Shedding Light on the Electromagnetic Spectrum

Prioritize…

At the completion of this section, you should be able to:

  1. define radiation, wavelength, and micron.
  2. discuss the organization of radiation in the electromagnetic spectrum by wavelength, including knowing which types of radiation have longer wavelengths and which have shorter wavelengths, for example).

Read…

So, we’ve now discussed that of the forms of energy, radiant energy (i.e., radiation) plays a central role. If you think of “radiation” and immediately conjure up images from science fiction movies or cautionary stories about nuclear energy, I can understand why! From a scientific perspective, radiation refers to the emission, transfer, and absorption of energy in the form of electromagnetic waves through space or a medium. It serves as a fundamental mechanism for transporting and exchanging energy within Earth's climate system. This encompasses solar radiation, which provides the energy that drives weather patterns and climate, as well as terrestrial radiation emitted by the Earth and its atmosphere.

Origins of Electromagnetic Spectrum of Radiation

During your science classes, you probably explored the electromagnetic spectrum of radiation. However, have you ever wondered about its origins? First, it's essential to recognize that all matter consists of atoms (the fundamental building blocks) and molecules (combinations of atoms). Within these already small structures exist even tinier particles with positive and negative charges, protons and electrons. Molecules tend to rotate andsibrate, and the electrons within them can move from lower energy orbitals to higher ones and vice versa. These movements of and within molecules lead to accelerations of the protons and electrons. Without delving into intricate details, physics teaches us that accelerated charges are the source of electromagnetic waves. It is amazing to think that all of the rotating water molecules around me (and most of the water molecules are indeed rotating!) are producing radiation, much of which strikes and is absorbed by my skin.

Another way to think about this is to imagine your hand as a vibrating molecule and a pond as the surrounding medium through which a wave propagates. Imagine moving your hand rapidly back and forth in the water – this generates waves that ripple out away from your hand and across the surface of the pond. Similarly, oscillating protons and electrons emit energy ripples known as electromagnetic "waves," and these waves propagate in every direction away from the accelerated charges whatever the surrounding medium might be, including the vacuum of space. These waves exhibit both electric and magnetic characteristics, hence the term “electromagnetic wave, or electromagnetic radiation, to describe them." The word “electromagnetic” is commonly abbreviated as “EM.”

Wavelengths

So, what gives rise to the different types of EM waves that form the complete spectrum? First, let's discuss the various categories of EM radiation based on wavelength. The wavelength of any wave is the distance from one identical point on the wave to the next, such as from crest to crest. Let's revisit our earlier analogy with the pond. When you move your hand through the water slowly, you generate a few waves with long wavelengths. Conversely, if you move your hand rapidly, you produce numerous waves with much shorter wavelengths. This same principle applies to an oscillating charge. When the oscillation is exceptionally fast (referred to as high frequency), the resulting EM radiation will have a short wavelength. Conversely, if the oscillation occurs at a slower rate (entailing a lower frequency), the electromagnetic waves will consist of longer wavelengths.

A wavelength with crest, trough amplitude and wavelength labled.
Basic Wavelength
Credit: Geoff Ruth, CC BY-SA 3.0 via Wikimedia Commons

Now, the frequencies at which of charges in molecules can oscillate is primarily determined by the type and arrangement of atoms that compose the molecules.The temperature of the medium in which the molecules are situated subsequently determines how many molecules are oscillating at each frequency. As the temperature of the medium goes up, higher frequency oscillations within the molecules occur Why? The temperature of any piece of matter is determined by the kinetic energy of the atoms or molecules that compose the material. Remember, kinetic energy is a measure of the energy of a substance due to translation through space – we usually think about it in terms of throwing a ball or a moving train, but atoms and moleculesare tiny forms of matter and they too, can be moving through space! The higher the temperature, the faster these particles are moving. When faster moving atoms and molecules bang into each other, they are able to transfer more kinetic energy into the rotations, vibrations, and orbital excitations within the colliding particles, which correspond to higher frequency oscillations. Higher frequency oscillations, in turn, correspond to smaller wavelengths of the EM waves they generate. Conversely, as the temperature of a collection of atoms and moleculesdecreases, the frequencies induced by colliding particles decreases, and the wavelengths emanating from the collection of particles increase.

Explore Further…

Take a few minutes to explore how to measure and compare wavelengths by completing the Describing a Wave activity.

A Caveat

Extremely high-frequency EM radiation emissions (e.g., gamma rays) necessitate an additional mechanism to produce them, which goes beyond the scope of what's necessary for this course as these emissions are not important for understanding weather and climate.

