Principles of Remote Sensing: The Photon and Radiometric Quantities

Most remote sensing texts begin by giving a survey of the main principles, to build a theoretical background, mainly in the physics of radiation. While it is important to have such a framework to pursue many aspects of remote sensing, we do not delve into this complex subject in much detail at this point. Instead, we offer on this and the next several pages an outline survey of the basics of relevant electromagnetic concepts. On this page, the nature of the photon is the prime topic. Photons of different energy values are distributed through what is called the Electromagnetic Spectrum. A full discussion of the electromagnetic spectrum (EMS) is deferred to page I-4. Hereafter in this Introduction and in the Sections that follow, we limit the discussion and scenes examined to remote sensing products obtained almost exclusively by measurements within the Electromagnetic Spectrum (force field and acoustic remote sensing are briefly covered elsewhere in the Tutorial). Our emphasis is on pictures (photos) and images (either TV-like displays on screens or “photos” made from data initially acquired as electronic signals, rather than recorded directly on film). We concentrate mainly on images produced by sensors operating in the visible and near-IR segments of the electromagnetic spectrum (see the spectrum map on page I-4), but also inspect a fair number of images obtained by radar and thermal sensors.

The next several pages strive to summarize much of the underlying theory – mainly in terms of Physics – appropriate to Remote Sensing. The reader can gain most of the essential knowledge just through those pages. The writer’s (NMS) original, but now unavailable, “Landsat Tutorial Workbook”, the information source from which this Remote Sensing Tutorial is an updated extension and expansion, contains a more detailed treatment of many aspects of the theory, including a different treatment of quantum theory and an examination of how spectroscopy helped to develop that theory. So, optionally you can choose to read a reproduction of extracts from the Landsat T W version to extend your basic understanding by clicking onto the hidden page I-2a. Or, if you choose not to, read this next inserted paragraph which synopsizes key ideas from both the present and the I-2a pages:


Synoptic Statement: The underlying basis for most remote sensing methods and systems is simply that of measuring the varying energy levels of a single entity, the fundamental unit in the electromagnetic (which may be abbreviated “EM”) force field known as the photon. As you will see later on this page, variations in photon energies (expressed in Joules or ergs) are tied to the parameter wavelength or its inverse, frequency. EM radiation that varies from high to low energy levels comprises the ElectroMagnetic spectrum (EMS). Radiation from specific parts of the EM spectrum contain photons of different wavelengths whose energy levels fall within a discrete range of values. When any target material is excited by internal processes or by interaction with incoming EM radiation, it will emit or reflect photons of varying wavelengths whose radiometric quantities differ at different wavelengths in a way diagnostic of the material. Photon energy received at detectors is commonly stated in power units such as Watts per square meter per wavelength unit. The plot of variation of power with wavelength gives rise to a specific pattern or curve that is the spectral signature for the substance or feature being sensed (discussed on page I-5).


Now, in more detail: The photon is the physical form of a quantum, the basic particle studied in quantum mechanics (which deals with the physics of the very small, that is, particles and their behavior at atomic and subatomic levels). The photon is also described as the messenger particle for EM force or as the smallest bundle of light. This subatomic massless particle comprises radiation emitted by matter when it is excited thermally, or by nuclear processes (fusion, fission), or by bombardment with other radiation. It also can become involved as reflected or absorbed radiation. Photons move at the speed of light: 299,792.46 km/sec (commonly rounded off to 300,000 km/sec or ~186,000 miles/sec). These particles also move as waves and hence, have a “dual” nature. These waves follow a pattern that can be described in terms of a sine (trigonometric) function, as shown in two dimensions in the figure below.

A simplified sketch shows the nature of a sine wave and the inter-relations of frequency (and wavelength) and relative energy.

The distance between two adjacent peaks on a wave is its wavelength. The total number of peaks (top of the individual up-down curve) that pass by a reference lookpoint in a second is that wave’s frequency (in units of cycles per second, whose SI version [SI stands for System International] is known as a Hertz [1 Hertz = 1/s-1]).

A photon travels as an EM wave having two components, oscillating as sine waves mutually at right angles, one consisting of the varying electric field, the other the varying magnetic field. Both have the same amplitudes (strengths) which reach their maxima-minima at the same time. Unlike other wave types which require a carrier (e.g., water waves), photon waves can transmit through a vacuum (such as in space). When photons pass from one medium to another, e.g., air to glass, their wave pathways are bent (follow new directions) and thus experience refraction.

A photon is said to be quantized, in that any given one possesses a certain quantity of energy. Some other photon can have a different energy value. Photons as quanta thus show a wide range of discrete energies. The amount of energy characterizing a photon is determined using Planck’s general equation:

Mathematical equation 1

where h is Planck’s constant (6.6260… x 10-34 Joules-sec)* and v is the Greek letter, nu, representing frequency (the letter “f” is sometimes used instead of v). Photons traveling at higher frequencies are therefore more energetic. If a material under excitation experiences a change in energy level from a higher level E2 to a lower level E1, we restate the above formula as:

Mathematical equation 2

where v has some discrete value determined by (v2v1). In other words, a particular energy change is characterized by producing emitted radiation (photons) at a specific frequency v and a corresponding wavelength at a value dependent on the magnitude of the change.λ.

