的显著偏差。为了解决基于电导的蒸散发模型存在的问题,我们提出了利用短波红外信息作为水分胁迫对植被蒸腾和土壤蒸发的约束,并提出了改进的蒸散发模型(PML_SWIR)。利用分布在中国各地的21个涡动相关通量塔的ET数据对PML_SWIR模型进行了校准,交叉验证数据显示PML_SWIR模型在估算ET方面表现良好(R2 = 0.70, RMSE = 0.72 mm/day)。与PML_V2(中国)和PML_V2(全球)相比,PML_SWIR对新疆省干旱和半干旱区ET的估计RMSE分别低7.86和25.93 mm/年,偏差分别小4.74和16.63%。此外,PML_SWIR对干旱区季节性河流ET的描述明显优于PML_V2。将PML_SWIR估算的ET值与其他ET产品进行比较。结果表明,PML_SWIR较好地表征了干旱区和半干旱区的ET格局,估算的ET值与中国主要流域基于水平衡的ET值吻合较好(R2 = 0.87, RMSE = 91.37 mm/年)。PML_SWIR ET估算结果表明,研究期间中国20.2%的地区ET显著增加,这主要是由于农田扩张和大规模植树造林造成的植被绿化。综上所述,我们的研究结果表明,将基于swir的水分胁迫约束纳入基于电导的ET模型是一种非常有前途的方法,可以精确地绘制干旱和半干旱区的ET, PML_SWIR模型在区域高时空ET制图中具有很高的适用性。
{"title":"Estimating actual evapotranspiration across China by improving the PML algorithm with a shortwave infrared-based surface water stress constraint","authors":"Yongmin Yang","doi":"10.1016/j.rse.2024.114544","DOIUrl":"10.1016/j.rse.2024.114544","url":null,"abstract":"<div><div>Accurate estimation of evapotranspiration (ET) is essential for the precise quantification of energy and water budgets under climate change. Remote sensing ET models provide an effective way to map ET across different spatial and temporal scales. However, conductance-based ET models such as PML_V2 are associated with limited or no water stress constraints on soil evaporation and canopy transpiration that could cause significant bias for sparse vegetation in arid and semi-arid areas. To meet this challenge for using conductance-based ET models, we proposed to use shortwave infrared information to serve as a water stress constraint to vegetation transpiration and soil evaporation, and an improved ET model (PML_SWIR) was proposed. The PML_SWIR model was calibrated with ET measurements from 21 eddy covariance flux towers distributed across China, and showed good performance for estimating ET (R<sup>2</sup> = 0.70 and RMSE = 0.72 mm/day) for the cross-validation dataset. PML_SWIR outperformed PML_V2 in estimating ET for arid and semi-arid areas, indicated by RMSE being 7.86 and 25.93 mm/year lower and bias being 4.74 and 16.63 % less compared with PML_V2(China) and PML_V2(Global) for ET estimation over Xinjiang Province. In addition, PML_SWIR was noticeably better than PML_V2 for depicting the ET patterns for these seasonal rivers in the arid areas. The ET values estimated by PML_SWIR were further compared with other ET products. The results indicated that PML_SWIR well characterized the ET pattern in arid and semi-arid areas, and the estimated ET values showed good agreement with the water balance-based ET (R<sup>2</sup> = 0.87, RMSE = 91.37 mm/year) in major river basins of China. The PML_SWIR ET estimates indicated that 20.2 % of the area of China increased significantly in ET over the study period, mainly due to vegetation greening caused by cropland expansion and the large-scale afforestation program. Overall, our results demonstrated that the incorporation of SWIR-based water stress constraints into the conductance-based ET model was a very promising way for accurately mapping ET in arid and semi-arid areas, and that the PML_SWIR model was highly applicable to regional high spatiotemporal ET mapping.</div></div>","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"318 ","pages":"Article 114544"},"PeriodicalIF":11.1,"publicationDate":"2024-12-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142760401","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
Archetypal crop trait dynamics for enhanced retrieval of biophysical parameters from Sentinel-2 MSI 从Sentinel-2 MSI中增强生物物理参数检索的作物原型性状动态
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-12-02 DOI: 10.1016/j.rse.2024.114510
