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Illumination correction for close-range hyperspectral images using spectral invariants and random forest regression 利用光谱不变式和随机森林回归对近距离高光谱图像进行光照校正
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-30 DOI: 10.1016/j.rse.2024.114467
Olli Ihalainen , Theresa Sandmann , Uwe Rascher , Matti Mõttus
Identifying materials and retrieving their properties from spectral imagery is based on their spectral reflectance calculated from the ratio of reflected radiance to the incident irradiance. However, obtaining the true reflectances of materials within a vegetation canopy is challenging given the varying illumination conditions across the canopy – i.e., the irradiance incident on a surface inside the canopy – caused by its complex 3D structure. Instead, in remote sensing, reflectances are calculated from the ratio of the spectral radiance measured by the sensor to the top-of-canopy (TOC) spectral irradiance, resulting in apparent reflectances that can significantly differ from the true reflectance spectra. To address this issue, we present a physically based illumination correction method for retrieving the true reflectances from close-range hyperspectral TOC reflectance images. The method uses five spectral invariant parameters to predict the illumination conditions from TOC reflectance and compute the corrected spectrum using a physically based model. For computational efficiency, the spectrally invariant parameters were retrieved using random forest regression trained with Monte Carlo ray tracing simulations. The method was tested on close-range imaging spectroscopy data from dense and sparse vegetation canopies for which reference in situ spectral measurements were available. This work is a step toward resolving the 3D radiation regime in vegetation canopies from TOC hyperspectral imagery. The retrieved spectral invariants provide a physical connection to the structure of the observed vegetation canopy. The true spectra of artificial and natural materials in a vegetation canopy, determined under various illumination conditions, allow their more robust (bio)chemical characterization, opening new applications in vegetation monitoring and material detection, and machine learning makes it possible to apply the method rapidly to large hyperspectral image sets.
从光谱图像中识别材料并检索其属性的依据是根据反射辐射率与入射辐照度之比计算出的材料光谱反射率。然而,由于植被冠层复杂的三维结构,冠层各处的光照条件(即入射到冠层内部表面的辐照度)各不相同,因此获取植被冠层内物质的真实反射率具有挑战性。相反,在遥感技术中,反射率是根据传感器测量到的光谱辐射率与冠层顶部(TOC)光谱辐照度之比计算得出的,因此表观反射率可能与真实的反射率光谱存在很大差异。为了解决这个问题,我们提出了一种基于物理的光照校正方法,用于从近距离高光谱 TOC 反射图像中检索真实的反射率。该方法使用五个光谱不变参数来预测 TOC 反射率的光照条件,并使用基于物理的模型计算校正光谱。为了提高计算效率,光谱不变参数是通过蒙特卡洛射线追踪模拟训练的随机森林回归法获得的。该方法在茂密和稀疏植被树冠的近距离成像光谱数据上进行了测试,这些数据均可作为原位光谱测量的参考。这项工作朝着从 TOC 高光谱图像中解析植被冠层的三维辐射机制迈出了一步。检索到的光谱不变量为观测到的植被冠层结构提供了物理联系。在各种光照条件下确定植被冠层中人工和天然材料的真实光谱,可对其进行更可靠的(生物)化学特征描述,为植被监测和材料检测开辟了新的应用领域。
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引用次数: 0
Nationwide operational mapping of grassland first mowing dates combining machine learning and Sentinel-2 time series 结合机器学习和 Sentinel-2 时间序列绘制全国范围的草地首次刈割日期操作图
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-30 DOI: 10.1016/j.rse.2024.114476
Henry Rivas , Hélène Touchais , Vincent Thierion , Jerome Millet , Laurence Curtet , Mathieu Fauvel
Grassland dynamics are modulated by management intensity and impact overall ecosystem functioning. In mowed grasslands, the first mowing date is a key indicator of management intensification. The aim of this work was to assess several supervised regression models for mapping grassland first mowing date at national-level using Sentinel-2 time series. Three deep-learning architectures, two conventional machine learning models and two threshold-based methods (fixed and relative) were compared. Algorithms were trained/calibrated and tested from field observations, using a spatial cross-validation approach. Our findings showed that time aware deep-learning models – Lightweight Temporal Attention Encoder (LTAE) and 1D Convolutional Neural Network (1D-CNN) – yielded higher performances compared to Multilayer Perceptron, Random Forest and Ridge Regression models. Threshold-based methods under-performed compared to all other models. Best model (LTAE) mean absolute error was within six days with a coefficient of determination of 0.52. Additionally, errors were accentuated at extreme (late/early) mowing dates, which were underrepresented in the data set. Oversampling techniques did not improve predicting extreme mowing dates. Finally, the best prediction accuracy was obtained when the number of clear dates surrounding the mowing event was greater than 2. Our outputs evidenced time aware deep-learning models’ potential for large-scale grassland first mowing event monitoring. A national-level map was produced to support bird-life monitoring or public policies for biodiversity and agro-ecological transition in France.
