Radiative transfer modelling reveals why canopy reflectance follows function

Optical remote sensing is potentially highly informative to track Earth’s plant functional diversity. Yet, causal explanations of how and why plant functioning is expressed in canopy reflectance remain limited. Variation in canopy reflectance can be described by radiative transfer models (here PROSAIL) that incorporate plant traits affecting light transmission in canopies. To establish causal links between canopy reflectance and plant functioning, we investigate how two plant functional schemes, i.e. the Leaf Economic Spectrum (LES) and CSR plant strategies, are related to traits with relevance to reflectance. These traits indeed related to both functional schemes, whereas only traits describing leaf properties correlated with the LES. In contrast, traits related to canopy structure showed no correlation to the LES, but to CSR strategies, as the latter integrates both plant economics and size traits, rather than solely leaf economics. Multiple optically relevant traits featured comparable or higher correspondence to the CSR space than those traits originally used to allocate CSR scores. This evidences that plant functions and strategies are directly expressed in reflectance and entails that canopy ‘reflectance follows function’. This opens up new possibilities to understand differences in plant functioning and to harness optical remote sensing data for monitoring Earth´s functional diversity

Linking Canopy Reflectance and Plant Functioning through Radiative Transfer Models

Von den Tropen bis zur Tundra hat sich die Pflanzenwelt durch Anpassungen an lokale Umwelteinflüsse diversifiziert. Diese Anpassungen sind in der Funktionsweise der Pflanzen manifestiert, welche unter anderem Wachstum, Fortpflanzung, Konkurrenzfähigkeit oder Ausdauer beinhalten. Pflanzenfunktionen haben nicht nur direkten Einfluss auf die Artenzusammensetzung, sondern auch auf großräumige Prozesse wie Bio- und Atmossphäreninteraktionen oder Stoffkreisläufe. Folglich wurden viele Forschungsanstrengungen unternommen um Pflanzenfunktionen weiter zu verstehen und zu erfassen, z.B. darauf abzielend generalisierende Modelle von Pflanzenfunktionen zu entwickeln oder individuelle Pflanzenmerkmale als Indikatoren für Pflanzenfunktion zu identifizieren. Trotz der wissenschaftlichen Fortschritte fehlt ein vollständiges Bild der Funktionsvielfalt der Pflanzenwelt, sowohl in geographischer als auch funktioneller Hinsicht. Dies ist im Wesentlichen auf die Komplexität und die logistischen Einschränkungen bei der Messung von Pflanzenfunktionen im Feld zurückzuführen. Um dieses Bild zu vervollständigen wird insbesondere optischen Erdbeobachtungsdaten ein hohes Potenzial zugeschrieben. Optische Erdbeobachtungssensoren erfassen das vom Kronendach reflektierte Sonnenlicht. Letzteres wird durch verschiedene biochemische und strukturelle Pflanzenmerkmale (im Folgenden optische Merkmale) beeinträchtigt (z.B. Blattchlorophyllgehalt oder Blattwinkel). Das Abfangen und Absorbieren von Sonnenlicht ist die Grundlage des pflanzeneigenen Metabolismus und folglich liegt es Nahe, dass diese optischen Merkmale direkt mit Pflanzenfunktionen zusammenhängen. Der Zusammenhang dieser optische Merkmale mit Pflanzenfunktionen wurde jedoch noch nicht systematisch untersucht, und ebenso ist der Zusammenhang zwischen Pflanzenfunktion und Kronendachreflektion noch nicht vollständig untersucht. Die physikalischen Interaktionen von Licht und optischen Pflanzenmerkmalen sind bereits hinreichend verstanden und in Strahlungstransfermodellen (RTM) für Vegetationskronendächer formuliert. RTM können als prozessbasierte Modelle betrachtet werden, die die Reflektion des Kronendachs in Abhängigkeit von optische Merkmalen, dem Bodenhintergrund und der Sonnen-Sensorgeometrie modellieren. Das Ziel und die Innovation dieser Dissertation war die kausalen Zusammenhänge zwischen Kronendachreflektion und Pflanzenfunktion mittels RTM zu verstehen und zu nutzen. Es wurde gezeigt, dass für die Fernerkundung von Pflanzenfunktionen die Kopplung von Kronendachreflektion und Pflanzenfunktionen durch RTM mehrere Potentiale bietet: Erstens, ermöglichen RTM die Kartierung von Pflanzenmerkmalen. Innerhalb einer Fallstudie wurde gezeigt, dass eine Inversion von RTM mit hyperspektralen Daten eine Kartierung von optischen Merkmalen erlaubt, für die keine Felddaten zur Modellkalibrierung benötigt werden. Die kartierten Merkmale zeigten eine hohe Übereinstimmung mit Merkmalsausprägungen aus unabhängigen Datenbanken und spiegelten die im Feld gemessenen ökologischen Gradienten wider. Dies deutet darauf hin, dass RTM-Inversion als äußerst übertragbare Methode betrachtet werden kann, um räumliche Karten von Pflanzenmerkmalen zu erstellen, die als