Late in the morning of April 28, 1958, the USSÂ
Boxer aircraft carrier ship was about 70 miles  off the coast of the Bikini Atoll in the PacificÂ
Ocean. The crew of the Boxer was preparing to  launch a high-altitude helium balloon. In fact,Â
this would be the 17th high-altitude balloon to be  launched from the ship. But this one was a littleÂ
different. Where those first 16 balloons carried  some instruments and dummy payloads, attached toÂ
this balloon was a 1.7 kiloton nuclear warhead,  code named Yucca. The ship, balloon, andÂ
bomb were all part of operation Hardtack,  a series of nuclear tests conducted by the UnitedÂ
States in 1958. Yucca was the first test of a  nuclear blast in the upper limits of earth’sÂ
atmosphere. About an hour and a half after the  balloon was launched, it reached an altitude ofÂ
85,000 feet or about 26,000 meters. As two B-36Â Â peacemaker bombers loaded down with instrumentsÂ
circled the area, the warhead was detonated. Of course, the research team collectedÂ
all kinds of data during the blast,  including the speed of the shockÂ
wave, the effect on air pressure,  and the magnitude of nuclear radiationÂ
released. But, from two locations on the ground,  they were also measuring the electromagneticÂ
waves resulting from the blast. It had been  known since the first nuclear explosionsÂ
that the blasts generate an electromagnetic  pulse or EMP, mainly because it kept fryingÂ
electronic instruments. But until Hardtack,  nobody had ever measured the waves generated fromÂ
a detonation in the upper atmosphere. What they  recorded was so far beyond their expectations,Â
that it was dismissed as an anomaly for years.  All that appears in the report is a casual mentionÂ
of the estimated electromagnetic field strength  at one of the monitoring stations being aroundÂ
5 times the maximum limit of the instruments. It wasn’t until 5 years later that the USÂ
physicist Conrad Longmire would propose  a theory for electromagnetic pulses fromÂ
high-altitude nuclear blasts that is still  the widely accepted explanation for why they areÂ
orders of magnitude stronger than those generated  from blasts on the ground. Since then, our fearsÂ
of nuclear war not only included the scenario of  a warhead hitting a populated area, destroyingÂ
cities and creating nuclear fallout, but also  the possibility of one detonating far above ourÂ
heads in the upper atmosphere, sending a strong  enough EMP to disrupt electronic devices and evenÂ
take out the power grid. As with most weapons,  the best and most comprehensive research onÂ
EMPs is classified. But, in 2019, a coalition  of energy organizations and government entitiesÂ
called the Electric Power Research Institute (or  EPRI) funded a study to try and understand exactlyÂ
what could happen to the power grid from a high  altitude nuclear EMP. It’s not the only studyÂ
of its kind, and it’s not without criticism from  those who think it leans optimistic, but it hasÂ
the most juicy engineering details from all the  research I could find. And the answers are quiteÂ
a bit different than Hollywood would have you  believe. This is a summary of that report, andÂ
it’s the first in a deep dive series of videos  about large-scale threats to the grid. I’mÂ
Grady, and this is Practical Engineering. In  today’s episode, we’re talking about the impactÂ
of a nuclear EMP on our power infrastructure. This video is sponsored by CuriosityStreamÂ
and Nebula. More on them later. A nuclear detonation is unwelcome inÂ
nearly every circumstance. These events  are inherently dangerous and the physics ofÂ
a blast go way beyond our intuitions. That’s  especially true in the upper atmosphere whereÂ
the detonation interacts with earth’s magnetic  field and its atmosphere in some very uniqueÂ
ways to create an electromagnetic pulse. An  EMP actually has three distinct componentsÂ
all formed by different physical mechanisms  that can have significantly different impactsÂ
here on Earth’s surface. The first part of an  EMP is called E1. This is the extremely fast andÂ
intense pulse that immediately follows detonation. The gamma rays released during any nuclearÂ
detonation collide with electrons, ionizing  atoms and creating a burst of electromagneticÂ
radiation. That’s generally bad on its own,  but when detonated high in the atmosphere,Â
earth’s magnetic field interacts with those  free electrons to produce a significantly strongerÂ
electromagnetic pulse than if detonated within the  denser air at lower altitudes. The E1 pulseÂ
comes and goes within a few nanoseconds,  and the energy is somewhat jokinglyÂ
referred to as DC to daylight,  meaning it’s spread across a hugeÂ
part of the electromagnetic spectrum. The E1 pulse generally reaches anywhereÂ
within a line of sight of the detonation,  and for a high-altitude burst, this canÂ