草地动态受管理强度的调节,并影响生态系统的整体功能。在刈割草地上,首次刈割日期是管理强度的一个关键指标。这项工作的目的是评估利用哨兵-2 时间序列绘制国家级草原首次刈割日期图的几种监督回归模型。对三种深度学习架构、两种传统机器学习模型和两种基于阈值的方法(固定和相对)进行了比较。采用空间交叉验证方法,根据实地观测结果对算法进行了训练/校准和测试。我们的研究结果表明,与多层感知器、随机森林和岭回归模型相比,时间感知深度学习模型--轻量级时空注意力编码器(LTAE)和一维卷积神经网络(1D-CNN)--性能更高。与所有其他模型相比,基于阈值的方法表现不佳。最佳模型(LTAE)的平均绝对误差在六天之内,决定系数为 0.52。此外,极端(晚/早)割草日期的误差更大,这在数据集中体现不足。过度取样技术并没有改善对极端割草日期的预测。最后,当围绕割草事件的晴朗日期数大于 2 时,预测准确率最高。我们的成果证明了时间感知深度学习模型在大规模草原首次刈割事件监测中的潜力。绘制的国家级地图可为法国的鸟类生活监测或生物多样性和农业生态转型公共政策提供支持。
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引用次数: 0
Resolution enhancement of SMOS brightness temperatures: Application to melt detection on the Antarctic and Greenland ice sheets 提高SMOS亮度温度的分辨率:应用于南极和格陵兰冰盖的融化探测
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-25 DOI: 10.1016/j.rse.2024.114469
Pierre Zeiger , Ghislain Picard , Philippe Richaume , Arnaud Mialon , Nemesio Rodriguez-Fernandez
A large part of the surface of the Greenland Ice Sheet (GrIS) and the margins of Antarctica are melting every summer, affecting their surface mass balance. Wet/dry snow status has been detected for decades using the peaks of brightness temperature at 19 GHz, and more recently at L-band (1.4 GHz) using both the SMOS and SMAP missions. SMOS owns a longer time series than SMAP with data since 2010, but the 52.5°incidence bin in the Level 3 (L3) product from Centre Aval de Traitement des Données SMOS (CATDS) that was previously used to detect melt suffers from a coarse spatial resolution. For this reason, we developed a new SMOS enhanced resolution brightness temperature (TB) product building on the radiometer version of the Scatterometter Image Reconstruction (rSIR) algorithm. We also exploited the SMOS L1C observations near 40°incidence angle instead of 52.5°as the native spatial resolution of SMOS is better at low incidence. The new product is posted on a 12.5 km polar stereographic grid and covers all the GrIS and Antarctica for 2010–2024 with twice-daily morning and afternoon acquisitions. The effective spatial resolution was evaluated to 30 km, a 30% enhancement compared to the SMOS L3TB at 40°and almost a 50% enhancement compared to the SMOS L3TB at 52.5°. Then, we applied a melt detection algorithm to both the enhanced resolution product at 40°and the L3TB product at 52.5°which is used in the literature. The spatial resolution enhancement results not only in the detection of smaller melt regions but also in a widespread increase in the annual number of melt days. This increase is larger than 30 days per year in the GrIS percolation area and on multiple Antarctic ice shelves. This is primarily due to the mix of dry and wet snow regions near the ice shelves grounding line, resulting in lower brightness temperature peaks in the SMOS L3TB product due to a large power spread. These findings highlight the dependence of melt detection in particular, and geophysical applications in general, on the spatial resolution of passive microwave observations. This study provides a new open dataset suitable to monitor melt at the surface and at depth on the two main ice-sheets.
格陵兰冰原(GrIS)的大部分表面和南极洲边缘每年夏季都在融化,影响了其表面质量平衡。几十年来,利用 19 千兆赫的亮度温度峰值,以及最近利用 SMOS 和 SMAP 任务的 L 波段(1.4 千兆赫),对干/湿雪状态进行了探测。SMOS拥有比SMAP更长的时间序列,从2010年起就有数据,但以前用于探测融雪的SMOS数据处理中心(CATDS)三级(L3)产品中的52.5°入射区空间分辨率较低。因此,我们在散射计图像重建(rSIR)算法辐射计版本的基础上,开发了一种新的 SMOS 增强分辨率亮度温度(TBTB)产品。我们还利用了 SMOS L1C 在 40°入射角附近而不是 52.5°入射角附近的观测数据,因为在低入射角时 SMOS 的本机空间分辨率更高。新产品发布在一个 12.5 千米的极地立体网格上,覆盖了 2010-2024 年的所有南极洲和南极洲,每天上午和下午各采集两次。经评估,其有效空间分辨率为∼∼30 千米,与 40° 时的 SMOS L3TB 相比提高了 30%,与 52.5° 时的 SMOS L3TB 相比提高了近 50%。然后,我们将文献中使用的熔融探测算法应用于 40° 的增强分辨率产品和 52.5° 的 L3TB 产品。空间分辨率的提高不仅使我们探测到了更小的融化区域,还使年融化天数普遍增加。在 GrIS 渗流区和多个南极冰架上,年融化天数的增加超过了 30 天。这主要是由于冰架接地线附近的干雪区和湿雪区混杂在一起,导致 SMOS L3TB 产品中的亮度温度峰值因功率差较大而降低。这些发现凸显了融雪探测以及地球物理应用对被动微波观测空间分辨率的依赖性。这项研究提供了一个新的开放数据集,适合监测两大冰原表面和深层的融化情况。
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引用次数: 0
Forest disturbance detection in Central Europe using transformers and Sentinel-2 time series 利用变压器和 Sentinel-2 时间序列探测中欧森林干扰
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-24 DOI: 10.1016/j.rse.2024.114475
Christopher Schiller , Jonathan Költzow , Selina Schwarz , Felix Schiefer , Fabian Ewald Fassnacht
