In June of 2022, the level in Lake Mead, theÂ
largest water reservoir in the United States  formed by the Hoover Dam, reached yet anotherÂ
all-time low of 175 feet or 53 meters below full,  a level that hasn’t been seen since the lake wasÂ
first filled in the 1930s. Rusted debris, sunken  boats, and even human remains have surfaced fromÂ
beneath the receding water level. And Lake Mead  doesn’t stand alone. In fact, it’s just a drop inÂ
the bucket. Many of the largest water reservoirs  in the western United States are at critically lowÂ
storage with the summer of 2022 only just getting  started. Lake Powell upstream of Lake Mead on theÂ
Colorado River is at its lowest level on record.  Lake Oroville (of the enormous spillway failureÂ
fame) and Lake Shasta, two of California’s  largest reservoirs, are at critical levels.Â
The combined reservoirs in Utah are below 50%Â Â full. Even many of the westernmost reservoirsÂ
here in Texas are very low going into summer. People use water at more or less a constantÂ
rate and yet, mother nature supplies it in  unpredictable sloshes of rain or snow thatÂ
can change with the seasons and often have  considerable dry periods between them. If theÂ
sloshes get too far apart, we call it a drought.  And at least one study has estimated that the pastÂ
two decades have been the driest period in more  than a thousand years for the southwestern UnitedÂ
States, leading to a so-called “mega-drought.”  Dams and reservoirs are one solution to thisÂ
tremendous variability in natural water supply.  But what happens when they stop filling up or (inÂ
the case of one lake in Oklahoma), what happens  when they never fill up in the first place?Â
I’m Grady, and this is Practical Engineering.  On today’s episode we’re talking about waterÂ
availability and water supply storage reservoirs. This video is sponsored by Brilliant,  the best way to learn math and scienceÂ
through problem solving. More on them later. The absolute necessity of water demands that cityÂ
planners always assume the worst case scenario.  If you have a dry year (or even a dry day),Â
you can’t just hunker down until the rainy  weather comes back. So the biggest question whenÂ
developing a new supply of water is the firm  yield. That’s the maximum amountÂ
of water the source will supply  during the worst possible drought.Â
Here’s an example to make this clearer: Imagine you’re the director of public works forÂ
a new town. To keep your residents hydrated and  clean, you build a pumping station on a nearbyÂ
river to collect that water and send it to a  treatment plant where it can be purified andÂ
distributed. This river doesn’t flow at a  constant rate. There’s lots of flow during theÂ
spring as mountain snowpack melts and runs off,  but the flow declines over the courseÂ
of the summer once that snow has melted  and rain showers are more spread out. InÂ
really dry years, when the snowpack is thin,  the flow in the river nearly driesÂ
up completely. In other words,  the river has no firm yield. It’s not a dependableÂ
supply of water in any volume. Of course, there is  water to be used most of the time, but most ofÂ
the time isn’t enough for this basic human need.  So what do you do? One option is to store someÂ
of that excess water so that it can keep the  pumps running and the taps flowing during theÂ
dry times. But, the amount of storage matters. A clearwell at a water treatment plant or anÂ
elevated water tower usually holds roughly  one day’s worth of supply. Those types ofÂ
tanks are meant to smooth out variability  in demands over the course of a day (and I haveÂ
a video on that topic), but they can’t do much  for the reliability of a water source. If theÂ
river dries up for more than one day at a time,  a water tower won’t do much good. For that, youÂ
need to increase your storage capacity by an  order of magnitude (or two). That’s why we buildÂ
dams to create reservoirs that, in some cases,  hold trillions of gallons or tens of trillions ofÂ
liters at a time, incredible (almost unimaginable)Â Â volumes. You could never build a tank to holdÂ
so much liquid, but creating an impoundment  across a river valley allows the water toÂ
fill the landscape like a bathtub. Dams take  advantage of mother nature’s topography to formÂ
simple yet monumental water storage facilities. Let’s put a small reservoir on your city’s riverÂ
and see how that changes the reliability of your  supply. If the reservoir is small, it staysÂ
full for most of the year. Any water that  isn’t stored simply flows downstreamÂ
as if the reservoir wasn’t even there.  But, during the summer, as flowsÂ
in the river start to decrease,  the reservoir can supplement the supply by makingÂ
releases. It’s still possible that in those dry  years, you won’t have a lot of water stored forÂ