cover an enormous area of land. At the  height of the Yucca test, that’s a circleÂ
with an area larger than Texas. A weapon  at 200 kilometers in altitude could impact aÂ
significant fraction of North America. But,  not everywhere within that circle experiencesÂ
the strongest fields. In general, the further  from the blast you are, the lower the amplitude ofÂ
the EMP. But, because of earth’s magnetic field,  the maximum amplitude occurs a little bit southÂ
of ground zero (in the northern hemisphere),  creating this pattern called a smile diagram.Â
But no one will be smiling to find out that  they are within the affected areaÂ
of a high altitude nuclear blast. Although a weapon like this wouldn’tÂ
damage buildings, create nuclear fallout,  be felt by humans, or probably even be visibleÂ
to most, that E1 pulse can have a huge effect  on electronic devices. You’re probably familiarÂ
with antennas that convert radio signals into  voltage and current within a conductor. Well, forÂ
a strong enough pulse spread across a huge range  of frequencies, essentially any metallic objectÂ
will act like an antenna, converting the pulse  into massive voltage spikes that can overwhelmÂ
digital devices. And, the E1 pulse happens  so quickly that even devices meant to protectÂ
against surges may not be effective. Of course,  with just about everything having embeddedÂ
electronics these days, this has far reaching  implications. But on the grid, there are reallyÂ
only a few places where an E1 pulse is a major  concern. The first is with the control systemsÂ
within power plants themselves. The second is  communications systems used to monitor and recordÂ
data to assist grid operators. The EPRI report  focused primarily on the third hazard associatedÂ
with an E1 pulse: digital protective relays. Most folks have seen the breakers that protectÂ
circuits in your house. The electrical grid has  similar equipment used to protect transmissionÂ
lines and transformers in the event of a short  circuit or fault. But, unlike the breakers in yourÂ
house that do both the sensing for trouble and  the circuit breaking all in one device, thoseÂ
roles are separate on the grid. The physical  disconnecting of a circuit under load is doneÂ
by large, motor controlled contactors quenched  in oil or dielectric gas to prevent the formationÂ
of arcs. And the devices that monitor voltage and  current for problems and tell the breakers when toÂ
fire are called relays. They’re normally located  in a small building in a substation to protectÂ
them from weather. That’s because most relays  these days are digital equipment full of circuitÂ
boards, screens, and microelectronics. And all  those components are particularly susceptibleÂ
to electromagnetic interference. In fact,  most countries have strict regulations aboutÂ
the strength and frequency of electromagnetic  radiation you can foist upon the airwaves, rulesÂ
that I hope I’m not breaking with this device. This is a pulse generator I bought off eBayÂ
just to demonstrate the weird effects that  electromagnetic radiation can have onÂ
electronics. It just outputs a 50 MHz  wave through this antenna, and you can seeÂ
when I turn it on near this cheap multimeter,  it has some strange effects. TheÂ
reading on the display gets erratic,  and sometimes I can get the backlight to turnÂ
on. You can also see the two different types  of E1 vulnerabilities here. An EMP can couple toÂ
the wires that serve as inputs to the device. And  an EMP can radiate the equipment directly.Â
In both cases, this little device wasn’t  strong enough to cause permanent damage to theÂ
electronics, but hopefully it helps you imagine  what’s possible when high strength fieldsÂ
are applied to sensitive electronic devices. The EPRI report actually subjected digitalÂ
relays to strong EMPs to see what the effects  would be. They used a Marx generatorÂ
which is a voltage multiplying circuit,  so I decided to try it myself. A Marx generatorÂ
stores electricity in these capacitors as they  charge in parallel. When triggered, the sparkÂ
gaps connect all the capacitors in series to  generate very high voltages, upwards of 80 or 90Â
kilovolts in my case. My fellow YouTube engineer  Electroboom has built one of these on hisÂ
channel if you want to learn more about them. Mine generates a high voltage sparkÂ
when triggered by this screwdriver. Don’t try this at home, by the way. I didn’t design an antenna to convertÂ
this high voltage pulse into an EMP,  but I did try a direct injection test. This cheapÂ
digital picture frame didn’t stand a chance.  Just to clarify, this is in no wayÂ
a scientific test. It’s just a fun  demonstration to give you an idea ofÂ
what an E1 pulse might be capable of. The E2 pulse is slower than E1 becauseÂ
it’s generated in a totally different way,  this time from the interaction of gamma raysÂ