Forests provide important ecosystem functions such as carbon sequestration and climate regulation, particularly in countries with high forest cover. Climate change-induced extreme weather events have a negative impact on many forest ecosystems. In Germany, for instance, the drought of the years 2018 until 2020 resulted in signs of damage in almost 80% of trees. This decline in forest vitality has additionally led to severe bark beetle infestations and widespread tree mortality, posing significant challenges to forest managers to obtain a complete picture of the state of their forests. Since a completely ground-based monitoring of forest condition is not feasible due to the forests' vast extent, remote sensing and particularly multispectral satellite image time series (SITS) analysis were suggested as efficient alternatives. Transformers, a state-of-the-art Deep Learning (DL) architecture, have shown promising results in the classification of multivariate SITS for other applications. Here, we use Transformers in combination with Sentinel-2 (S2) time series data to test if they can improve forest disturbance detection capabilities in comparison to conventional methods by automatically extracting relevant information from background variability throughout the whole time series. To match the large training data needs of Transformers, we use a two-step approach including pre-training and finetuning. During pre-training, we use outputs of earlier presented SITS approaches, while during finetuning, we use detailed reference data of known disturbances covering between 10 and 100% of a Sentinel-2 pixel as extracted from aerial images. We test three setups: DL base using ten S2 bands, DL IND using ten vegetation indices (VIs), and DL +IND utilising both as model input. F1-scores across all of our six study sites range between approx. 0.65 (DL +IND) and 0.72 (DL base) in a binary classification (undisturbed vs. disturbed) when considering both full and partial disturbances. DL base outperforms the other setups in forest disturbance detection, and detects disturbance extents as small as 40 m2 within pixels of 100 m2 size. Given the best performance of DL base, handcrafted vegetation indices (VIs) do not improve the model. Our model is competitive with existing approaches and slightly outperforms most earlier reported results, even though a direct comparison is challenging. Considering the option to further refine our trained model if additional reference data becomes available over time, we conclude that a combination of Transformers and Sentinel-2 time series can be developed into an effective tool for forest disturbance monitoring of Central European forests at fine spatial grain.
森林具有重要的生态系统功能,如碳吸收和气候调节,尤其是在森林覆盖率高的国家。气候变化引发的极端天气事件对许多森林生态系统产生了负面影响。例如,在德国,2018 年至 2020 年的干旱导致近 80% 的树木出现受损迹象。森林生命力的下降还导致了严重的树皮甲虫虫害和大面积的树木死亡,这给森林管理者全面了解森林状况带来了巨大挑战。由于森林幅员辽阔,完全基于地面的森林状况监测并不可行,因此遥感,特别是多光谱卫星图像时间序列(SITS)分析被认为是有效的替代方法。Transformers是一种最先进的深度学习(DL)架构,在其他应用的多变量SITS分类中显示出了良好的效果。在此,我们将 Transformers 与哨兵-2(Sentinel-2,S2)时间序列数据相结合,测试它们是否能通过自动从整个时间序列的背景变异中提取相关信息,从而与传统方法相比提高森林干扰检测能力。为了满足 Transformers 的大量训练数据需求,我们采用了包括预训练和微调在内的两步方法。在预训练过程中,我们使用了之前介绍的 SITS 方法的输出结果;而在微调过程中,我们使用了从航空图像中提取的已知干扰的详细参考数据,其覆盖范围为哨兵-2 像素的 10%到 100%。我们测试了三种设置:DL base 使用 10 个 S2 波段,DL IND 使用 10 个植被指数 (VI),DL +IND 将两者都作为模型输入。在考虑全部和部分干扰的二元分类(未受干扰与受干扰)中,我们所有六个研究地点的 F1 分数介于约 0.65(DL +IND)和 0.72(DL base)之间。在森林干扰检测方面,DL base 的表现优于其他设置,它可以在 100 平方米大小的像素内检测到小至 40 平方米的干扰范围。鉴于 DL base 的最佳性能,手工制作的植被指数(VI)并不能改善模型。尽管直接比较具有挑战性,但我们的模型与现有方法相比具有竞争力,并略微优于大多数早期报告的结果。考虑到随着时间的推移,如果有更多的参考数据可用,我们还可以进一步完善我们训练有素的模型,因此我们得出结论,将 Transformers 和 Sentinel-2 时间序列结合起来,可以开发出一种有效的工具,用于对中欧森林进行精细空间粒度的森林干扰监测。
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引用次数: 0
Temperature dependence of L-band vegetation optical depth over the boreal forest from 2011 to 2022 2011 年至 2022 年北方森林 L 波段植被光学深度的温度依赖性
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-23 DOI: 10.1016/j.rse.2024.114470
Mike Schwank , Yiwen Zhou , Arnaud Mialon , Philippe Richaume , Yann Kerr , Christian Mätzler
