Humans.
They are an interesting species aren’t they?
At the time of this production, there are estimated to be 7.7 billion of them roaming
around the surface, and that figure is still rising.
There are many reasons why people live in the places that they do.
On the coast, or along rivers, for trade.
Security in the hills, away from invaders.
Occasionally, rulers arbitrarily create new capitals in the centre of their realms.
But the main determinant for human settlement is the availability of clean, fresh water.
Because without it, crops cannot grow, livestock cannot be raised.
Without those, there is no food.
Without food, there is no population.
And what determines the availability of clean, fresh water?
Rainfall and temperature.
Too little rain, and you have a desert.
Too cold, and you have frozen ground.
Too much rain and heat, and you could have disease.
So climate and population are inextricably linked.
And if you know a bit about climate classification, then you’ve probably wondered which climate
types have the least and most populations.
Well it’s time to wonder no more, because after extensive original research and tabulation
this data is about to be presented, in this the latest video in my Climate Casebook.
If you’ve watched any of my other videos then you should be familiar with the Koppen
climate system, which breaks down the world into zones of climate types based on temperature
and rainfall patterns.
If you haven’t, then I recommend you check out my Secrets of World Climate series in
my channel, or for a quick overview, the video linked top right.
There are 29 Koppen zones in total, but I’ve grouped most of these into the twelve more
distinct categories that formed each episode in my Secrets of World Climate series.
So, let’s get right into which climate zones support what populations.
You’re probably wondering which zone has the biggest population,
but to keep you in suspense, we’re going to go in reverse order, starting with the most empty of human life.
At number twelve there are no surprises for guessing that the least populated climate
zone is the Icecap.
Since temperatures never rise above freezing, no self-sustaining settlements are possible,
and so research stations make up the “population” here.
The number of scientists varies depending on the season with summer being higher than
winter, and the vast majority of this population numbering in the thousands is in Antarctica
with typically less than one hundred on the Greenland ice sheet at any given time.
At number eleven, we have the next coldest zone – that of the Tundra.
In these bleak, treeless lands, agriculture is impossible, and any settlements here either
have to rely on supplies from outside, or on hunting wildlife.
Total tundra population worldwide is estimated to be in the hundreds of thousands – a tiny
fraction of the total human population.
These populations are scattered worldwide with about half spread along the coasts of
the Arctic and the other half concentrated in the southern tip of South America.
Some of you may take issue with the inclusion of Tierra del Fuego, since it’s not true
tundra in that it does not experience very cold winters like the arctic, and is in fact
a slightly cooler version of the Subpolar Oceanic variety where summer temperatures
rarely exceed 10°C. But it would be an omission to not mention it.
At number ten, we have the next coldest zone – the vast subarctic band that spreads across
northern North America, Europe and Asia.
Now we are getting into the millions in terms of population, but still less than a fifth
of one percent of humans live in the vast boreal forests that experience warm summers
but very cold winters here.
This population is mostly found in Russia, which is to be expected as it contains the
largest land area under this climate type, including the vast stretches of Siberia.
There are a number of Koppen subtypes in the Subarctic.
Most people live in the standard Subarctic of cold winters and year round precipitation,
with a smaller fraction in the east of Asia where only light snow falls in winter, with
more consistent rain in summer.
A much smaller fraction live in the area of very cold winters in north-east Siberia.
At number nine, and we switch from the coldest zones to one of the hottest – the year round
rain and warmth of the Tropical Rainforest.
With a global population of just over a quarter billion, we are at last into an area that
is home to a significant percentage of total human numbers.
Almost half of them live in just one country – Indonesia, with most of the others also
within SE Asia, and significantly fewer numbers in South America and Africa.
At number eight and we head to the mid-latitudes, and the western fringes of the continents
under the sway of maritime westerly winds – the Oceanic, characterised by rain year
round and relatively mild temperatures between winter and summer.
Of the two hundred and seventy million souls living in this zone, the vast majority are
within the densely populated and fertile lands of northwest Europe, with the three larger
countries there accounting for almost three quarters of the global Oceanic population.
There are two Koppen subtypes in the Oceanic – the standard and the subpolar variety,
the latter of which experiences cooler summers and is akin to a perpetual autumn.
With this description it’s perhaps not surprising that only a comparatively tiny number live
in this sub-zone.
Onto number seven now, and with just over 300 million people, we’re back in the tropics,
but this time at the cooler elevations of upland areas, providing year round spring
like temperatures.
Populations are split across all continents here, with high population countries with
significant upland areas like Ethiopia, Mexico, China and Colombia topping this list.
Koppen listed three different variants of this climate type.
Two monsoon forms separated by warm or cool temperatures which both have wet and dry seasons,
and an all year warm and wet form.
The warm monsoon form dominates in terms of population.
By the way, when you see the word “Humid” in climate classification, it is simply designating
year round rain, and is not a comment on the clamminess of air.
Up to a third of a billion now as we reach number six and the cool deserts.
In terms of population, Central Asia, with its vast continental deserts of hot summers
and cold winters, dominates, with all but two countries in this list from that area.
China’s contribution comes from its north-western dry region that is part of the central Asian
desert area, while most of Iran’s large population lies in this climate zone due to
the high elevation of that country that would otherwise have put it in the predominately
hot desert Middle East.
There are two Koppen subtypes here, the semi-arid steppe, and the true cool desert.
Since the latter is one of the harshest climates on earth, it’s no surprise that the steppe
dominates in terms of population.
At number five in our countdown toward the most populous climate zone, and we reach the
Mediterranean, and the copies of its unique dry summer rainfall pattern across most continents,
home to almost four hundred million people.