Feng Yin , Philip E. Lewis , Jose L. Gómez-Dans , Thomas Weiß
<div><div>We present a new method for estimating biophysical parameters from Earth Observation (EO) data using a crop-specific empirical model based on the PROSAIL Radiative Transfer (RT) model, called an ‘archetype’ model. The first-order model presented uses maximum biophysical parameter magnitude, phenological and soil parameters to describe the spectral reflectance (400–2500 nm) of vegetation over time. The approach assumes smooth variation and archetypical coordination of crop biophysical parameters over time for a given crop. The form of coordination is learned from a large sample of observations. Using Sentinel-2 observations of maize from Northeast China in 2019, we map reflectance to biophysical parameters using an inverse model operator, synchronise the parameters to a consistent time frame using a double logistic model of <span><math><mrow><mi>L</mi><mi>A</mi><mi>I</mi></mrow></math></span>, then derive the model archetypes as the median value of the synchronised samples. We apply the model to estimate time series of biophysical parameters for different cereal crops using an ensemble framework with a weighted K-nearest neighbour solution, and validate the results with ground measurements of different crops collected near Munich, Germany in 2017 and 2018. The results show <span><math><mi>R</mi></math></span> values greater than 0.8 for leaf area index (<span><math><mrow><mi>L</mi><mi>A</mi><mi>I</mi></mrow></math></span>) and leaf brown pigment content (<span><math><msub><mrow><mi>C</mi></mrow><mrow><mi>b</mi><mi>r</mi><mi>o</mi><mi>w</mi><mi>n</mi></mrow></msub></math></span>), with an RMSE of 0.94 <span><math><mrow><msup><mrow><mtext>m</mtext></mrow><mrow><mn>2</mn></mrow></msup><mo>/</mo><msup><mrow><mtext>m</mtext></mrow><mrow><mn>2</mn></mrow></msup></mrow></math></span> for <span><math><mrow><mi>L</mi><mi>A</mi><mi>I</mi></mrow></math></span> and 0.15 for <span><math><msub><mrow><mi>C</mi></mrow><mrow><mi>b</mi><mi>r</mi><mi>o</mi><mi>w</mi><mi>n</mi></mrow></msub></math></span>. The chlorophyll content (<span><math><msub><mrow><mi>C</mi></mrow><mrow><mi>a</mi><mi>b</mi></mrow></msub></math></span>) and canopy water content (<span><math><mrow><mi>C</mi><msub><mrow><mi>C</mi></mrow><mrow><mi>w</mi></mrow></msub></mrow></math></span>) were retrieved at a higher level of accuracy, with <span><math><mi>R</mi></math></span> values around 0.9 and an RMSE of <span><math><mrow><mn>6</mn><mo>.</mo><mn>59</mn><mi>μ</mi><msup><mrow><mtext>g/cm</mtext></mrow><mrow><mn>2</mn></mrow></msup></mrow></math></span> for <span><math><msub><mrow><mi>C</mi></mrow><mrow><mi>a</mi><mi>b</mi></mrow></msub></math></span> and 0.03 <span><math><msup><mrow><mtext>g/cm</mtext></mrow><mrow><mn>2</mn></mrow></msup></math></span> for <span><math><mrow><mi>C</mi><msub><mrow><mi>C</mi></mrow><mrow><mi>w</mi></mrow></msub></mrow></math></span>. Comparison of forward-modelled hyperspectral reflectance with independent ground measures shows that the retrieved paramete
本文提出了一种基于PROSAIL辐射传输(RT)模型的作物特异性经验模型,即“原型”模型,从地球观测(EO)数据中估计生物物理参数的新方法。提出的一阶模型使用最大生物物理参数、物候和土壤参数来描述植被随时间的光谱反射率(400-2500 nm)。该方法假定作物生物物理参数随时间的平滑变化和典型协调。协调的形式是从大量的观察样本中习得的。利用2019年中国东北地区的Sentinel-2玉米观测数据,利用逆模型算子将反射率映射到生物物理参数,利用LAILAI的双逻辑模型将参数同步到一致的时间框架,然后推导模型原型作为同步样本的中位数。我们将该模型应用于使用加权k近邻解决方案的集成框架来估计不同谷类作物的生物物理参数时间序列,并使用2017年和2018年在德国慕尼黑附近收集的不同作物的地面测量数据验证结果。结果表明,叶面积指数(LAILAI)和叶棕色色素含量(cbrownbrown)的RR值均大于0.8,其中LAILAI的RMSE为0.94 m2/m2m2/m2, cbrownbrown的RMSE为0.15。叶绿素含量(CabCab)和冠层含水量(CCwCCw)的反演精度较高,RR值在0.9左右,RMSE为6.59μg/ cmm2, CabCab为26.59μg/cm2, CCwCCw为0.03 g/cm2。正演模拟高光谱反射率与独立地面测量数据的对比表明,反演参数占冠层反射率变化的90%,反射率单位的总体RMSE约为0.05。在考虑测量和预测不确定性的情况下,除由于冠层结构和林下植被的复杂性,叶片和冠层水分在季前和季后存在一定的变化外,其余各项的反演结果均在1σ1σ范围内。该方法为同时估计生物物理参数提供了一种新的约束形式,大大降低了问题的阶数。它适用于监测作物条件,其中生物物理参数随时间平稳变化,与每个原型形式一致。该方法可以针对其他冠层类型和冠层表示进行改进,并且可以对预期的平滑变化的冠层特征提供强有力的约束,以帮助解释电磁波谱不同区域的EO信号。