<div><div>The dependence of L-band Vegetation Optical Depth (L-VOD, <span><math><mi>τ</mi></math></span>) on Vegetation temperature <span><math><msub><mi>T</mi><mi>V</mi></msub></math></span> is investigated for 1165 boreal forest grid cells selected for latitudes > 55° and high radiometric forest fraction <span><math><mi>FFO</mi><mo>≥</mo><mn>90</mn><mo>%</mo></math></span>. SMOS Level-3 Brightness Temperatures (BT) at ascending orbits acquired from 2011 to 2022 are used. This is a spatio-temporal extension of our previous study on <span><math><mi>τ</mi><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span> made over the “Sodankylä grid cell” (Finland) in 2019. It demonstrated the Electromagnetic (EM) reasons for <span><math><mi>τ</mi><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span> reaching maximum at 0°C and decreasing when <span><math><msub><mi>T</mi><mi>V</mi></msub></math></span> is moving away from 0°C. The parameterisation of the "L-VOD model" developed in the previous study is simplified and updated to take into account the conservation of salt in sap-water during freezing. The “forward operator” based on the Two-Stream Microwave Emission Model (2S-MEM) is inverted to retrieve <span><math><msub><mi>τ</mi><mi>SMOS</mi></msub><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span> together with effective Ground permittivities <span><math><msub><mi>ε</mi><mi>G</mi></msub></math></span> during seasonal Warming Periods (WPs) determined from ERA-interim air temperatures. The “L-VOD model” parameters <span><math><mfenced><msub><mi>T</mi><mi>melt</mi></msub><msub><mi>WC</mi><mi>wood</mi></msub></mfenced></math></span> are estimated for the boreal forest grid cells by minimizing squared differences between <span><math><msub><mi>τ</mi><mi>SMOS</mi></msub><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span> and simulated <span><math><msub><mi>τ</mi><mi>sim</mi></msub><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span>. The vegetation melt-parameter <span><math><msub><mi>T</mi><mi>melt</mi></msub></math></span> represents the “number of degrees below 0°C” at which sap-water melts, and <span><math><msub><mi>WC</mi><mi>wood</mi></msub></math></span> is the gravimetric wood-Water Content of branches. Reasonable values of <span><math><mfenced><msub><mi>T</mi><mi>melt</mi></msub><msub><mi>WC</mi><mi>wood</mi></msub></mfenced></math></span> are achieved for a majority of the boreal forest grid cells. It is found that <span><math><msub><mi>T</mi><mi>melt</mi></msub></math></span> tends to be too high over Northern Europe, a region with longer WP durations compared to other regions of the boreal forest belt. By optimising the scattering albedo used to retrieve <span><math><msub><mi>τ</mi><mi>SMOS</mi></msub><mfenced><msub><mi>T</mi><mi>V</mi></msub></mfenced></math></span>, the correlations between <span><math><msub><mi>τ</mi><mi>sim</mi></msub><mfenced><msub><mi>T</mi><mi>V</mi></msub
在纬度 > 55° 和高辐射森林分数 FFO≥90%FFO≥90% 的 1165 个北方森林网格单元中,研究了 L 波段植被光学深度(L-VOD,ττ)与植被温度 TVTV 的关系。使用的是 2011 年至 2022 年期间获取的上升轨道上的 SMOS Level-3 亮度温度 (BT)。这是我们之前于 2019 年在 "索丹屈莱网格单元"(芬兰)上进行的τTVτTV 研究的时空延伸。它证明了τTVτTV在0°C时达到最大值,而当TVTV远离0°C时则逐渐减小的电磁(EM)原因。对之前研究中开发的 "L-VOD 模型 "的参数化进行了简化和更新,以考虑到冰冻过程中树液水中盐分的保存。对基于双流微波发射模式(2S-MEM)的 "前向算子 "进行反演,以检索τSMOSTVτSMOSTV 和根据ERA-临时气温确定的季节性变暖期(WPs)的有效地面容积εGεG。北方森林网格单元的 "L-VOD 模型 "参数 TmeltWCwoodTmeltWCwood 是通过最小化 τSMOSTVτSMOSTV 与模拟 τsimTVτsimTV 之间的平方差来估算的。植被融化参数 TmeltTmelt 表示树液水融化的 "0℃以下度数",WCwoodWCwood 是树枝的重量木材含水量。大部分北方森林网格单元的 TmeltWCwoodTmeltWCwood 都达到了合理值。研究发现,北欧地区的 TmeltTmelt 值往往过高,与北方森林带的其他地区相比,该地区的可湿性粉末持续时间较长。通过优化用于检索 τSMOSTVτSMOSTV 的散射反照率,可以提高 τsimTVτsimTV 与 τSMOSTVτSMOSTV 之间的相关性,从而提高 TmeltWCwoodTmeltWCwood 的可靠性。研究结果为北方森林散射反照率的参数化提供了另一种方法的可能性,这种方法是通过与 TmeltTmelt 与预期值的一致性相关联的 τSMOSTVτSMOSTV 的现实性来实现的。研究还表明,使用 L-VOD 估算北方森林的地面生物量 (AGB),必须考虑到木质树枝中的树液水结冰导致的电磁原因造成的 L-VOD 降低,这在 L 波段的辐射传输中占主导地位。
{"title":"Temperature dependence of L-band vegetation optical depth over the boreal forest from 2011 to 2022","authors":"Mike Schwank ,&nbsp;Yiwen Zhou ,&nbsp;Arnaud Mialon ,&nbsp;Philippe Richaume ,&nbsp;Yann Kerr ,&nbsp;Christian Mätzler","doi":"10.1016/j.rse.2024.114470","DOIUrl":"10.1016/j.rse.2024.114470","url":null,"abstract":"&lt;div&gt;&lt;div&gt;The dependence of L-band Vegetation Optical Depth (L-VOD, &lt;span&gt;&lt;math&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;/math&gt;&lt;/span&gt;) on Vegetation temperature &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; is investigated for 1165 boreal forest grid cells selected for latitudes &gt; 55° and high radiometric forest fraction &lt;span&gt;&lt;math&gt;&lt;mi&gt;FFO&lt;/mi&gt;&lt;mo&gt;≥&lt;/mo&gt;&lt;mn&gt;90&lt;/mn&gt;&lt;mo&gt;%&lt;/mo&gt;&lt;/math&gt;&lt;/span&gt;. SMOS Level-3 Brightness Temperatures (BT) at ascending orbits acquired from 2011 to 2022 are used. This is a spatio-temporal extension of our previous study on &lt;span&gt;&lt;math&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; made