Summary
Contents
Subject index
Remote sensing acquires and interprets small or large-scale data about the Earth from a distance. Using a wide range of spatial, spectral, temporal, and radiometric scales remote sensing is a large and diverse field for which this Handbook will be the key research reference. Illustrated throughout, an essential resource for the analysis of remotely sensed data, The SAGE Handbook of Remote Sensing provides researchers with a definitive statement of the core concepts and methodologies in the discipline.
Remote Sensing for Terrestrial Biogeochemical Modeling
Remote Sensing for Terrestrial Biogeochemical Modeling
Keywords
carbon cycling, ecosystem modeling, evapotranspiration, hyperspectral imaging, model data assimilation, net primary production, vegetation properties.
Introduction
Remote sensing and biogeochemical modeling share a highly complementary nature, whichhasled to a growing number of applications that involve some degreeof coupling between the two. Whereas remote sensing represents the only means by which landscape and vegetation properties can be sampled over large and contiguous portions of the Earth's surface, models focus on the underlying biogeochemical processes that regulate the flow and storage of water, carbon and nutrients, often over much longer time scales than can be considered through remote sensing alone. The aims and goals of biogeochemical modeling are wide ranging and include studies of carbon (C) and water cycling, analyses of nitrogen (N) enrichment and leaching to aquatic ecosystems, and trace gas transfers from soils to the atmosphere. Biogeochemical models are also used as part of larger, integrated modeling environments of regional and global biosphere–atmosphere interactions, biogeography, and climate change (e.g., Sellerset al. 1997, Cramer et al. 2001). More recently, biogeochemical modeling has taken a role in decision support for conservation, management, and policy development (Potter et al. 2006).
Remote sensing can provide biogeochemical models with information on vegetation type, leaf area index (LAI), canopy height, the fraction of absorbed photosynthetically active radiation (fPAR), light-use efficiency (LUE), leaf N concentration, pigments and other biochemical compounds to simulate plant growth and mortality. Other remote sensing-related inputs have included temperature, precipitation, solar radiation levels, and soil moisture. In this chapter, we review a number of approaches through which remote sensing data can be applied to the detection of vegetation properties, and discuss the trade-offs of various methods with respect to biogeochemical modeling. Given the breadth of the topic, our goal in preparing this chapter was not to provide a working manual of all remote sensing-model integration methods available. Instead, we sought to summarize important overall strategies for vegetation detection into a framework that involves the types of instruments used, the ecological properties they can be designed to detect, and the manner in which those properties can be utilized by models.
Models Utilizing Remote Sensing
This section provides a brief overview of major categories of ecosystem biogeochemistry models that can be driven or guided by remote sensing. In the interest of simplicity, we describe each type of model as being distinct from one another, but readers should be aware that the boundaries between them are often blurry, and hybrid approaches are also available.
Simple Empirical Models
The simplest type of remote sensing/model linkage consists of a small number of empirically derived algorithms that combine field-based relationships with remotely sensed vegetation properties that correlate strongly with some aspect of ecosystem behavior. For example, Ollinger et al. (2002a) used imaging spectroscopy to detect leaf lignin to nitrogen ratios in temperate forests, which provided a direct connection to decomposition, C:N ratios, and N cycling rates in soils. When such relationships are available, this approach offers a straightforward means of producing estimates that are constrained to known patterns. The resulting accuracy is dependent only on the strength of the observed trends and on the accuracy of the vegetation property estimates. The principal disadvantage is that these approaches include no mechanisms that would allow extrapolation in time or under varying environmental conditions.
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