But true to form, and the actual Mediterranean dominates the population list with only the
extensive dry summer pattern of the western coast of the United States providing numbers
to counter those of the populous countries with Mediterranean shorelines.
There are two Koppen subtypes within this climate, separated by summer temperatures,
and the “classic” Mediterranean Csa hot summer type dominates in terms of population
as it does land area.
We step a gear in terms of population sizes now as we reach number four in our list, the
Continental climate.
Defined by big temperature ranges between summer and winter and plenty of rain and snow,
these regions, which occur only in North America and Eurasia, are home to almost eight hundred
million souls.
China is the largest contributor here, with its densely populated north eastern region
centred around its capital Beijing lying within the wet summer variants of this climate.
Next is Russia, where the majority of that vast country’s population is housed on the
rich and fertile plains of Eastern Europe, as Ukraine and Poland demonstrate also in
this list.
A significant chunk of the USA’s population is within this zone, and almost all of Canada’s.
There are six different Koppen types here with the classic “Humid” form of year
round precipitation and warm summers dominating population as it does land area.
Almost all of the population of the “Monsoon” types are from China, with the remainder from Korea
The dry summer variants demonstrate their rarity in this chart, making up only a tiny
fraction of the whole.
Onto number three now in our most populated climate zone list, and one of the biggest
surprises.
Close to one billion people on our planet live in hot desert or hot semi-arid conditions.
The Indian Subcontinent dominates here, with the dry region of Western India and Pakistan
being inhabited in great numbers in this generally highly populated part of the world.
Common with Pakistan and two other countries on the list – Egypt and Iraq – is the
presence of major rivers flowing through an otherwise completely barren region – the
Nile in Egypt, the Indus in Pakistan and the Tigris/Euphrates in Iraq.
These rivers provide for vast areas of irrigation, allowing huge bounties in crops in the ever-present sunshine.
Other significant populations occur across the Sahel semi-arid region immediately south
of the Sahara desert.
In terms of Koppen climate types, the true desert and semi-arid forms are fairly evenly
split in terms of population.
We’re now down to the final two - the two most populated climates on Earth.
It was actually a close call in terms of the numbers.
Both have enormous populations.
If you’ve watched my other videos you’ll have heard clues about which ones they are.
Ok, so the second most highly populated region of earth is…
The Tropical Wet and Dry zones – the Tropical Monsoon and Savannah.
Spreading out across a vast swathe of the Tropics, and encompassing such well known
populous nations as India, Indonesia, Nigeria, Bangladesh and Brazil, it’s no surprise
that this climate type is topping out in terms of population.
Two... billion… people, ladies and gentleman.
That’s over one in four of all people on our planet.
The reason for this is simple – the combination of all year round warmth and plenty of rain,
albeit in a seasonal pattern, allows for bountiful crop harvests, often multiple times per year,
feeding vast numbers.
India, with its vast population in its southern half, makes up a full quarter of the total
in this climate zone at half a billion alone.
In the Koppen classification, the Monsoon and Savannah separate out the Tropical Wet
and Dry climates, with the Monsoon being wetter with less distinct dry seasons than the Savannah.
As the Savannah accounts for more land area than the Monsoon, it makes up the majority
of population also.
And so we come to number one on our list.
The climate zone with more people in it than any other.
This is the subject of Episode 5 in my Secrets of World Climate series, when at that time
I mentioned its large populations and awarded it with the most number of major world cities
than any other.
Lying just beyond the tropics, and found on the easterly margins of every continent of
earth, it is home to a whopping 2.2 billion people.
It is defined by hot and wet summers, but comparatively cool winters…
And unless you follow climate, you’ve probably never heard of it.
It is the Humid Subtropical.
The vast population of China – almost two thirds of that country’s population are
in this zone – a billion people!
The equally vast population of India – a third of Indians live in this zone – half
a billion again.
And what about the United States?
Over half of all Americans live in this zone – that was a surprise even to me.
Almost ninety percent of Japanese live here in their overcrowded islands.
It is probably the most culturally and geographically diverse of any climate zone.
Something about this climate type allows it to support such vast populations.
With plenty of rain, either throughout the year, or during the summer, there is plenty
of water.
But unlike the tropics, the winters are cool – perhaps this is the clue – in that tropical
diseases are much less common here, allowing for healthier populations.
It is unclear.
But the population densities are higher here
than in any other zone, on practically every continent.
The two subtypes are broken down by rainfall pattern, Cfa for year round rain, and Cwa
for a summer monsoon peak.
Interestingly they both contribute near equally to the huge population numbers
at a billion each.
So, with our list complete, let’s now make a comparison of our twelve grouped zones,
in our final graphic.
This chart shows just how dominant the two largest climate types are, with over half
the people in our planet living in them.
The next quarter of our planet’s population live in the next two, while all other climate
types fill out the remaining quarter.
In some cases these differences in population score are a reflection of the relative land
areas taken up by such zones – for instance Mediterranean zones occupy a much smaller
land area than, say the Tropical Savannah.
But in other cases, such as the subarctic, it can be seen that such vast areas support
comparatively little population.
This demonstrates that the most populous regions of earth are indeed a result of climates that
offer plenty of clean, running water.
It’s not really any more complex than that.
So I hope you enjoyed this tour of Earth in respect to climate and population.
I want to specially thank Richard Torres for the many hours he spent poring over Koppen
climate maps and population tables – without his help this video would have taken a lot
longer, and with a lot more headaches for me.
Please like and share this video if you found it useful, and don’t forget to subscribe
to my channel, so you get notified about future videos.
There is now plenty of content in my channel covering aspects of climate, so feel free
to binge watch the back catalogue.
Let me know in the comments any thoughts you might have on what you’ve seen.
Thanks again for watching, and I’ll see you in the next episode of the Climate Casebook.