Complete Spectrum of Electromagnetic Radiation

Now that we've addressed that caveat, let's examine the complete spectrum of electromagnetic radiation depicted below. Firstly, it's important to recognize the vast range of wavelengths that different types of electromagnetic radiation encompass — from hundreds of meters down to the dimensions of an atom's nucleus. Additionally, it's worth acknowledging that visible light falls within the category of electromagnetic radiation, albeit occupying just a minuscule portion of the entire spectrum. This fact underscores that our eyes are effectively blind to nearly all forms of electromagnetic radiation.

Video: What it Light? Maxwell and the Electromagnetic Spectrum (3:55)

What it Light? Maxwell and the Electromagnetic Spectrum

Professor David: Hey it's Professor Dave, let's learn about light. He knows a lot about the science stuff, Professor Dave explains. Since we've been able to look up at the sun, we've been aware of light. As darkness is one of very few things that we instinctually fear, we have always bestowed light with godlike properties. But for all of antiquity, we had no idea what light really was.

Figures like Newton and Huygens worked with light in the 17th century, but a more sophisticated description of light, which we call classical electromagnetism, was developed largely by James Clerk Maxwell in the 19th century. This theory depicts light as a transverse wave composed of oscillating electric and magnetic fields, which are at right angles to each other, and perpendicular to the direction that the wave moves. We will learn more about these fields later. Just like the kinds of waves we have previously discussed, electromagnetic waves have amplitudes, wavelengths, and frequencies, but instead of different frequencies producing different pitches like sound waves, different frequencies of electromagnetic waves produce different kinds of light. If the light is visible, these frequencies will correspond to different colors.

Frequencies greater than this will exist as UV radiation, X-rays, or gamma rays, and frequencies less than this qualify as infrared radiation, microwaves, or radio waves. All of these phenomena are collectively referred to as electromagnetic radiation,, and they can be found on the electromagnetic spectrum. Here we can see all the wavelengths and frequencies ranging from radio waves to gamma rays, and we have found some technological use for all of these in modern society. Even though they seem dramatically different, some requiring things like antennas or other equipment to manipulate, all of them are fundamentally the same thing as the light you can see with your eyeballs. They are just of different wavelengths.

All electromagnetic radiation moves at the speed of light, which is about 300 million meters per second in a vacuum, the fastest speed possible in the universe. This is fast enough to get from here to the moon in about a second, and since we know that all waves move at a speed that is equal to their wavelength times their frequency, This product will be equal to the speed of light for any type of electromagnetic radiation. How is it that electromagnetic radiation is produced? To answer this question, we have to learn about electric fields, which are coming up soon. For now, let's check comprehension.

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Video: Science at NASA: An Introduction to the Electromagnetic Spectrum (5:19)

The Electromagnetic Spectrum

Presenter: Something surrounds you, bombards you. Some of which you can't see, touch, or even feel. Every day, everywhere you go, it is odorless and tasteless, yet you use it and depend on it every hour of every day. Without it, the world you know could not exist. What is it?

Electromagnetic radiation. These waves spread across a spectrum from very short gamma rays to X-rays, ultraviolet rays, visible light waves, even longer infrared waves, microwaves, to radio waves which can measure longer than a mountain range. This spectrum is the foundation of the information age and of our modern world. Your radio, remote control, text message, television, microwave oven, even a doctor's x-ray all depend on waves within the electromagnetic spectrum. Electromagnetic waves, or EM waves, are similar to ocean waves in that both are energy waves.

They transmit energy. EM waves are produced by the vibration of charged particles and have electrical and magnetic properties. But unlike ocean waves that require water, EM waves travel through the vacuum of space at the constant speed of light. EM waves have crests and troughs like ocean waves. The distance between crests is the wavelength.

While some EM wavelengths are very long and are measured in meters, many are tiny and are measured in billionths of a meter, nanometers. The number of these crests that pass a given point within 1 second is described as the frequency of the wave. One wave, or cycle, per second is called a hertz. Long EM waves, such as radio waves, have the lowest frequency and carry less energy. Adding energy increases the frequency of the wave and makes the wavelength shorter.

Gamma rays are the shortest, highest-energy waves in the spectrum. So, as you sit watching TV, not only are there visible light waves from the TV striking your eyes, but also radio waves transmitting from a nearby station, and microwaves carrying cell phone calls and text messages, and waves from your neighbor's Wi-Fi, and GPS units in the cars driving by. There is a chaos of waves from all across the spectrum passing through your room right now. With all these waves around you, how can you possibly watch your TV show? Similar to tuning a radio to a specific radio station, Our eyes are tuned to a specific region of the EM spectrum and can detect energy with wavelengths from 400 to 700 nanometers, the visible light region of the spectrum.

Objects appear to have color because EM waves interact with their molecules. Some wavelengths in the visible spectrum are reflected and other wavelengths are absorbed. This leaf looks green because EM waves interact with the chlorophyll molecules. Waves between 492 and 577 nanometers in length are reflected, and our eye interprets this as the leaf being green. Our eyes see the leaf as green but cannot tell us anything about how the leaf reflects ultraviolet, microwave, or infrared waves.