Proxies für Pflanzenfunktionen dienen können. Allerdings erfordert die Implementierung von RTM Inversionen fundierte Kenntnisse über die Prinzipien der Strahlentransfermodellierung und der zu untersuchenden Vegetationscharakteristiken. Zweitens, ermöglichen RTM die Untersuchung von Zusammenhängen zwischen Pflanzenfunktion und der Kronendachreflektion. In der vorliegenden Thesis wurden simulierte Kronendachspektren aus einem RTM verwendet, um den Beitrag der optischen Merkmale zu den spektralen Unterschieden zwischen Pflanzenfunktionstypen zu erfassen. Die Ergebnisse zeigten die dominanten Pflanzenmerkmale und die entsprechenden spektralen Charakteristiken die für eine fernerkundliche Unterscheidung der Pflanzenfunktion von großer Relevanz sind. Darüber hinaus wurde gezeigt, dass RTM-basierte Simulationen Einschränkungen von Fallstudien kompensieren und Kenntnisse über die Zusammenhänge von Pflanzenfunktionen, Pflanzeneigenschaften und Kronendachtreflektion erweitern können. Diese Kenntnisse bilden die Grundlage für die Entwicklung und Verbesserung von Sensoren und Algorithmen zur Fernerkundung von Pflanzenfunktionen. Drittens, erweitern RTM und die darin enthaltenen optischen Merkmale unsere Möglichkeiten Unterschiede in der Pflanzenfunktion zu verstehen und zu quantifizieren. Mit Hilfe von in-situ gemessenen Merkmalsausprägungen konnte gezeigt werden, dass die in RTM enthaltenen optischen Merkmale kausal mit primären Pflanzenfunktionen zusammenhängen. Dies wiederum bedeutet, dass die Reflexion des Kronendachs unmittelbar mit den primären Funktionen der Pflanze zusammenhängt (‘Reflektion folgt Funktion’). Darüber hinaus wurde festgestellt, dass optische Merkmale vergleichbare oder sogar höhere Korrelationen mit den verwendeten pflanzlichen Funktionsgradienten aufweisen als die in der Pflanzenökologie üblich verwendeten Merkmale. Entsprechend bieten RTM sowohl eine alternative Perspektive als auch ein Set von Pflanzenmerkmalen mit denen Unterschiede der Pflanzenfunktion charakterisiert und quantifiziert werden können. Diese Merkmale können somit als wertvolle Ergänzung oder Alternative zu den in der Pflanzenökologie üblichen Merkmalen dienen. Zusammengefasst zeigt diese Thesis, dass RTM unsere Möglichkeiten erweiterten können die funktionelle Vielfalt der globalen Vegetationsbedeckung weiter zu verstehen und zu erfassen und führt zukunftsrelevante Forschungspotentiale auf

Improving ecological forecasts using model and data constraints

Terrestrial ecosystems are essential to human well-being, but their future remains highly uncertain, as evidenced by the huge disparities in model projections of the land carbon sink. The existence of these disparities despite the recent explosion of novel data streams, including the TRY plant traits database, the Landsat archive, and global eddy covariance tower networks, suggests that these data streams are not being utilized to their full potential by the terrestrial ecosystem modeling community. Therefore, the overarching objective of my dissertation is to identify how these various data streams can be used to improve the precision of model predictions by constraining model parameters. In chapter 1, I use a hierarchical multivariate meta-analysis of the TRY database to assess the dependence of trait correlations on ecological scale and evaluate the utility of these correlations for constraining ecosystem model parameters. I find that global trait correlations are generally consistent within plant functional types, and leveraging the multivariate trait space is an effective way to constrain trait estimates for data-limited traits and plant functional types. My next two chapters assess the ability to measure traits using remote sensing by exploring the links between leaf traits and reflectance spectra. In chapter 2, I introduce a method for estimating traits from spectra via radiative transfer model inversion. I then use this approach to show that although the precise location, width, and quantity of spectral bands significantly affects trait retrieval accuracy, a wide range of sensor configurations are capable of providing trait information. In chapter 3, I apply this approach to a large database of leaf spectra to show that traits vary as much within as across species, and much more across species within a functional type than across functional types. Finally, in chapter 4, I synthesize the findings of the previous chapters to calibrate a vegetation model's representation of canopy radiative transfer against observed remotely-sensed surface reflectance. Although the calibration successfully constrained canopy structural parameters, I identify issues with model representations of wood and soil reflectance that inhibit its ability to accurately reproduce remote sensing observations