{"title":"Archetypal crop trait dynamics for enhanced retrieval of biophysical parameters from Sentinel-2 MSI","authors":"Feng Yin ,&nbsp;Philip E. Lewis ,&nbsp;Jose L. Gómez-Dans ,&nbsp;Thomas Weiß","doi":"10.1016/j.rse.2024.114510","DOIUrl":"10.1016/j.rse.2024.114510","url":null,"abstract":"&lt;div&gt;&lt;div&gt;We present a new method for estimating biophysical parameters from Earth Observation (EO) data using a crop-specific empirical model based on the PROSAIL Radiative Transfer (RT) model, called an ‘archetype’ model. The first-order model presented uses maximum biophysical parameter magnitude, phenological and soil parameters to describe the spectral reflectance (400–2500 nm) of vegetation over time. The approach assumes smooth variation and archetypical coordination of crop biophysical parameters over time for a given crop. The form of coordination is learned from a large sample of observations. Using Sentinel-2 observations of maize from Northeast China in 2019, we map reflectance to biophysical parameters using an inverse model operator, synchronise the parameters to a consistent time frame using a double logistic model of &lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mi&gt;L&lt;/mi&gt;&lt;mi&gt;A&lt;/mi&gt;&lt;mi&gt;I&lt;/mi&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt;, then derive the model archetypes as the median value of the synchronised samples. We apply the model to estimate time series of biophysical parameters for different cereal crops using an ensemble framework with a weighted K-nearest neighbour solution, and validate the results with ground measurements of different crops collected near Munich, Germany in 2017 and 2018. The results show &lt;span&gt;&lt;math&gt;&lt;mi&gt;R&lt;/mi&gt;&lt;/math&gt;&lt;/span&gt; values greater than 0.8 for leaf area index (&lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mi&gt;L&lt;/mi&gt;&lt;mi&gt;A&lt;/mi&gt;&lt;mi&gt;I&lt;/mi&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt;) and leaf brown pigment content (&lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;b&lt;/mi&gt;&lt;mi&gt;r&lt;/mi&gt;&lt;mi&gt;o&lt;/mi&gt;&lt;mi&gt;w&lt;/mi&gt;&lt;mi&gt;n&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt;), with an RMSE of 0.94 &lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;msup&gt;&lt;mrow&gt;&lt;mtext&gt;m&lt;/mtext&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mn&gt;2&lt;/mn&gt;&lt;/mrow&gt;&lt;/msup&gt;&lt;mo&gt;/&lt;/mo&gt;&lt;msup&gt;&lt;mrow&gt;&lt;mtext&gt;m&lt;/mtext&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mn&gt;2&lt;/mn&gt;&lt;/mrow&gt;&lt;/msup&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt; for &lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mi&gt;L&lt;/mi&gt;&lt;mi&gt;A&lt;/mi&gt;&lt;mi&gt;I&lt;/mi&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt; and 0.15 for &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;b&lt;/mi&gt;&lt;mi&gt;r&lt;/mi&gt;&lt;mi&gt;o&lt;/mi&gt;&lt;mi&gt;w&lt;/mi&gt;&lt;mi&gt;n&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt;. The chlorophyll content (&lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;a&lt;/mi&gt;&lt;mi&gt;b&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt;) and canopy water content (&lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;w&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt;) were retrieved at a higher level of accuracy, with &lt;span&gt;&lt;math&gt;&lt;mi&gt;R&lt;/mi&gt;&lt;/math&gt;&lt;/span&gt; values around 0.9 and an RMSE of &lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mn&gt;6&lt;/mn&gt;&lt;mo&gt;.