To learn more about the world around us, scientists and engineers have devised ways to enable us to see beyond that sliver of the EM spectrum called visible light. Data from multiple wavelengths help scientists study all kinds of amazing phenomena on Earth, from seasonal change to specific habitats. Everything around us emits, reflects, and absorbs EM radiation differently based on its composition. A graph showing these interactions across a region of the EM spectrum is called a spectral signature. Characteristic patterns, like fingerprints within the spectra, allow astronomers to identify an object's chemical composition and to determine such physical properties as temperature and density.

NASA's Spitzer Space Telescope observed the presence of water and organic molecules in a galaxy 3.2 billion light-years away. Viewing our Sun in multiple wavelengths with the SOHO satellite allows scientists to study and understand sunspots that are associated with solar flares and eruptions harmful to satellites, astronauts, and communications here on Earth. We are constantly learning more about our world and universe by taking advantage of the unique information contained in the different waves across the EM spectrum.

Credit: BestOfScience. The Electromagnetic Spectrum. YouTube. August 1, 2010.

 

Starting from the far end of the spectrum characterized by its longest wavelengths, often referred to as the “long-wave” segment, we encounter radio waves and microwaves, boasting wavelengths ranging from hundreds of meters to just a few millimeters (one-thousandth of a meter, or 10^-3 meters). As we delve into shorter wavelengths, we find measurements often expressed in micrometers, more commonly termed microns (one-millionth of a meter, or 10^-6 meters). Within this range, when wavelengths decrease to the scale of tens of microns, comparable in size to a bacterium or a virus, we classify these emissions as infrared, visible, and ultraviolet light. In the final stretch of the spectrum, characterized by exceedingly short wavelengths comparable in size to individual molecules or atoms, we encounter X-rays and gamma rays.

Electromagnetic spectrum
A diagram of the electromagnetic spectrum, with longer wavelengths on the left and shorter ones on the right. In this class, we'll be most particularly concerned with infrared, visible, and ultraviolet radiation.

A detailed visual representation of various types of electromagnetic radiation, their wavelengths, frequencies, and the temperature at which they are most intensely emitted. It includes a horizontal illustration of the electromagnetic spectrum, starting from radio waves on the left to gamma rays on the right.

Penetration of Earth's Atmosphere: A horizontal bar at the top illustrates whether each type of radiation penetrates Earth's atmosphere. It is divided into sections marked “Y” (Yes) and “N” (No), indicating if the radiation type can reach Earth.

Radiation Types and Wavelengths: A red waveform visually depicts the wavelength of each radiation type, starting with long wavelengths for radio waves and shortening progressively to gamma rays. Below, several categories of radiation types are listed with their respective wavelengths in meters: Radio (10³), Microwave (10⁻²), Infrared (10⁻⁵), Visible (0.5×10⁻⁶), Ultraviolet (10⁻⁸), X-ray (10⁻¹⁰), and Gamma ray (10⁻¹²).

Approximate Scale of Wavelengths: Various objects are depicted to represent the approximate scale of each radiation type's wavelength: buildings (radio), humans (microwave), butterflies (infrared), needle points (visible), protozoans (ultraviolet), molecules (X-ray), atoms (gamma ray), and atomic nuclei (gamma ray).

Frequency: A horizontal bar denotes the frequency range (Hz) corresponding to each type of radiation, starting from 10⁴ Hz (radio waves) to 10²⁰ Hz (gamma rays).

Temperature of Most Intense Emission: A colored horizontal scale at the bottom represents the temperature (in Kelvin and Celsius) at which each type of radiation is most intensely emitted. It ranges from 1K (-272°C) for radio waves to 10,000,000K (~10,000,000°C) for gamma rays.

Credit: EM Spectrum Properties by Inductive load, National Aeronautic and Space Administration (NASA) (Public Domain)

In the context of this course, our primary focus will be on infrared, visible, and ultraviolet radiation, as these are relevant for climate scientists studying how energy is transferred into, within, and out of the Earth system. Additionally, we'll delve further into the infrared spectrum in this lesson, which extends “beyond red.” Notably, a significant portion of the infrared spectrum, spanning approximately 3 to 100 microns, is called “terrestrial” or “longwave” radiation — radiation originating from Earth. This is because at the temperatures commonly observed on our planet, including those within Earth's atmosphere, the molecules that compose the Earth system emit EM waves mostly with these wavelengths.

Now that you are familiar with the terminology used to describe the various segments of the electromagnetic spectrum, it's imperative to explore the characteristics governing the emission of radiation. These properties are organized into what we can think of as the “four laws of radiation.” Let's delve into these further.

Quiz Yourself…