the summer, but you’ll still have more than zero,  meaning your supply has a firm yield, a safeÂ
amount of water you can promise to deliver even  under the worst conditions, roughly equal to theÂ
average flow rate over the course of a dry year. Now let’s imagine you build a bigger dam toÂ
increase the size of your reservoir so it can  hold more than just a season’s worth of supply.Â
Instead of simply making up a deficit during the  driest few months, now you can make up the deficitÂ
of one or more dry years. The firm yield of your  water source goes up even further, approaching theÂ
long-term average of river flows, and completely  eliminating the idea of a drought by convertingÂ
all those inconsistent sloshes of rain and snow  into a perfectly constant supply. Beyond this, anyÂ
increase in reservoir capacity doesn’t contribute  to yield. After all, a reservoir doesn’t createÂ
water, it just stores what’s already there. Of course, dams do more than merely store waterÂ
for cities that need a firm supply for their  citizens. They also store water for agricultureÂ
and hydropower that have more flexibility in their  demand. Reservoirs serve as a destination forÂ
recreation, driving massive tourism economies.  Some reservoirs are built simply to provideÂ
cooling water for power plants. And, many dams  are constructed larger than needed for just waterÂ
conservation so they can also absorb a large flood  event (even when the reservoir is full). EveryÂ
reservoir has operating guidelines that clarify  when and where water can be withdrawn orÂ
released and under what conditions and no  two are the same. But, I’m explainingÂ
all this to clarify one salient point:  an empty reservoir isn’t necessarily a bad thing. Dams are expensive to build. They tie up hugeÂ
amounts of public resources. They are risky  structures that must be vigilantly monitored,Â
maintained, and rehabilitated. And in many cases,  they have significant impacts on the naturalÂ
environment. Put simply, we don’t build dams  bigger than what’s needed. Empty reservoirsÂ
might create a negative public perception.  Dried up lake beds are ugly, and the “bathtubÂ
ring” around Lake Mead is a stark reminder of  water scarcity in the American Southwest. But,Â
not using the entire storage volume available can  be considered a lack of good stewardship of theÂ
dam, and that means reservoirs should be empty  sometimes. Why build it so big if you’re not goingÂ
to use the stored water during periods of drought?  Storage is the whole point of the thing…Â
except there’s one more thing to discuss: Engineers and planners don’t actually know whatÂ
the worst case scenario drought will be over the  lifetime of a reservoir. In an ideal world, weÂ
could look at thousands of years of historical  streamflow records to get a sense of how longÂ
droughts can last for a particular waterbody.  And in fact, some rivers do have stream gages thatÂ
have been diligently collecting data for more than  a century, but most don’t. So, when assessingÂ
the yield of a new water supply reservoir,  planners have to make a lot of assumptionsÂ
and use indirect sources of information.  But even if we could look at a long-termÂ
historical record as the basis of design,  there’s another problem. There’s no rule thatÂ
says the future climate on earth will look  anything like the past one, and indeed weÂ
have reason to believe that the long-term  average streamflows in many areas of the worldÂ
- along with many other direct measures of  climate - are changing. In that case, it makesÂ
sense to worry that reservoirs are going dry.  Like I said, reservoirs don’t create water, soÂ
if the total amount delivered to the watershed  through precipitation is decreasing overÂ
time, so will a reservoirs firm yield That brings me to the question of the whole video:Â
what happens when a reservoir runs out of water?  It’s a pretty complicated question, not onlyÂ
because water suppliers and distributors  are relatively independent of each other andÂ
decentralized (capable of making very different  decisions in the face of scarcity), but alsoÂ
because the effects happen over a long period  of time. Most utilities maintain long-termÂ
plans that look far into the future for both  supply and demand, allowing them to developÂ
new supplies or implement conservation measures  well before the situation becomes an emergencyÂ
for their customers. Barring major failures in  government or public administration, you’reÂ
unlikely to turn on your tap someday and  not have flowing water. In reality, waterÂ
availability is mostly an economic issue.  We don’t so much run out as we just use moreÂ
expensive ways to get it. Utilities spend  more money on infrastructure like pipelines thatÂ