&lt;/mo&gt;&lt;mn&gt;59&lt;/mn&gt;&lt;mi&gt;μ&lt;/mi&gt;&lt;msup&gt;&lt;mrow&gt;&lt;mtext&gt;g/cm&lt;/mtext&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mn&gt;2&lt;/mn&gt;&lt;/mrow&gt;&lt;/msup&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt; for &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;a&lt;/mi&gt;&lt;mi&gt;b&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; and 0.03 &lt;span&gt;&lt;math&gt;&lt;msup&gt;&lt;mrow&gt;&lt;mtext&gt;g/cm&lt;/mtext&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mn&gt;2&lt;/mn&gt;&lt;/mrow&gt;&lt;/msup&gt;&lt;/math&gt;&lt;/span&gt; for &lt;span&gt;&lt;math&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;msub&gt;&lt;mrow&gt;&lt;mi&gt;C&lt;/mi&gt;&lt;/mrow&gt;&lt;mrow&gt;&lt;mi&gt;w&lt;/mi&gt;&lt;/mrow&gt;&lt;/msub&gt;&lt;/mrow&gt;&lt;/math&gt;&lt;/span&gt;. Comparison of forward-modelled hyperspectral reflectance with independent ground measures shows that the retrieved paramete","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"318 ","pages":"Article 114510"},"PeriodicalIF":11.1,"publicationDate":"2024-12-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142758647","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
An advanced dorsiventral leaf radiative transfer model for simulating multi-angular and spectral reflection: Considering asymmetry of leaf internal and surface structure 一种模拟多角度反射和光谱反射的先进叶片背侧辐射传输模型:考虑叶片内部和表面结构的不对称性
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-30 DOI: 10.1016/j.rse.2024.114531
Dongjie Ran , Zhongqiu Sun , Shan Lu , Kenji Omasa
Understanding the optical properties of dorsiventral leaves and quantifying leaf biochemical traits through physical models are important for interpreting canopy radiative transfer and monitoring plant growth. Previous models, such as the dorsiventral leaf model (DLM), have effectively accounted for the inner asymmetry of the leaf but neglected the asymmetry of surface structures between the upper and lower epidermis. In this study, we found marked differences in bidirectional reflectance factors (BRF) between the adaxial and abaxial surfaces of leaves under multi-angular measurements due to surface structural distinctions. To address this asymmetry in both internal and surface leaf structures, we subsequently proposed an advanced DLM model (MADLM) for simulating both multi-angular and spectral BRF of two leaf sides, linking the angular reflection of leaf adaxial and abaxial sides to surface structural parameters (roughness and refractive index) based on microfacet theory. Results show that MADLM accurately simulates multi-angular and spectral BRF for both sides of dorsiventral leaves, and yields satisfactory retrieval accuracy of leaf traits from all observation geometries. For close-range hyperspectral imaging applications, we further introduced a simplified version, sMADLM, which characterizes the surface reflection of two leaf sides in terms of the product of a leaf-side dependent parameter and the wavelength-dependent Fresnel factor. The sMADLM improves the mapping accuracy of leaf biochemical traits by effectively reducing the surface reflection effects in dorsiventral leaves. The MADLM and sMADLM deepen our understanding of the optical properties of dorsiventral leaves and provide practical methods for retrieving leaf biochemical traits via optical remote sensing.