over the “Sodankylä grid cell” (Finland) in 2019. It demonstrated the Electromagnetic (EM) reasons for &lt;span&gt;&lt;math&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; reaching maximum at 0°C and decreasing when &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; is moving away from 0°C. The parameterisation of the \"L-VOD model\" developed in the previous study is simplified and updated to take into account the conservation of salt in sap-water during freezing. The “forward operator” based on the Two-Stream Microwave Emission Model (2S-MEM) is inverted to retrieve &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mi&gt;SMOS&lt;/mi&gt;&lt;/msub&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; together with effective Ground permittivities &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;ε&lt;/mi&gt;&lt;mi&gt;G&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; during seasonal Warming Periods (WPs) determined from ERA-interim air temperatures. The “L-VOD model” parameters &lt;span&gt;&lt;math&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;melt&lt;/mi&gt;&lt;/msub&gt;&lt;msub&gt;&lt;mi&gt;WC&lt;/mi&gt;&lt;mi&gt;wood&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; are estimated for the boreal forest grid cells by minimizing squared differences between &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mi&gt;SMOS&lt;/mi&gt;&lt;/msub&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; and simulated &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mi&gt;sim&lt;/mi&gt;&lt;/msub&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt;. The vegetation melt-parameter &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;melt&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; represents the “number of degrees below 0°C” at which sap-water melts, and &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;WC&lt;/mi&gt;&lt;mi&gt;wood&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; is the gravimetric wood-Water Content of branches. Reasonable values of &lt;span&gt;&lt;math&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;melt&lt;/mi&gt;&lt;/msub&gt;&lt;msub&gt;&lt;mi&gt;WC&lt;/mi&gt;&lt;mi&gt;wood&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt; are achieved for a majority of the boreal forest grid cells. It is found that &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;melt&lt;/mi&gt;&lt;/msub&gt;&lt;/math&gt;&lt;/span&gt; tends to be too high over Northern Europe, a region with longer WP durations compared to other regions of the boreal forest belt. By optimising the scattering albedo used to retrieve &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mi&gt;SMOS&lt;/mi&gt;&lt;/msub&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub&gt;&lt;/mfenced&gt;&lt;/math&gt;&lt;/span&gt;, the correlations between &lt;span&gt;&lt;math&gt;&lt;msub&gt;&lt;mi&gt;τ&lt;/mi&gt;&lt;mi&gt;sim&lt;/mi&gt;&lt;/msub&gt;&lt;mfenced&gt;&lt;msub&gt;&lt;mi&gt;T&lt;/mi&gt;&lt;mi&gt;V&lt;/mi&gt;&lt;/msub","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"315 ","pages":"Article 114470"},"PeriodicalIF":11.1,"publicationDate":"2024-10-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142487538","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
Can satellite products monitor solar brightening in Europe? 卫星产品能否监测欧洲的太阳亮度?
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-23 DOI: 10.1016/j.rse.2024.114472
Ruben Urraca , Jörg Trentmann , Uwe Pfeifroth , Nadine Gobron
Satellite products provide the best way to monitor the solar radiation reaching the Earth’s surface on a global scale. However, their capability to monitor solar radiation trends needs to be constantly evaluated. This depends on their temporal stability and the accurate representation of all processes driving solar radiation. This study evaluates these aspects by comparing and cross-comparing different solar radiation products (ERA5, CAMS-RAD 4.6, SARAH-3, CLARA-A3, CERES-EBAF 4.2) against in-situ measurements over Europe.
All products show a moderate positive bias over Europe but strong differences in their root mean squared deviation (RMSD) related to their different cloud transmittance models. Geostationary-based products (SARAH-3, CAMS-RAD 4.6) provide the smallest RMSD closely followed by CLARA-A3, whereas ERA5 shows a large RMSD due to random errors in cloud transmittance.