bring in water from places with greater abundance,  wells that can take advantage of groundwaterÂ
resources, or even desalination plants that can  convert brackish sources or even seawaterÂ
into a freshwater source. Alternatively,  utilities might invest in advertising and variousÂ
conservation efforts to convince their customers  to use less. Either way, those costs getÂ
passed down to the ratepayers and beyond. For some, like those in cities, the higher waterÂ
prices might be worth the cost to live in a  climate that would otherwise be inhospitable. ForÂ
others, especially farmers, the increased cost of  water might offset their margins, forcing themÂ
to let fields fallow temporarily or for good.  So, while drying reservoirs might notÂ
constitute an emergency for most individuals,  the impacts trickle down toÂ
everyone through increased rates,  increased costs of food, and a whole host ofÂ
other implications. That’s why many consider  what’s happening in the American southwest toÂ
be a quote-unquote “slow moving trainwreck.” In 2019, all the states that use water fromÂ
the Colorado River signed a drought contingency  plan that involves curtailing use, startingÂ
in Arizona and Nevada. Those curtailments  will force farmers to tap into groundwaterÂ
supplies which are both expensive and limited.  Eventually, irrigated farming in ArizonaÂ
and Nevada may become a thing of the past.  There’s no question that the climateÂ
is changing in the American Southwest,  as years continue to be hotter and drier thanÂ
any time in recorded history. It can be hard to  connect cause and effect for such widespread andÂ
dramatic shifts in long-term weather patterns,  but I have one example of an empty reservoirÂ
where there’s no question about why it’s dry. In 1978, the US Army Corps of EngineersÂ
completed Optima Lake Dam across the Beaver  River in Oklahoma. The dam is an earth embankmentÂ
120 feet (or 37 meters) high and over 3 miles or  5 kilometers long. The Beaver River in OklahomaÂ
had historically averaged around 30 cubic feet  or nearly a cubic meter per second of flowÂ
and the river even had some major floods,  sending huge volumes of water downstream.Â
However, during construction of the dam,  it became clear that things were rapidly changing.Â
It turns out that most of the flows in the Beaver  River were from springs, areas where groundwaterÂ
seeps up to the surface. Over the 1960s and 70s,  pumping of groundwater for cities and agricultureÂ
reduced the level of the aquifer in this area,  slashing streamflow in the Beaver River as it did.Â
The result was that when construction was finished  on this massive earthen dam, the reservoirÂ
never filled up. Now Optima Lake Dam sits  mostly high and dry in the Oklahoma Panhandle,Â
never having reached more than 5 percent full,  as a monument to bad assumptions aboutÂ
the climate and a lesson to engineers,  water planners, and everyone about theÂ
challenges we face in a drier future. Drought seems really simple when you’re justÂ
looking at the level in a reservoir, but I hope  this video helped you appreciate the technicalÂ
complexity in developing and managing water  supply for a large area that involves hydrology,Â
geology, meteorology, climatology, and of course  a lot of civil engineering. In fact, I’ve foundÂ
through everything I do that the all the best and  most important projects combine the expertise andÂ
knowledge of lots of different fields of study.  And the way you get exposed to those differentÂ
fields isn’t by reading or watching videos.  It’s by doing the thing, coding the program, byÂ
building the project. That’s why I’m so thankful  to have Brilliant as the sponsor of today’s video.Â
Brilliant is a learning platform for science,  technology, engineering and math, that is superÂ
interactive. There are courses on logic, computer  science, math, and actually my favorite is thisÂ
one called the Physics of the Everyday that just  pulls back the scientific curtain on aspects ofÂ
the world that you only learned about in grade  school (for example, one of my favorite obsessionsÂ
- the weather). If that sounds interesting to you,  go try Brilliant yourself completely free atÂ
brilliant.org/PracticalEngineering. You don’t  pay anything to sign up, and the first 200Â
people that use the link will get 20% off an  annual premium subscription. Thank you forÂ
watching, and let me know what you think.
SS: Interesting video, but the guy never really answers the question. It really is just the Futurama meme of "we added bigger and bigger blocks of ice..."
Spend more and more money and energy trying to band-aid over the problem. But eventually the bill comes due.
there was an entire civilization in eastern iran around an inland sea that dried up after deforestation.