通过物理模型了解背侧叶片的光学特性,量化叶片生化特性,对解释冠层辐射转移和监测植物生长具有重要意义。以前的模型,如背侧叶模型(DLM),有效地考虑了叶片内部的不对称性,但忽略了上下表皮表面结构的不对称性。本研究发现,在多角度测量下,由于叶片表面结构的差异,叶片正面和背面的双向反射因子(BRF)存在显著差异。为了解决叶片内部和表面结构的这种不对称性,我们随后提出了一个先进的DLM模型(MADLM),用于模拟叶片两侧的多角度和光谱BRF,将叶片正面和背面的角反射与表面结构参数(粗糙度和折射率)联系起来。结果表明,MADLM能够准确地模拟叶片背面的多角度和光谱BRF,并能从所有观测几何形状中获得满意的叶片特征检索精度。对于近距离高光谱成像应用,我们进一步引入了一个简化版本sMADLM,它通过叶片侧相关参数和波长相关菲涅耳因子的乘积来表征叶片两侧的表面反射。sMADLM通过有效降低背侧叶片的表面反射效应,提高了叶片生化性状的制图精度。MADLM和sMADLM加深了我们对背侧叶片光学特性的认识,为通过光学遥感检索叶片生化特性提供了实用的方法。
{"title":"An advanced dorsiventral leaf radiative transfer model for simulating multi-angular and spectral reflection: Considering asymmetry of leaf internal and surface structure","authors":"Dongjie Ran ,&nbsp;Zhongqiu Sun ,&nbsp;Shan Lu ,&nbsp;Kenji Omasa","doi":"10.1016/j.rse.2024.114531","DOIUrl":"10.1016/j.rse.2024.114531","url":null,"abstract":"<div><div>Understanding the optical properties of dorsiventral leaves and quantifying leaf biochemical traits through physical models are important for interpreting canopy radiative transfer and monitoring plant growth. Previous models, such as the dorsiventral leaf model (DLM), have effectively accounted for the inner asymmetry of the leaf but neglected the asymmetry of surface structures between the upper and lower epidermis. In this study, we found marked differences in bidirectional reflectance factors (BRF) between the adaxial and abaxial surfaces of leaves under multi-angular measurements due to surface structural distinctions. To address this asymmetry in both internal and surface leaf structures, we subsequently proposed an advanced DLM model (MADLM) for simulating both multi-angular and spectral BRF of two leaf sides, linking the angular reflection of leaf adaxial and abaxial sides to surface structural parameters (roughness and refractive index) based on microfacet theory. Results show that MADLM accurately simulates multi-angular and spectral BRF for both sides of dorsiventral leaves, and yields satisfactory retrieval accuracy of leaf traits from all observation geometries. For close-range hyperspectral imaging applications, we further introduced a simplified version, sMADLM, which characterizes the surface reflection of two leaf sides in terms of the product of a leaf-side dependent parameter and the wavelength-dependent Fresnel factor. The sMADLM improves the mapping accuracy of leaf biochemical traits by effectively reducing the surface reflection effects in dorsiventral leaves. The MADLM and sMADLM deepen our understanding of the optical properties of dorsiventral leaves and provide practical methods for retrieving leaf biochemical traits via optical remote sensing.</div></div>","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"318 ","pages":"Article 114531"},"PeriodicalIF":11.1,"publicationDate":"2024-11-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142753404","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
Angular normalization of GOES-16 and GOES-17 land surface temperature over overlapping region using an extended time-evolving kernel-driven model 基于扩展时变核驱动模型的GOES-16和GOES-17重叠区地表温度角归一化
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-30 DOI: 10.1016/j.rse.2024.114532
Boxiong Qin , Shuisen Chen , Biao Cao , Yunyue Yu , Peng Yu , Qiang Na , Enqing Hou , Dan Li , Kai Jia , Yingpin Yang , Tian Hu , Zunjian Bian , Hua Li , Qing Xiao , Qinhuo Liu
Land surface temperature (LST) is an important parameter that critically contributes to Earth’ s climate. Thermal anisotropy is a major challenge that must be addressed while generating long-term LST products from satellites. For instance, the differences between GOES-16 and GOES-17 LST products caused by thermal anisotropy have not yet been resolved, which impacts the high-frequency monitoring of the land surface. The coupled contributions of the gap fraction and hotspot effects in the thermal infrared domain result in the existence of thermal anisotropy effect. The time-evolving kernel-driven model (TEKDM) is a recently proposed practical tool for conducting LST angular normalization for geostationary satellites. However, the existing six-parameter TEKDM considers only the hotspot effect and ignores the gap fraction effect, which may limit the TEKDM-based angular normalization method. In this study, we proposed an extended seven-parameter TEKDM considering both the gap fraction and hotspot effects and normalized the angular effect of GOES-16 and GOES-17 LST products over the overlapping region using this model. The accuracy of this seven-parameter TEKDM was evaluated using a physically based discrete anisotropic radiative transfer (DART) simulation dataset. Subsequently, the seven-parameter TEKDM-based angular normalization method was evaluated using the GOES-16 and GOES-17 LST products of the overlapping region for one year against ten AmeriFlux sites. The results showed that the seven-parameter TEKDM had a RMSE (MBE) of 0.36 K (0.0019 K). Compared with the RMSE of the NOAA-released GOES LST products, the seven-parameter TEKDM-based normalization method could reduce the RMSE of GOES-16 and GOES-17 LST products from 2.2 K and 2.6 K to 1.7 K, respectively, with a reduction of 0.5 K (22.7 %) and 0.9 K (34.6 %), respectively. Furthermore, the RMSE/MBE of GOES-17 LST exhibited a different diurnal variation pattern than that of GOES-16 LST, which could be explained by the different illumination-viewing geometries of the two satellites. This emphasizes the necessity of conducting angular normalization of current geostationary satellite LST products. The seven-parameter TEKDM provides a feasible method for generating long-term high-quality LST datasets for remote sensing communities.