I-4 Is there something wrong with the equation just above? ANSWER

Wavelength is the inverse of frequency (higher frequencies associate with shorter wavelengths; lower with longer), as given by the relationship:

Mathematical equation 3

where c is the constant that expresses the speed of light, so that we can also write the Planck equation as

Mathematical equation 4

I-5 Come up with a very simple mnemonic phrase (one that helps your memory) for associating the energy level (amount of energy) with wavelength. ANSWER

I-6: Calculate the wavelength of a quantum of radiation whose photon energy is 2.10 x 10-19 Joules; use 3 x 108 m/sec as the speed of light c. ANSWER

I-7: A radio station broadcasts at 120 MHz (megahertz or a million cycles/sec); what is the corresponding frequency in meters (hint: convert MHz to units of Hertz). ANSWER

A beam of radiation (such as from the Sun) is usually polychromatic (has photons of different energies); if only photons of one wavelength are involved the beam is monochromatic. The distribution of all photon energies over the range of observed frequencies is embodied in the term spectrum (a concept developed on the next page). A photon with some specific energy level occupies a position somewhere within this range, i.e., lies at some specific point in the spectrum

How are the photon energy levels in EM radiation quantified and measured? The answer lies in the discovery of the photoelectric effect made by Albert Einstein in 1905. Consider this diagram:

The photoelectric effect.

Einstein found that when light strikes a metal plate C, photoelectrons (negative charges) are ejected from its surface. In the vacuum those electrons will flow to a positively charged wire (unlike charges attract) that acts as a cathode. Their accumulation there produces an electric current which can be measured by an ammeter or voltmeter. The photoelectrons have kinetic energy whose maximum is determined by making the wire potential ever more negative (less positive) until at some value the current ceases. The magnitude of the current depends on the radiation frequencies involved and on the intensity of each frequency. From a quantum standpoint (Einstein’s discovery helped to verify Planck’s quantum hypothesis), the maximum kinetic energy is given by:

K.E. = hf + φ (the energy needed to free the electron)

This equation indicates that the energy associated with the freed electron depends on the frequency (multiplied by the Planck constant h) of the photon that strikes the plate plus a threshold amount of energy required to release the electron (φ, the work function). By measuring the current, and if that work energy is known and other adjustments are made, the frequency of the photon can be determined. His experiments also revealed that regardless of the radiation intensity, photoelectrons are emitted only after a threshold frequency is exceeded. For frequencies below the threshold, no electron emission takes place; for those higher than the threshold value (exceeding the work function) the numbers of photoelectrons released re proportional to the number of incident photons (this number is given by the intensities involved.

When energies involved in processes from the molecular to subatomic level are involved (as in the photoelectric effect), these energies are measured in electron volt units (1 eV = 1.602 x 10-19; this number relates to the charge on a single electron, as a fraction of the SI unit for charge quantity, the Coulomb [there are about 6.24 x 1018 electrons in one Coulomb).

Astute readers may have recognized the photoelectric effect as being involved in the operation of vacuum tubes in early radio sets. In remote sensing, the sensors used contain detectors that produce currents (and voltages, remember V = IR) whose quantities for any given frequency depend on the photoelectric effect.

From what’s been covered so far on this page, let’s modify the definition of remote sensing (previous page) to make it “quantum phenomenological”. In this approach, electromagnetic remote sensing involves the detection of photons of varying energies coming from the target (after the photons are generated by selective reflectance or by internal emittance from the target material(s)) by passing them through frequency (wavelength)- dependent dispersing devices (filters; prisms) onto metals or metallic compounds/alloys which undergo photoelectric responses to produce currents that become signals that can be analyzed in terms of energy-dependent parameters (frequency, intensity, etc.) whose variations are controlled by the atomic level composition of the targets. The spectral (wavelength) dependency of each material is diagnostic of its unique nature. When these photon variations are plotted in X-Y space, the shapes of the varied distributions of photon levels produce patterns that further aid in identifying each material (with likely regrouping into a class or physical feature.

There is much more to the above than the brief exposition and summary given. Read the next page for more elaboration. Consult a physics text for more information. Or, for those with some physics background, read the Chapter on The Nature of Electromagnetic Radiation in the Manual of Remote Sensing, 2nd Ed., published by the American Society of Photogrammetry and Remote Sensing (ASPRS). This last source contains a summary table that lists and defines what can be called basic radiometric quantities but the print is too small to reproduce on this page. The following is an alternate table which should be legible on most computer screens.

Table of Radiometric Quantities.

From the Manual of Remote Sensing Chapter 2, the writer has extracted the following useful information that explains some of the radiometric terminology and the concepts they represent as used by specialists in the remote sensing field: Radiant energy (Q), transferred as photons moving in a radiation stream, is said to emanate in minutely short bursts (comprising a wave train) from a source in an excited state. This stream of photons moves along lines of flow (also called rays) as a flux (φ) which is defined as the time rate at which the energy Q passes a spatial reference (in calculus terms:φ = dQ/dt). The energy involved is capable of doing work. The SI units of work are Joules per second (alternately expressed in ergs, which equal 10-7 Joules). The flux concept is related to power, defined as the time rate of doing work or expending energy (1 J/sec = 1 Watt, the unit of power). The nature of the work can be one, or a combination, of these: changes in motion of particles acted upon by force fields; heating; physical or chemical change of state. Depending on circumstances, the energy spreading from a point source may be limited to a specific direction (a beam) or can disperse in all directions.