and neutrons. It turns out that an E2 pulse is  roughly comparable to a lightning strike.Â
In fact, many lightning strikes are more  powerful than those that could be generated byÂ
high-altitude nuclear detonations. Of course,  the grid’s not entirely immune to lightning,Â
but we do use lots of lightning protection  technology. Most equipment on the grid isÂ
already hardened against some high voltage  pulses such that lightning strikesÂ
don’t usually create much damage. So,  the E2 pulse isn’t as threatening to our powerÂ
infrastructure, especially compared to E1 and E3. The final component of an EMP, called E3,Â
is, again, much different from the other two.  It’s really not even a pulse at all, becauseÂ
it’s generated in an entirely different way.  When a nuclear detonation happens in the upperÂ
atmosphere, earth’s magnetic field is disturbed  and distorted. As the blast dissipates, theÂ
magnetic field slowly returns to its original  state over the course of a few minutes. This isÂ
similar to what happens when a geomagnetic storm  on the sun disrupts earth’s gravity, and largeÂ
solar events could potentially be a bigger threat  than a nuclear EMP to the grid. In both cases,Â
it’s because of the disturbance and movement of  earth’s magnetic field. You probably know whatÂ
happens when you move a magnetic field through  a conductor: you generate a current. We call thatÂ
coupling, and it’s essentially how antennas work.  And in fact, antennas work best when their sizeÂ
matches the size of the electromagnetic waves. For example, AM radio uses frequenciesÂ
between down to 540 kilohertz. That  corresponds to wavelengths that canÂ
be upwards of 1800 feet or 550 meters,  big waves. Rather than serving as a place toÂ
mount antennas like FM radio or cell towers,  AM radio towers are the antenna. The entire metalÂ
structure is energized! You can often tell an AMÂ Â tower by looking at the bottom becauseÂ
they sit atop a small ceramic insulator  that electrically separates them from the ground.Â
As you can imagine, the longer the wavelength, the  larger an antenna has to be to couple well withÂ
the electromagnetic radiation. And hopefully you  see what I’m getting at. Electrical transmissionÂ
and distribution lines often run for miles, making  them the ideal place for an E3 pulse to coupleÂ
and generate current. Here’s why that’s a problem. All along the grid we use transformers to changeÂ
the voltage of electricity. On the transmission  side, we increase the voltage to reduce lossesÂ
in the lines. And on the distribution side,  we lower the voltage back down to make itÂ
safer for customers to use in their houses  and buildings. Those transformers workÂ
using electromagnetic fields. One coil  of wire generates a magnetic field thatÂ
passes through a core to induce current  to flow through an adjacent coil. In fact, theÂ
main reason we use alternating current on the  grid is because it allows us to use theseÂ
really simple devices to step voltage up or  relationship between how much current flows andÂ
the strength of the resulting magnetic field. But,  this relationship breaks down at the saturationÂ
point, beyond which additional current won’t  create much further magnetism to driveÂ
current on the secondary winding. An E3 pulse  can induce a roughly DC flow of current throughÂ
transmission lines. So you have DC on top of AC,  which creates a bias in the sine wave. If there’sÂ
too much DC current, the transformer core might  saturate when current moves in one direction butÂ
not the other, distorting the output waveform.  That can lead to hot spots in the transformerÂ
core, damage to devices connected to the grid  that expect a nice sinusoidal voltageÂ
pattern, and lots of other funky stuff. So what are the implications of all this? For theÂ
E1 pulse damaging some relays, that’s probably not  a big deal. There are often redundant paths forÂ
current to flow in the transmission system. That’s  why it’s called the grid. But the more equipmentÂ
that goes offline and the greater the stress on  the remaining lines, the greater the likelihoodÂ
of a cascading failure or total collapse. EPRI did  tests simulating a one megaton bomb detonatedÂ
at 200 kilometers in altitude. They estimated  that about 5% of transmission lines could haveÂ
a relay that gets damaged or disrupted by the  resulting EMP. That alone probably isn’t enoughÂ
to cause a large-scale blackout of the power grid,  but don’t forget about E3. EPRI found that theÂ
third part of an EMP could lead to regional  blackouts encompassing multiple states becauseÂ
of transformer core saturation and imbalances  between supply and demand of electricity.Â
Their modeling didn’t lead to widespread  damage to the actual transformers, and that’s aÂ