地表温度(LST)是影响地球气候的一个重要参数。热各向异性是卫星产生长期地表温度产品时必须解决的主要挑战。例如,由于热各向异性导致的GOES-16和GOES-17地表温度产品差异尚未得到解决,这影响了对地表的高频监测。热红外区间隙分数和热点效应的耦合作用导致了热各向异性效应的存在。时间演化核驱动模型(TEKDM)是最近提出的一种用于地球静止卫星LST角归一化的实用工具。然而,现有的六参数TEKDM只考虑了热点效应,忽略了间隙分数效应,这可能会限制基于TEKDM的角归一化方法。在本研究中,我们提出了一个同时考虑间隙分数和热点效应的扩展的七参数TEKDM模型,并利用该模型对重叠区域上GOES-16和GOES-17 LST产品的角效应进行了归一化。使用基于物理的离散各向异性辐射传输(DART)模拟数据集评估了这种七参数TEKDM的准确性。随后,利用10个AmeriFlux站点的GOES-16和GOES-17重叠区域1年的LST产品,对基于tekdm的7参数角归一化方法进行了评估。结果表明,7参数TEKDM的RMSE (MBE)为0.36 K (0.0019 K),与noaa释放的GOES LST产品的RMSE相比,基于TEKDM的7参数归一化方法可将GOES-16和GOES-17 LST产品的RMSE分别从2.2 K和2.6 K降低到1.7 K,分别降低0.5 K(22.7%)和0.9 K(34.6%)。此外,GOES-17 LST的RMSE/MBE呈现出不同于GOES-16 LST的日变化模式,这可能与两颗卫星不同的光照观测几何形状有关。这就强调了对现有地球静止卫星LST产品进行角度归一化的必要性。7参数TEKDM为遥感群落长期高质量地表温度数据集的生成提供了一种可行的方法。
{"title":"Angular normalization of GOES-16 and GOES-17 land surface temperature over overlapping region using an extended time-evolving kernel-driven model","authors":"Boxiong Qin ,&nbsp;Shuisen Chen ,&nbsp;Biao Cao ,&nbsp;Yunyue Yu ,&nbsp;Peng Yu ,&nbsp;Qiang Na ,&nbsp;Enqing Hou ,&nbsp;Dan Li ,&nbsp;Kai Jia ,&nbsp;Yingpin Yang ,&nbsp;Tian Hu ,&nbsp;Zunjian Bian ,&nbsp;Hua Li ,&nbsp;Qing Xiao ,&nbsp;Qinhuo Liu","doi":"10.1016/j.rse.2024.114532","DOIUrl":"10.1016/j.rse.2024.114532","url":null,"abstract":"<div><div>Land surface temperature (LST) is an important parameter that critically contributes to Earth’ s climate. Thermal anisotropy is a major challenge that must be addressed while generating long-term LST products from satellites. For instance, the differences between GOES-16 and GOES-17 LST products caused by thermal anisotropy have not yet been resolved, which impacts the high-frequency monitoring of the land surface. The coupled contributions of the gap fraction and hotspot effects in the thermal infrared domain result in the existence of thermal anisotropy effect. The time-evolving kernel-driven model (TEKDM) is a recently proposed practical tool for conducting LST angular normalization for geostationary satellites. However, the existing six-parameter TEKDM considers only the hotspot effect and ignores the gap fraction effect, which may limit the TEKDM-based angular normalization method. In this study, we proposed an extended seven-parameter TEKDM considering both the gap fraction and hotspot effects and normalized the angular effect of GOES-16 and GOES-17 LST products over the overlapping region using this model. The accuracy of this seven-parameter TEKDM was evaluated using a physically based discrete anisotropic radiative transfer (DART) simulation dataset. Subsequently, the seven-parameter TEKDM-based angular normalization method was evaluated using the GOES-16 and GOES-17 LST products of the overlapping region for one year against ten AmeriFlux sites. The results showed that the seven-parameter TEKDM had a RMSE (MBE) of 0.36 K (0.0019 K). Compared with the RMSE of the NOAA-released GOES LST products, the seven-parameter TEKDM-based normalization method could reduce the RMSE of GOES-16 and GOES-17 LST products from 2.2 K and 2.6 K to 1.7 K, respectively, with a reduction of 0.5 K (22.7 %) and 