Jakob J. Zyl - Introduction to the Physics and Techniques of Remote Sensing

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Discover cutting edge theory and applications of modern remote sensing in geology, oceanography, atmospheric science, ionospheric studies, and more  The thoroughly revised third edition of the 
delivers a comprehensive update to the authoritative textbook, offering readers new sections on radar interferometry, radar stereo, and planetary radar. It explores new techniques in imaging spectroscopy and large optics used in Earth orbiting, planetary, and astrophysics missions. It also describes remote sensing instruments on, as well as data acquired with, the most recent Earth and space missions. 
Readers will benefit from the brand new and up-to-date concept examples and full-color photography, 50% of which is new to the series. You’ll learn about the basic physics of wave/matter interactions, techniques of remote sensing across the electromagnetic spectrum (from ultraviolet to microwave), and the concepts behind the remote sensing techniques used today and those planned for the future. 
The book also discusses the applications of remote sensing for a wide variety of earth and planetary atmosphere and surface sciences, like geology, oceanography, resource observation, atmospheric sciences, and ionospheric studies. This new edition also incorporates: 
A fulsome introduction to the nature and properties of electromagnetic waves An exploration of sensing solid surfaces in the visible and near infrared spectrums, as well as thermal infrared, microwave, and radio frequencies A treatment of ocean surface sensing, including ocean surface imaging and the mapping of ocean topography A discussion of the basic principles of atmospheric sensing and radiative transfer, including the radiative transfer equation Perfect for senior undergraduate and graduate students in the field of remote sensing instrument development, data analysis, and data utilization, 
 will also earn a place in the libraries of students, faculty, researchers, engineers, and practitioners in fields like aerospace, electrical engineering, and astronomy.

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Depending on the type of the sensor, different properties of the field are measured. In the case of synthetic aperture imaging radars, the amplitude, polarization, frequency, and phase of the fields are measured at successive locations along the flight line. In the case of optical spectrometers, the energy of the field at a specific location is measured as a function of wavelength. In the case of radiometers, the main parameter of interest is the total radiant energy flux. In the case of polarimeters, the energy flux at different polarizations of the wave vector is measured.

In the case of x‐ray and gamma‐ray detection, the detector itself is usually the collecting aperture. As the particles interact with the detector material, ionization occurs, leading to light emission or charge release. Detection of the emitted light or generated current gives a measurement of the incident energy flux.

2.5 Interaction of Electromagnetic Waves with Matter: Quick Overview

The interaction of electromagnetic waves with matter (e.g., molecular and atomic structures) calls into play a variety of mechanisms which are mainly dependent on the frequency of the wave (i.e., its photon energy) and the energy level structure of the matter. As the wave interacts with a certain material, be it gas, liquid, or solid, the electrons, molecules, and/or nuclei are put into motion (rotation, vibration, or displacement), which leads to exchange of energy between the wave and the material. This section gives a quick simplified overview of the interaction mechanisms between waves and matter. Detailed discussions are given later in the appropriate chapters throughout the text.

Atomic and molecular systems exist in certain stationary states with well‐defined energy levels. In the case of isolated atoms, the energy levels are related to the orbits and spins of the electrons. These are called the electronic levels. In the case of molecules, there are additional rotational and vibrational energy levels which correspond to the dynamics of the constituent atoms relative to each other. Rotational excitations occur in gases where molecules are free to rotate. The exact distribution of the energy levels depends on the exact atomic and molecular structure of the material. In the case of solids, the crystalline structure also affects the energy levels’ distribution.

In the case of thermal equilibrium, the density of population N iat a certain level i is proportional to (Boltzmann’s law):

(2.39) Introduction to the Physics and Techniques of Remote Sensing - изображение 90

where E iis the level energy, k is Boltzmann’s constant, and T is the absolute temperature. At absolute zero all the atoms will be in the ground state. Thermal equilibrium requires that a level with higher energy be less populated than a level of lower energy ( Fig. 2.13).

To illustrate, for T = 300 K, the value for kT is 0.025 eV (one eV is 1.6 × 10 −19joules). This is small relative to the first excited energy level of most atoms and ions, which means that very few atoms will be in the excited states. However, in the case of molecules, some vibrational and many rotational energy levels could be even smaller than kT , thus allowing a relatively large population in the excited states.

Figure 213 Curve illustrating the exponential decrease of population as a - фото 91

Figure 2.13 Curve illustrating the exponential decrease of population as a function of the level energy for the case of thermal equilibrium.

Let us assume a wave of frequency ν is propagating in a material where two of the energy levels i and j are such that

(2.40) Introduction to the Physics and Techniques of Remote Sensing - изображение 92

This wave would then excite some of the population of level i to level j . In this process, the wave loses some of its energy and transfers it to the medium. The wave energy is absorbed. The rate p ijof such an event happening is equal to:

(2.41) картинка 93

where ℰ νis the wave energy density per unit frequency and B ijis a constant determined by the atomic (or molecular) system. In many texts, p ijis also called transition probability.

Once exited to a higher level by absorption, the atoms may return to the original lower level directly by spontaneous or stimulated emission, and in the process they emit a wave at frequency ν , or they could cascade down to intermediate levels and in the process emit waves at frequencies lower than ν (see Fig. 2.14). Spontaneous emission could occur any time an atom is at an excited state independent of the presence of an external field. The rate of downward transition from level j to level i is given by

(2.42) картинка 94

where A jiis characteristic of the pair of energy levels in question.

Stimulated emission corresponds to downward transition which occurs as a result of the presence of an external field with the appropriate frequency. In this case the emitted wave is in phase with the external field and will add energy to it coherently. This results in an amplification of the external field and energy transfer from the medium to the external field. The rate of downward transition is given by

(2.43) Figure 214 An incident wave of frequency ν ijis adsorbed due to population - фото 95

Figure 214 An incident wave of frequency ν ijis adsorbed due to population - фото 96

Figure 2.14 An incident wave of frequency ν ijis adsorbed due to population excitation from E ito E j. Spontaneous emission for the above system can occur at ν ijas well as by cascading down via the intermediate levels l and k .

The relationships between A ji, B ji, and B ijare known as the Einstein’s relations:

(2.44) 245 where n is the index of refraction of the medium Let us now consider - фото 97

(2.45) where n is the index of refraction of the medium Let us now consider a medium - фото 98

where n is the index of refraction of the medium.

Let us now consider a medium that is not necessarily in thermal equilibrium and where the two energy levels i and j are such that E i< E j. N iand N jare the population in the two levels, respectively. The number of downward transitions from level j to level i is ( A ji+ B jiℰ ν) N j. The number of upward transitions is B ijℰ ν N i= B jiℰ ν N i. The incident wave would then lose ( N i− N j) B ijℰ νquanta per second. The spontaneously emitted quanta will appear as scattered radiation which does not add coherently to the incident wave.

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