Doctor of Philosophy

dissertationWildfire is a multifaceted, global phenomenon with ecological, environmental, climatic and socioeconomic impacts. Live fuel moisture content (LFMC) is a critical fuel property for determining fire danger. Previous research has used meteorological data and remote sensing to estimate LFMC with the goal of extending direct ground measurement. A fundemental understanding of plant physiology and spectral response toLFMC variation is needed to advance use of LFMC for fire risk management and remote sensing applications. This study integrates field samples of three species, lab measurements, remote sensing dataand statistical analysis to construct a more complete knowledge of the physical foundations of LFMC seasonalityfrom three perspectives: 1)relationships between soil moisture and LFMC; 2) spectroscopic analysis of seasonal changes in LFMC and leaf dry mass; 3) relationships between LFMC and leaf net heat content, and between leaf net heat content and remotely sensed indices. This study is the first to demonstrate a relationship between in situ soil moisture and LFMC. It also challengesthe current asumption of changing water content and stable dry matter content over time in remote sensing esimation of LFMC, showing the dominant contribution of dry matter in LFMC variation in some conifer species. The resultsdemonstrate the combination of spectroscopic data and partial least squares regression can improve modeling accuray for LFMC temporal variation, but the spectral response to changing LFMC and dry mass is difficult to seperate from broader spectral trends due to temporal change in chlorophyll, leaf structure, water and covaried biochemical components. Lastly it introducesa new vegetation variable, leaf net heat content, and demostrates its relationship with LFMC and potential for remote sensing estimation.This study will improve present capabilities of remote sensing for monitoring vegetation water stress and physiological properties. It will also advance understanding of seasonal changes in LFMC to better estimate fire danger and potential impacts of fire on ecosystems and the carbon cycle

Three dimensional estimation of vegetation moisture content using dual-wavelength terrestrial laser scanning

PhD ThesisLeaf Equivalent Water Thickness (EWT) is a water status metric widely used in vegetation health monitoring. Optical Remote Sensing (RS) data, spaceborne and airborne, can be used to estimate canopy EWT at landscape level, but cannot provide information about EWT vertical heterogeneity, or estimate EWT predawn. Dual-wavelength Terrestrial Laser Scanning (TLS) can overcome these limitations, as TLS intensity data, following radiometric corrections, can be used to estimate EWT in three dimensions (3D). In this study, a Normalized Difference Index (NDI) of 808 nm wavelength, utilized in the Leica P20 TLS instrument, and 1550 nm wavelength, employed in the Leica P40 and P50 TLS systems, was used to produce 3D EWT estimates at canopy level. Intensity correction models were developed, and NDI was found to be able to minimize the incidence angle and leaf internal structure effects. Multiple data collection campaigns were carried out. An indoors dry-down experiment revealed a strong correlation between NDI and EWT at leaf level. At canopy level, 3D EWT estimates were generated with a relative error of 3 %. The method was transferred to a mixed-species broadleaf forest plot and 3D EWT estimates were generated with relative errors < 7 % across four different species. Next, EWT was estimated in six short-rotation willow plots during leaf senescence with relative errors < 8 %. Furthermore, a broadleaf mixed-species urban tree plot was scanned during and two months after a heatwave, and EWT temporal changes were successfully detected. Relative error in EWT estimates was 6 % across four tree species. The last step in this research was to study the effects of EWT vertical heterogeneity on forest plot reflectance. Two virtual forest plots were reconstructed in the Discrete Anisotropic Radiative Transfer (DART) model. 3D EWT estimates from TLS were utilized in the model and Sentinel-2A bands were simulated. The simulations revealed that the top four to five metres of canopy dominated the plot reflectance. The satellite sensor was not able to detect severe water stress that started in the lower canopy layers. This study showed the potential of using dual-wavelength TLS to provide important insights into the EWT distribution within the canopy, by mapping the EWT at canopy level in 3D. EWT was found to vary vertically within the canopy, with EWT and Leaf Mass per Area (LMA) being highly correlated, suggesting that sun leaves were able to hold more moisture than shade leaves. The EWT vertical profiles varied between species, and trees reacted in different ways during drought conditions, losing moisture from different canopy layers. The proposed method can provide time series of the change in EWT at very high spatial and temporal resolutions, as TLS instruments are active sensors, independent of the solar illumination. It also has the potential to provide EWT estimates at the landscape level, if coupled with automatic tree ii segmentation and leaf-wood separation techniques, and thus filling the gaps in the time series produced from satellite data. In addition, the technique can potentially allow the characterisation of whole-tree leaf water status and total water content, by combining the EWT estimates with Leaf Area Index (LAI) measurements, providing new insights into forest health and tree physiology.Egyptian Ministry of Higher Educatio