0.9 K (34.6 %), respectively. Furthermore, the RMSE/MBE of GOES-17 LST exhibited a different diurnal variation pattern than that of GOES-16 LST, which could be explained by the different illumination-viewing geometries of the two satellites. This emphasizes the necessity of conducting angular normalization of current geostationary satellite LST products. The seven-parameter TEKDM provides a feasible method for generating long-term high-quality LST datasets for remote sensing communities.</div></div>","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"318 ","pages":"Article 114532"},"PeriodicalIF":11.1,"publicationDate":"2024-11-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142753405","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
Unsupervised object-based spectral unmixing for subpixel mapping 基于亚像素映射的无监督对象光谱解混
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-30 DOI: 10.1016/j.rse.2024.114514
Chengyuan Zhang , Qunming Wang , Peter M. Atkinson
Subpixel mapping (SPM) addresses the widespread mixed pixel problem in remote sensing images by predicting the spatial distribution of land cover within mixed pixels. However, conventional pixel-based spectral unmixing, a key pre-processing step for SPM, neglects valuable spatial contextual information and struggles with spectral variability, ultimately undermining SPM accuracy. Additionally, while extensively utilized, supervised spectral unmixing is labor-intensive and user-unfriendly. To address these issues, this paper proposes a fully automatic, unsupervised object-based SPM (UO-SPM) model that exploits object-scale information to reduce spectral unmixing errors and subsequently enhance SPM. Given that mixed pixels are typically located at the edges of objects (i.e., the inner part of objects is characterized by pure pixels), segmentation and morphological erosion are employed to identify pure pixels within objects and mixed pixels at the edges. More accurate endmembers are extracted from the identified pure pixels for the secondary spectral unmixing of the remaining mixed pixels. Experimental results on 10 study sites demonstrate that the proposed unsupervised object (UO)-based analysis is an effective model for enhancing both spectral unmixing and SPM. Specifically, the spectral unmixing results of UO show an average increase of 3.65 % and 1.09 % in correlation coefficient (R) compared to Fuzzy-C means (FCM) and linear spectral mixture model (LSMM)-derived coarse proportions, respectively. Moreover, the UO-derived results of four SPM methods (i.e., Hopfield neural network (HNN), Markov random field (MRF), pixel swapping (PSA) and radial basis function interpolation (RBF)) exhibit an average increase of 5.89 % and 3.04 % in overall accuracy (OA) across the four SPM methods and 10 study sites compared to the FCM and LSMM-based results, respectively. Moreover, the proportions of both mixed and pure pixels are more accurately predicted. The advantage of UO-SPM is more evident when the size of land cover objects is larger, benefiting from more accurate identification of objects.