All products show an increase in surface solar radiation, or brightening, over the last 40 years over Europe, but the magnitude of the trends and their spatiotemporal variability differ between products. Despite finding temporal inhomogeneities in some products, the different trends are mostly due to different aerosol modeling approaches implemented by each product. Both SARAH-3 (+2.3 W/m2/decade, 2001–22) and CERES-EBAF 4.2 (+2.2 W/m2/decade, 2001–22) provide the most consistent trends compared to in-situ data, showing that after stabilizing in the late 2000s, brightening is particularly recovering in Western Europe. In-situ measurements show a reduction of aerosol optical depth from 2001 to 2022 that has been accentuated in the last 10 years, particularly in Western Europe. This would be consistent with the hypothesis that brightening recovery is driven by an aerosol reduction, though other analyses suggest that clouds also play a role in this recovery. More work is needed to understand the contribution of aerosols to solar radiation trends and the exact aerosol effects represented by each solar radiation product.
卫星产品为监测全球范围内到达地球表面的太阳辐射提供了最佳途径。然而,它们监测太阳辐射趋势的能力需要不断评估。这取决于卫星产品的时间稳定性和对太阳辐射所有驱动过程的准确呈现。本研究通过将不同的太阳辐射产品(ERA5、CAMS-RAD 4.6、SARAH-3、CLARA-A3、CERES-EBAF 4.2)与欧洲上空的实地测量数据进行比较和交叉比较,对这些方面进行了评估。基于地球静止轨道的产品(SARAH-3、CAMS-RAD 4.6)提供的均方根偏差最小,紧随其后的是 CLARA-A3,而 ERA5 则由于云层透射率的随机误差而显示出较大的均方根偏差。尽管在一些产品中发现了时间上的不均匀性,但不同的趋势主要是由于每个产品采用的气溶胶建模方法不同造成的。SARAH-3(+2.3 W/m2/decadeW/m2/decade,2001-22 年)和 CERES-EBAF 4.2(+2.2 W/m2/decadeW/m2/decade,2001-22 年)都提供了与原地数据最一致的趋势,表明在 2000 年代后期趋于稳定之后,西欧的增亮正在恢复。原位测量结果表明,从 2001 年到 2022 年,气溶胶光学深度有所下降,而在过去 10 年中,这种下降趋势更加明显,尤其是在西欧。这与亮度恢复是由气溶胶减少驱动的假设是一致的,尽管其他分析表明云也在亮度恢复中发挥了作用。要了解气溶胶对太阳辐射趋势的贡献以及每种太阳辐射产品所代表的气溶胶效应,还需要做更多的工作。
{"title":"Can satellite products monitor solar brightening in Europe?","authors":"Ruben Urraca ,&nbsp;Jörg Trentmann ,&nbsp;Uwe Pfeifroth ,&nbsp;Nadine Gobron","doi":"10.1016/j.rse.2024.114472","DOIUrl":"10.1016/j.rse.2024.114472","url":null,"abstract":"<div><div>Satellite products provide the best way to monitor the solar radiation reaching the Earth’s surface on a global scale. However, their capability to monitor solar radiation trends needs to be constantly evaluated. This depends on their temporal stability and the accurate representation of all processes driving solar radiation. This study evaluates these aspects by comparing and cross-comparing different solar radiation products (ERA5, CAMS-RAD 4.6, SARAH-3, CLARA-A3, CERES-EBAF 4.2) against in-situ measurements over Europe.</div><div>All products show a moderate positive bias over Europe but strong differences in their root mean squared deviation (RMSD) related to their different cloud transmittance models. Geostationary-based products (SARAH-3, CAMS-RAD 4.6) provide the smallest RMSD closely followed by CLARA-A3, whereas ERA5 shows a large RMSD due to random errors in cloud transmittance.</div><div>All products show an increase in surface solar radiation, or brightening, over the last 40 years over Europe, but the magnitude of the trends and their spatiotemporal variability differ between products. Despite finding temporal inhomogeneities in some products, the different trends are mostly due to different aerosol modeling approaches implemented by each product. Both SARAH-3 (+2.3 <span><math><mrow><msup><mrow><mi>W/m</mi></mrow><mrow><mn>2</mn></mrow></msup><mo>/</mo><mi>decade</mi></mrow></math></span>, 2001–22) and CERES-EBAF 4.2 (+2.2 <span><math><mrow><msup><mrow><mi>W/m</mi></mrow><mrow><mn>2</mn></mrow></msup><mo>/</mo><mi>decade</mi></mrow></math></span>, 2001–22) provide the most consistent trends compared to in-situ data, showing that after stabilizing in the late 2000s, brightening is particularly recovering in Western Europe. In-situ measurements show a reduction of aerosol optical depth from 2001 to 2022 that has been accentuated in the last 10 years, particularly in Western Europe. This would be consistent with the hypothesis that brightening recovery is driven by an aerosol reduction, though other analyses suggest that clouds also play a role in this recovery. More work is needed to understand the contribution of aerosols to solar radiation trends and the exact aerosol effects represented by each solar radiation product.</div></div>","PeriodicalId":417,"journal":{"name":"Remote Sensing of Environment","volume":"315 ","pages":"Article 114472"},"PeriodicalIF":11.1,"publicationDate":"2024-10-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142488943","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
4D imaging of the volcano feeding system beneath the urban area of the Campi Flegrei caldera 坎皮弗莱格雷火山口城市地区下方火山馈源系统的四维成像
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-22 DOI: 10.1016/j.rse.2024.114480
Pietro Tizzani , José Fernández , Andrea Vitale , Joaquín Escayo , Andrea Barone , Raffaele Castaldo , Susi Pepe , Vincenzo De Novellis , Giuseppe Solaro , Antonio Pepe , Anna Tramelli , Zhongbo Hu , Sergey V. Samsonov , Isabel Vigo , Kristy F. Tiampo , Antonio G. Camacho
This paper describes an approach to analyze ground deformation data collected by InSAR (Interferometric Synthetic Aperture Radar) imaging the volcano feeding system (VFS) beneath a caldera. The approach is applied to the Campi Flegrei caldera in southern Italy, a densely populated area at high risk for volcanic eruption. The method is a 4D tomographic inversion that considers a combination of 3D pressure sources and dislocations (strike-slip, dip-slip and tensile) acting simultaneously. This is in contrast to traditional methods that assume a priori geometries and type for the volcanic source. Another novelty is that we carry out a time-series analysis of multifrequency InSAR displacement data. The analysis of these multiplatform and multifrequency InSAR data from 2011 to 2022 reveals an inflating source at a depth of 3–4 km that is interpreted as a pressurized magmatic intrusion. The source broadens and migrates laterally over time, with a possible new magmatic pulse arriving in 2018–2020. The model also identifies a shallow region (at 400 m depth) that may be feeding fumaroles in the area. The analysis also reveals a zone of weakness (dip-slip) that could influence the path of rising magma. This method provides a more detailed dynamic 4 - dimensional image of the VFS than previously possible and could be used to improve hazard assessments in active volcanic areas.