Refining terrestrial biosphere feedbacks to climate change through precise characterization of terrestrial vegetation

Climate change is primarily driven by the human activities of fossil fuel combustion and land use change, which together result in the emissions of greenhouse gases such as carbon dioxide (CO₂). The terrestrial biosphere currently absorbs about a third of total anthropogenic CO₂ emissions, mostly through primary production by vegetation. The continued function of vegetation as a CO₂ sink is uncertain, as climate change has the potential to enhance or restrict the carbon uptake capacity of vegetation. Uncertainty in terrestrial vegetation function in the context of climate change, due in part to a lack of precise observations of leaf biochemistry and function with which to develop models, therefore limits the confidence of climate change projections. In its entirety, this thesis examines the potential for more precise observations of leaf function and their integration across a variety of models and observational scales. The first chapter provides an introductory overview of the subsequent four chapters and how each compliments the other. The second chapter demonstrates the role of the terrestrial biosphere in influencing the relationship between temperature change and cumulative CO₂ emissions. The third chapter provides adaptations to current radiative transfer modelling approaches to improve estimations of leaf biochemical constituents. The fourth chapter applies high spatiotemporal resolution observations of leaf phenology, the timing of leaf emergence and senescence, across North America to predict species-specific leaf phenology patterns under various emissions scenarios throughout the 21st century. The fifth chapter provides an approach to detect declines in ecosystem processes such as carbon uptake using observational leaf phenology networks. These chapter results indicate that 1) uncertainty in the land-borne fraction of carbon emissions contributes largely to uncertainty in the relationship between temperature change and emissions, 2) spectral subdomains and prior estimation of leaf structure improves leaf biochemistry estimations, 3) leaf senescence timing may diverge between boreal and temperate species under a high emissions scenario, and 4) declines in vegetational carbon uptake can be accurately detected using quantitative phenocam-based indicators. The fundamental and technical insights provided through this thesis will facilitate more reliable and functionally resolved projections of terrestrial biosphere feedbacks to climate change

Remote Sensing of Biophysical Parameters

Vegetation plays an essential role in the study of the environment through plant respiration and photosynthesis. Therefore, the assessment of the current vegetation status is critical to modeling terrestrial ecosystems and energy cycles. Canopy structure (LAI, fCover, plant height, biomass, leaf angle distribution) and biochemical parameters (leaf pigmentation and water content) have been employed to assess vegetation status and its dynamics at scales ranging from kilometric to decametric spatial resolutions thanks to methods based on remote sensing (RS) data.Optical RS retrieval methods are based on the radiative transfer processes of sunlight in vegetation, determining the amount of radiation that is measured by passive sensors in the visible and infrared channels. The increased availability of active RS (radar and LiDAR) data has fostered their use in many applications for the analysis of land surface properties and processes, thanks to their insensitivity to weather conditions and the ability to exploit rich structural and texture information. Optical and radar data fusion and multi-sensor integration approaches are pressing topics, which could fully exploit the information conveyed by both the optical and microwave parts of the electromagnetic spectrum.This Special Issue reprint reviews the state of the art in biophysical parameters retrieval and its usage in a wide variety of applications (e.g., ecology, carbon cycle, agriculture, forestry and food security)