good thing because power transformers are large,  expensive devices that are hard to replace,Â
and most utilities don’t keep many spares  sitting around. All that being said,Â
their report isn’t without criticism and  many believe that an EMP could result in farÂ
more damage to electric power infrastructure. When you combine the effects of the E1 pulse andÂ
the E3 pulse, it’s not hard to imagine how the  grid could be seriously disabled. It’s also easyÂ
to see how, even if the real damages to equipment  aren’t that significant, the widespread natureÂ
of an EMP, plus its potential impacts on other  systems like computers and telecommunications,Â
has the potential to frustrate the process of  getting things back online. A multi-day,Â
multi-week, or even multi-month blackout  isn’t out of the question in the worst-caseÂ
scenario. It’s probably not going cause a  hollywood-style return to the stone age forÂ
humanity, but it is certainly capable of  causing a major disruption to our daily lives.Â
We’ll explore what that means in a future video. But if you have trouble waiting forÂ
the next Practical Engineering video,  you should know that they go live on NebulaÂ
before hitting YouTube, and you can watch them  without any ads. If you haven’t heard aboutÂ
Nebula by now, it’s a streaming service built  by creators that uses a different model thanÂ
YouTube. Instead of being supported by ads,  you just pay a small subscription fee. That soundsÂ
like a small difference, but the result is a  huge distinction in content, including videosÂ
that just don’t work well on YouTube and lots  of original series from your favorite creatorsÂ
like Wendover Productions and Real Engineering. And, we’re super excited to continue ourÂ
partnership with CuriosityStream, a service with  thousands of big-budget documentaries on prettyÂ
much every subject you can imagine. Curiosity  Stream loves independent creators, so they’reÂ
offering free access to Nebula when you sign  up at CuriosityStream.com/practicalengineering.Â
I know it’s a little hard to keep track of all  the streaming services out there right now, butÂ
this bundle is so cheap that you barely have to  even consider it. You pay one time, 15 bucks, toÂ
get an entire year of access to CuriosityStream  PLUS you get a free year of access to Nebula too.Â
If you’re looking for more about the power grid,  the How Cities Work series on CuriosityStream hasÂ
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for watching, and let me know what you think!
I love this channel, found it about a year ago and watch every one when they release. Always super educational and interesting topics
Love the googly eyes on the oscilloscope
The real danger (which he somewhat alluded to) is not so much from a nuclear weapon, but instead from naturally occurring geomagnetic storms originating from solar flares, like the Carrington Event:
https://en.wikipedia.org/wiki/Carrington_Event
That event occurred in 1859 and was so intense it made telegraph stations catch on fire. You can somewhat imagine what it would do in our modern age of highly sensitive digital technology. The good news is, we can kind of see this coming by monitoring the sun and space weather, and might be able to disconnect some of the more sensitive portions of the power grid ahead of time. The bad news is, it is difficult to EMP-harden the power transmission lines; about the most effective thing would be bury all of them, but that would be extremely expensive, time consuming, and in many places impossible.
If you want a (rather terrifying) read on how this might impact civilization, I recommend reading One Second After:
https://en.m.wikipedia.org/wiki/One_Second_After
Countries that have strategic nuclear weapons include this ability with strikes. A weapon is detonated in the atmosphere to create the EMP to knock out electronics which include communications and defence systems (good reason why military hardware is generally EMP hardened) shortly afterward the actual strikes happen.
If there's a time when a nuclear exchange could happen at any time and you're driving to work but suddenly everyone's car stops along with everything electronic for a seemingly unknown reason. You may as well step out of the car, put the sunglasses on and make peace with your maker.
Well I have to give this 2 thumbs up, pretty complete and accurate.
N. S
DNA EM-1 - Capabilities of Nuclear Weapons is a good read (though heavily redacted).
"Detonations above about 130,000 feet produce EMP effects on the ground over areas that may encompass thousands of square miles. Although the strengths of these fields are less than half those in the highly ionized region surrounding a surface burst, they are of sufficient magnitude to damage electrical and electronic equipment. The mechanisms of formation of EMP are treated in Chapter 7. "