本文介绍了一种分析 InSAR(干涉合成孔径雷达)采集的地面变形数据的方法,该方法对火山口下方的火山供能系统(VFS)进行成像。该方法应用于意大利南部的坎皮弗莱格雷火山口,该地区人口稠密,火山爆发风险很高。该方法是一种四维层析反演法,考虑了同时作用的三维压力源和位错(走向滑动、倾覆滑动和拉伸)的组合。这与假定火山源的先验几何形状和类型的传统方法截然不同。另一个新颖之处是,我们对多频 InSAR 位移数据进行了时间序列分析。对这些 2011 年至 2022 年的多平台和多频率 InSAR 数据的分析表明,在 3-4 千米深处有一个膨胀源,被解释为加压岩浆侵入体。随着时间的推移,该源会扩大并向横向移动,2018-2020 年可能会出现一个新的岩浆脉冲。该模型还确定了一个浅层区域(深度为 400 米),该区域可能是该地区的燧岩。分析还揭示了可能影响岩浆上升路径的薄弱区(倾覆滑动)。这种方法提供了比以前更详细的活火山四维动态图像,可用于改进活火山地区的危险评估。
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引用次数: 0
Improvements in land surface temperature and emissivity retrieval from Landsat-9 thermal infrared data 改进 Landsat-9 热红外数据的地表温度和发射率检索
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-22 DOI: 10.1016/j.rse.2024.114471
Xiaopo Zheng, Youying Guo, Zhongliang Zhou, Tianxing Wang
Land surface temperature (LST) is the key parameter for characterizing the water and energy balance of the Earth’ surface. At present, thermal infrared (TIR) remote sensing provides the most efficient way to obtain accurate LST regionally and globally. Among existing satellites, the Landsat-9 could observe the Earth's surface via two TIR channels, making it possible to generate the global LST product with a remarkable spatial resolution of 100 m. Currently, the single channel method and split window method generally were used to recover LST from the Landsat-9 TIR measurements. However, accurate land surface emissivity (LSE) is needed in both algorithms, which is very difficult to obtain at the pixel scale. To overcome this issue, an improved LST and LSE separation method was proposed in this study. Firstly, the traditional water vapor scaling (WVS) method was refined to address the atmospheric effects in the satellite measurements. Then, the traditional temperature and emissivity separation method (TES) was adapted to the Landsat-9 observations with only two TIR channels. Finally, an iterative process was designed to retrieve the LST and LSE simultaneously. Validations using in-situ measured LST indicated that the root mean square error (RMSE) of the retrieved LST was around 2.92 K, outperforming the official Landsat-9 LST product with an RMSE of about 4.20 K. Taking ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) products as the references, the RMSE of our retrieved LST and LSE was found to be < 1.55 K and < 0.015, respectively. Overall, conclusions can be made that the proposed method was able to retrieve accurate LST and LSE simultaneously from the Landsat-9 TIR measurements with high spatial resolution, which may greatly facilitate the relevant applications.