Remote Sensing of Plant Biodiversity

This Open Access volume aims to methodologically improve our understanding of biodiversity by linking disciplines that incorporate remote sensing, and uniting data and perspectives in the fields of biology, landscape ecology, and geography. The book provides a framework for how biodiversity can be detected and evaluated—focusing particularly on plants—using proximal and remotely sensed hyperspectral data and other tools such as LiDAR. The volume, whose chapters bring together a large cross-section of the biodiversity community engaged in these methods, attempts to establish a common language across disciplines for understanding and implementing remote sensing of biodiversity across scales. The first part of the book offers a potential basis for remote detection of biodiversity. An overview of the nature of biodiversity is described, along with ways for determining traits of plant biodiversity through spectral analyses across spatial scales and linking spectral data to the tree of life. The second part details what can be detected spectrally and remotely. Specific instrumentation and technologies are described, as well as the technical challenges of detection and data synthesis, collection and processing. The third part discusses spatial resolution and integration across scales and ends with a vision for developing a global biodiversity monitoring system. Topics include spectral and functional variation across habitats and biomes, biodiversity variables for global scale assessment, and the prospects and pitfalls in remote sensing of biodiversity at the global scale

Remote Sensing of Plant Biodiversity

At last, here it is. For some time now, the world has needed a text providing both a new theoretical foundation and practical guidance on how to approach the challenge of biodiversity decline in the Anthropocene. This is a global challenge demanding global approaches to understand its scope and implications. Until recently, we have simply lacked the tools to do so. We are now entering an era in which we can realistically begin to understand and monitor the multidimensional phenomenon of biodiversity at a planetary scale. This era builds upon three centuries of scientific research on biodiversity at site to landscape levels, augmented over the past two decades by airborne research platforms carrying spectrometers, lidars, and radars for larger-scale observations. Emerging international networks of fine-grain in-situ biodiversity observations complemented by space-based sensors offering coarser-grain imagery—but global coverage—of ecosystem composition, function, and structure together provide the information necessary to monitor and track change in biodiversity globally. This book is a road map on how to observe and interpret terrestrial biodiversity across scales through plants—primary producers and the foundation of the trophic pyramid. It honors the fact that biodiversity exists across different dimensions, including both phylogenetic and functional. Then, it relates these aspects of biodiversity to another dimension, the spectral diversity captured by remote sensing instruments operating at scales from leaf to canopy to biome. The biodiversity community has needed a Rosetta Stone to translate between the language of satellite remote sensing and its resulting spectral diversity and the languages of those exploring the phylogenetic diversity and functional trait diversity of life on Earth. By assembling the vital translation, this volume has globalized our ability to track biodiversity state and change. Thus, a global problem meets a key component of the global solution. The editors have cleverly built the book in three parts. Part 1 addresses the theory behind the remote sensing of terrestrial plant biodiversity: why spectral diversity relates to plant functional traits and phylogenetic diversity. Starting with first principles, it connects plant biochemistry, physiology, and macroecology to remotely sensed spectra and explores the processes behind the patterns we observe. Examples from the field demonstrate the rising synthesis of multiple disciplines to create a new cross-spatial and spectral science of biodiversity. Part 2 discusses how to implement this evolving science. It focuses on the plethora of novel in-situ, airborne, and spaceborne Earth observation tools currently and soon to be available while also incorporating the ways of actually making biodiversity measurements with these tools. It includes instructions for organizing and conducting a field campaign. Throughout, there is a focus on the burgeoning field of imaging spectroscopy, which is revolutionizing our ability to characterize life remotely. Part 3 takes on an overarching issue for any effort to globalize biodiversity observations, the issue of scale. It addresses scale from two perspectives. The first is that of combining observations across varying spatial, temporal, and spectral resolutions for better understanding—that is, what scales and how. This is an area of ongoing research driven by a confluence of innovations in observation systems and rising computational capacity. The second is the organizational side of the scaling challenge. It explores existing frameworks for integrating multi-scale observations within global networks. The focus here is on what practical steps can be taken to organize multi-scale data and what is already happening in this regard. These frameworks include essential biodiversity variables and the Group on Earth Observations Biodiversity Observation Network (GEO BON). This book constitutes an end-to-end guide uniting the latest in research and techniques to cover the theory and practice of the remote sensing of plant biodiversity. In putting it together, the editors and their coauthors, all preeminent in their fields, have done a great service for those seeking to understand and conserve life on Earth—just when we need it most. For if the world is ever to construct a coordinated response to the planetwide crisis of biodiversity loss, it must first assemble adequate—and global—measures of what we are losing