亚像元映射(Subpixel mapping, SPM)通过预测混合像元内土地覆盖的空间分布,解决了遥感图像中普遍存在的混合像元问题。然而,传统的基于像元的光谱解混(SPM的关键预处理步骤)忽略了宝贵的空间背景信息,并与光谱变异性作斗争,最终降低了SPM的精度。此外,虽然广泛使用,监督光谱分解是劳动密集型和用户不友好的。为了解决这些问题,本文提出了一种全自动、无监督的基于目标的SPM (UO-SPM)模型,该模型利用目标尺度信息来减少光谱解混误差,从而增强SPM。考虑到混合像元通常位于物体的边缘(即物体的内部以纯像元为特征),采用分割和形态侵蚀来识别物体内部的纯像元和边缘的混合像元。从已识别的纯像元中提取更精确的端元,对剩余的混合像元进行二次光谱解混。在10个研究点上的实验结果表明,基于无监督目标(UO)的分析是提高光谱解混和SPM的有效模型。具体而言,UO的光谱分解结果显示,与模糊均值(FCM)和线性光谱混合模型(LSMM)衍生的粗比相比,相关系数(R)分别平均提高了3.65%和1.09%。此外,4种SPM方法(即Hopfield神经网络(HNN)、马尔科夫随机场(MRF)、像素交换(PSA)和径向基函数插值(RBF))在4种SPM方法和10个研究地点的总体精度(OA)平均比基于FCM和lsmm的结果分别提高了5.89%和3.04%。此外,混合像素和纯像素的比例都可以更准确地预测。oo - spm的优势在地表覆盖物规模较大时更为明显,有利于更准确地识别目标。
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引用次数: 0
Mapping and reconstruct suspended sediment dynamics (1986–2021) in the source region of the Yangtze River, Qinghai-Tibet Plateau using Google Earth Engine 基于谷歌Earth Engine的青藏高原长江源区悬沙动态(1986-2021)制图与重建
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-11-29 DOI: 10.1016/j.rse.2024.114533
Jinlong Li, Genxu Wang, Shouqin Sun, Jiapei Ma, Linmao Guo, Chunlin Song, Shan Lin
Using remote sensing to measure suspended sediment concentration (SSC) in mountainous rivers can compensate for the scarcity of in situ sediment observations, providing valuable direct supplementation to observational records. However, for inland rivers, remote sensing SSC assessments face challenges such as data quality, long-term water body changes, environmental noise, flood events, and the transferability of local calibrations. Here, we introduce and apply remote sensing big data techniques using 12,445 cloud-free Landsat 5, 7, and 8 satellite images to calibrate SSC in the source region of the Yangtze River (SRYR). Utilizing Google Earth Engine, we implemented a series of image preprocessing techniques and water fraction methods to extract precise inland river water masks. Then we used unsupervised K-Means clustering and machine learning algorithms to model the relationship between water optical properties and SSC. By integrating these methodologies, we achieved an average relative calibration error of 0.26 for each optical cluster, and an average relative station deviation of 0.24 based on in situ measurements, minimizing SSC calibration to acceptable levels. Additionally, our results reveal that geomorphic patterns significantly influence sediment yield and transport by regulating sediment sources and sinks, fluvial morphology, and water-sediment connectivity. Over the past two decades, approximately 35.73 % of the sediment relative to the basin outlet discharge in the SRYR has been temporarily stored or confined within sediment sinks. These methods and findings hold significant implications for assessing and projecting fluvial sediment dynamics and the associated ecological and environmental issues in ungauged cold headwater regions.
利用遥感测量山地河流悬浮泥沙浓度(SSC)可以弥补原位沉积物观测的不足,为观测记录提供有价值的直接补充。然而,对于内陆河流,遥感SSC评估面临着数据质量、长期水体变化、环境噪声、洪水事件和局部校准可转移性等挑战。本文介绍并应用遥感大数据技术,利用12445张无云Landsat 5、7和8卫星图像对长江源区(SRYR)的SSC进行校准。利用谷歌Earth Engine,实现了一系列图像预处理技术和水分方法,精确提取内河水掩模。然后,我们使用无监督K-Means聚类和机器学习算法来建模水光学性质与SSC之间的关系。通过整合这些方法,我们实现了每个光学集群的平均相对校准误差为0.26,基于原位测量的平均相对站偏差为0.24,将SSC校准降至可接受的水平。此外,我们的研究结果表明,地貌格局通过调节泥沙源和汇、河流形态和水沙连通性显著影响泥沙的产沙和输沙。在过去的20年里,相对于SRYR流域出水口流量,大约35.73%的泥沙被暂时储存或限制在泥沙汇内。这些方法和发现对于评估和预测未测量的冷源区的河流沉积动力学以及相关的生态和环境问题具有重要意义。
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引用次数: 0
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Remote Sensing of Environment
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