陆地表面温度(LST)是表征地球表面水和能量平衡的关键参数。目前,热红外(TIR)遥感是获取区域和全球精确地表温度的最有效方法。在现有的卫星中,Landsat-9 可以通过两个热红外通道观测地球表面,因此可以生成空间分辨率高达 100 米的全球 LST 产品。然而,这两种算法都需要精确的地表发射率(LSE),而这在像素尺度上很难获得。为了克服这一问题,本研究提出了一种改进的 LST 和 LSE 分离方法。首先,针对卫星测量中的大气效应,对传统的水汽比例(WVS)方法进行了改进。然后,对传统的温度和发射率分离方法(TES)进行了调整,使其适用于只有两个红外通道的 Landsat-9 观测数据。最后,设计了一个迭代过程来同时检索 LST 和 LSE。使用原地测量的 LST 进行的验证表明,检索到的 LST 均方根误差(RMSE)约为 2.92 K,优于官方 Landsat-9 LST 产品约 4.20 K 的均方根误差;以空间站上的 ECOSTRESS 空间热辐射计实验(ECOSTRESS)产品为参考,我们检索到的 LST 和 LSE 均方根误差分别为 1.55 K 和 0.015。总之,可以得出结论,所提出的方法能够同时从 Landsat-9 TIR 高空间分辨率测量中获取精确的 LST 和 LSE,这将极大地促进相关应用。
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引用次数: 0
Corrigendum to “Retrieval of high-resolution melting-season albedo and its implications for the Karakoram Anomaly” [Remote Sensing of Environment Volume 315 (2024) 114438] 对 "高分辨率融化季节反照率的检索及其对喀喇昆仑异常现象的影响 "的更正[《环境遥感》第 315 卷 (2024) 114438]
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-21 DOI: 10.1016/j.rse.2024.114474
Fuming Xie , Shiyin Liu , Yu Zhu , Xinyi Qing , Shucheng Tan , Yongpeng Gao , Miaomiao Qi , Ying Yi , Hui Ye , Muhammad Mannan Afzal , Xianhe Zhang , Jun Zhou
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引用次数: 0
Development of China's atmospheric environment monitoring satellite CO2 IPDA lidar retrieval algorithm based on airborne campaigns 基于机载活动的中国大气环境监测卫星 CO2 IPDA 激光雷达检索算法的开发
IF 11.1 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-21 DOI: 10.1016/j.rse.2024.114473
Shuaibo Wang , Chonghui Cheng , Sijie Chen , Jiqiao Liu , Xingying Zhang , Lingbing Bu , Jingxin Zhang , Kai Zhang , Jiesong Deng , Wentao Xu , Weibiao Chen , Dong Liu
China successfully launched the Atmospheric Environment Monitoring Satellite (AEMS) equipped with an Atmospheric Carbon Dioxide Lidar (ACDL) on April 16, 2022, which is the world's first satellite based on Integrated Path Differential Absorption (IPDA) technique to detect the atmospheric CO2 column-weighted dry-air mixing ratio (XCO2). In order to accurately and quickly process the AEMS measurements, we proposed a systematic retrieval algorithm for the AEMS ACDL and conducted two airborne campaigns to validate its performance. The first airborne campaign was conducted in the land-sea interface region of northeast China in 2019. The CO2 retrieval algorithm distinguished significant horizontal XCO2 gradients over different underlying surfaces and obtained an apparent XCO2 enhancement of 8–18 ppm between the urban and forests. The CO2 retrievals not only demonstrated the excellent detection capability of the ACDL for carbon sources and sinks, but also proved the feasibility of the retrieval algorithm in complex terrain and variable atmospheric conditions. The second airborne experiment was conducted in 2021 in the interior desert region of China, which is an excellent flight field to explore the accuracy and precision limits of the retrieval algorithm. We validated the XCO2 retrievals with the airborne in-situ CO2 profiles and demonstrated that the XCO2 accuracy and precision were 0.29 ppm and 0.63 ppm with 1.5-km averages over the desert surface, indicating the accuracy of the retrieval algorithm. The hard target elevation (HTE) retrieval validation results indicate that the IPDA lidar ranging precision is 0.69 m and 6.29 m for the ocean and land surface, respectively. In addition, further analysis combined with the space-borne IPDA lidar simulator showed high consistency in CO2 precision between airborne measurements and simulation results in East Asia, demonstrating the robustness of the retrieval algorithm at continental scales.
中国于2022年4月16日成功发射了配备大气二氧化碳激光雷达(ACDL)的大气环境监测卫星(AEMS),这是世界上第一颗基于集成路径差分吸收(IPDA)技术探测大气二氧化碳柱加权干气混合比(XCO2)的卫星。为了准确、快速地处理 AEMS 测量数据,我们提出了一种 AEMS ACDL 系统检索算法,并进行了两次机载试验来验证其性能。第一次机载试验于 2019 年在中国东北海陆交界地区进行。二氧化碳检索算法区分了不同底层表面上显著的水平 XCO2 梯度,并在城市和森林之间获得了 8-18 ppm 的 XCO2 表观增强。二氧化碳检索结果不仅证明了ACDL对碳源和碳汇的卓越探测能力,也证明了该检索算法在复杂地形和多变大气条件下的可行性。第二次机载实验于 2021 年在中国内陆沙漠地区进行,该地区是探索检索算法准确度和精度极限的绝佳飞行区域。我们利用机载原位二氧化碳剖面图验证了 XCO2 的检索结果,结果表明,在沙漠表面 1.5 公里的平均范围内,XCO2 的精度和准确度分别为 0.29 ppm 和 0.63 ppm,表明了检索算法的准确性。硬目标高程(HTE)检索验证结果表明,IPDA 激光雷达在海洋和陆地表面的测距精度分别为 0.69 米和 6.29 米。此外,结合空间 IPDA 激光雷达模拟器进行的进一步分析表明,东亚地区的机载测量和模拟结果在二氧化碳精度方面具有很高的一致性,证明了该检索算法在大陆尺度上的稳健性。
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Remote Sensing of Environment
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