Radiant flux density is just the energy per unit volume (cubic meters or cubic centimeters). The flux density is proportional to the squares of the amplitudes of the component waves. Flux density as applied to radiation coming from an external source to the surface of a body is referred to as irradiance (E); if the flux comes out of that body, it’s nomenclature is exitance (M) (see below for a further description).

. The intensity of radiation is defined as the power P that flows through unit area A (I = P/A); power itself is given by P = ΔE/Δt (the rate at which radiant energy is generated or is received). The energy of an EM wave (sine wave) depends on the square of its amplitude (height of wave in the x direction; see wave illustration above); thus, doubling the amplitude increases the power by 4. Another formulation of radiant intensity is given by the radiant flux per unit of solid angle ω (in steradians – a cone angle in which the unit is a radian or 57 degrees, 17 minutes, 44 seconds); this diagram may help to visualize this:

Radiant Intensity Diagram.

Thus, for a surface at a distance R from a point source, the radiant intensity I is the flux Φ flowing through a cone of solid angle ω on to the circular area A at that distance, and is given by I = Φ/(A/R2). Note that the radiation is moving in some direction or pathway relative to a reference line as defined by the angle θ.

From this is derived a fundamental EM radiation entity known as radiance (commonly noted as “L”). In the ASPRS Manual of Remote Sensing, “radiance is defined as the radiant flux per unit solid angle leaving an extended source (of area A) in a given direction per unit projected surface area in that direction.” This diagram, from that Manual, visualizes the terms and angles involved:

Radiance defined diagrammatically.

As stated mathematically, L = Watt � m-2 � sr-1; where the Watt term is the radiant flux (power, or energy flowing through the reference surface area of the source [square meters] per unit time), and “sr” is a solid angle Ω given as 1 steradian. From this can be derived L = Φ/Ω times 1/Acos θ, where θ is the angle formed by a line normal to the surface A and the direction of radiant flow. Or, restated with intensity specified, L = I/Acosθ. Radiance is loosely related to the concept of brightness as associated with luminous bodies. What really is measured by remote sensing detectors are radiances at different wavelengths leaving extended areas (which can “shrink” to point sources under certain conditions). When a specific wavelength, or continuum of wavelengths (range) is being considered, then the radiance term becomes Lλ.

In practical use, the radiance measured by a sensor operating above the ground is given by:

Ltot = ρET/π + Lp

where Ltot is the total spectral radiance (all wavelength) received by the sensor; ρ is the reflectance from the ground object being sensed; E is the irradiance (incoming radiant energy acting on the object); T is an atmospheric transmission function; and Lp is radiance from the atmospheric path itself.

Radiant fluxes that come out of sources (internal origin) are referred to as radiant exitance (M) or sometimes as “emittance” (now obsolete). Radiant fluxes that reach or “shine upon” any surface (external origin) are called irradiance. Thus, the Sun, a source, irradiates the Earth’s atmosphere and surface.

The above radiometric quantities Q, φ, I, E, L, and M, apply to the entire EM spectrum. Most wave trains are polychromatic, meaning that they consist of numerous sinusoidal components waves of different frequencies. The bundle of varying frequencies (either continuous within the spectral range involved or a mix of discrete but discontinuous monochromatic frequencies [wavelengths]) constitutes a complex or composite wave. Any complex wave can be broken into its components by Fourier Analysis which extracts a series of simple harmonic sinusoidal waves each with a characteristic frequency, amplitude, and phase. The radiometric parameters listed in the first sentence can be specified for any given wavelength or wavelength interval (range); this spectral radiometric quantity (which has a value different from those of any total flux of which they are a part [unless the flux is monochromatic]) is recognized by the addition to the term of a subscript λ, as in Lλ and Qλ. This subscript denotes the specificity of the radiation as at a particular wavelength. When the wavelengths being considered are confined to the visual range of human eyes (0.4 to 0.7 µm), the term “luminous” precedes the quantities and their symbols are presented with the subscript “v”, as Φv for a luminous flux.

EM radiation can be incoherent or coherent. Waves whose amplitudes are irregular or randomly related are incoherent; polychromatic light fits this state. If two waves of different wavelengths can be combined so as to develop a regular, systematic relationship between their amplitudes, they are said to be coherent; monochromatic light generated in lasers meet this condition.

The above, rather abstract, sets of ideas and terminology is important to the theorist. We include this synopsis mainly to familiarize you with these radiometric quantities in the event you encounter them in other reading.

SOURCE:http://rst.gsfc.nasa.gov

About Rashid Faridi

I am Rashid Aziz Faridi ,Writer, Teacher and a Voracious Reader.
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1 Response to Principles of Remote Sensing: The Photon and Radiometric Quantities

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