The world’s most famous sea.

Endless coastlines and beaches.

Histories and culture as rich as any on earth.

Blessed with one of our planet’s finest climates – it’s the only one with a dry

summer and wet winter.

But you’d be mistaken in thinking that this sea was the only place where such a climate

existed.

Copied across four other continents, this much-desired climate is home to a very famous

state, and three very different countries far into the southern hemisphere.

But in all places, this climate just has one name, the ancient home of the summer sun – the

Mediterranean.

As we continue our journey in this series from equator to poles, it’s now time to

consider the second of the three climates occupying the temperate areas of the mid-latitudes,

the Mediterranean Climate.

This climate zone has a similar temperature range to the Humid Subtropical climate that

we covered in our last episode – between 20 and 35 degrees in summer, and 5 to 20 degrees

in winter.

But the most immediate and striking aspect of this climate is in its rainfall pattern.

Most world climates have their rainfall peak in the hottest months of the year, while others

have year-round rain.

But only one reverses the most common pattern - only the Mediterranean climate has a dry

summer and wet winter.

To explain this unusual pattern, we have to consider both our earlier episodes on the

Tropical Monsoons, as well as the Hot Deserts.

You might want to view these earlier episodes to really get what’s about to follow.

Due to the 23 degree tilt of the earth, the convergence of trade winds in the tropics

called the Doldrums shifts north and south throughout the year.

The band that lies on the poleward side of this band is usually dry, due to extensive

high pressures brought on by the downward component of the Hadley Cell of tropical air

movement.

In summer, this band of high pressure is pushed further out toward the poles, away from the

Hot Deserts and into the temperate zone, causing a long drought in this season.

In winter, the Doldrums are either back at the equator or in the other hemisphere, so

the high pressure area also follows it back that way.

This allows more unstable air to return in the form of oceanic westerly winds, which,

when blown onto westward facing coasts, bring rain.

This explains why the Mediterranean climates zones lie on the western fringes of each continent.

The presence of the Mediterranean Sea at just the right latitude, allows these westerlies

to gather continual moisture as they travel east, extending the winter rain all the way

to the coasts of Lebanon and Israel at the far end of this sea.

The consistency of this climate type is well illustrated by comparing city graphs from

the west to the east of the Mediterranean.

We’ll talk more about the Westerlies in the next episode on the Oceanic climate, since

they are the dominant component of weather in those regions lying immediately poleward

to the Mediterranean areas.

Because the Mediterranean summer is uniquely drought-filled, compared to all other climates

except deserts, this peak season of heat is accompanied by low humidity – what Californians

love to call “a dry heat”.

As perspiration is more efficient in dry air, this heat is a good deal more comfortable

than, say, the humid summers of Georgia or Florida at the same latitude.

There are two subdivisions of the Mediterranean climate within the Koppen Classification system

both of which share the dry summers and wet winters just described, and differing only

by temperature range.

The first, and more common form is Csa, which experiences a hot summer of at least 22 degrees

averaged across the night-day cycle.

This is known as the Hot Summer Mediterranean.

Where the average summer temperature is below 22 degrees, this is known as the Warm Summer

Mediterranean and has the Koppen code Csb.

So where in the world do we find the Mediterranean climate?

Well, the short answer is, on every inhabited continent except Asia, which lacks the necessary

west coast.

We begin in Europe, and the sea from which this climate gains its name.

To the west of the Mediterranean, out in the Atlantic, the Azores experience warm dry summers

and wet winters.

Moving east onto the Iberian Peninsula we find the cooler Csb variant of warm summers

and very wet winters in the north of Portugal and North-Western Spain.

Further south, we move into the hot summer Csa variant that Portugal’s capital of Lisbon

experiences, along with most of Spain, and its capital Madrid.

In the extensive interior of the Iberian Peninsula, however, some areas are so dry that they are

classed as cool semi-desert – we’ll pick these up in a future episode.

The wet winters that define the Mediterranean type extend deep into Morocco on the North

African coast, and as we move east into the western Mediterranean basin, the entire Algerian

coast and northern Tunisia also fall within this climate.

All the islands in this area have this climate - the Balearics, Corsica, Sardinia, Sicily

and Malta.

The northern coast includes the luxurious Cote d’Azur of France and this coast extends

east into Italy, the heart of Mediterranean, where the dry summer / wet winter pattern

extends inland across all western and southern provinces, including the nation’s capital,

the Eternal City, Rome.

Continuing east across the Adriatic sea, much of the coast of Croatia and all of Albania

are within this climate, along with all of Greece, including its legendary capital of

Athens, and all of the Greek islands.

Now firmly into the Eastern Mediterranean basin, we reach the long coastline of Turkey,

where the wet winters and dry summers extend well inland, encompassing that country’s

largest city, the ancient metropolis of Istanbul.

Finally, at the eastern end of the Mediterranean, the coast turns south into Syria, Lebanon

and Israel, including the cities of Damascus, Beirut and Jerusalem.

In North America, the entire west coast of the United States comes under the influence

of this climate, from the coasts of Washington and Oregon in the north, with their very wet

winters – this is the largest area on Earth where we experience the warm summer Csb variant

of this climate.

As we head south into California, the winters become shorter and drier, the summers longer

and hotter, and we have the classic Csa Koppen variant.

An exception is San Francisco, which stays much cooler than the surrounding area due

to the proximity to cold ocean currents which often shroud the city in fog.

As we reach Southern California, and the massive conurbation of Greater Los Angeles, fog and

coastal cloud is less common, and summers hotter, especially as one moves further inland

away from the cool ocean.

The last stop for this climate zone are the cities of San Diego and Tijuana lying on each

side of the US/Mexico border, before the climate gives way to the hot desert of Baja.

Moving now into the Southern Hemisphere and South America, we encounter this climate in

the cooler Csb form, worlds away from its namesake, along the mid-coast of that longest

of countries, Chile.

It’s in this zone where most of that country’s population lies, including the main port of

Valparaiso, and the capital Santiago.

In Africa, south of the Namib Desert, we find the extreme south-west of South Africa caught

by the wet winter westerlies that typifies the Csa form of the Mediterranean climate,

most notably around the city of Cape Town, famous for its dramatic backdrop of Table

Mountain.

The last continent to experience this climate zone is Australia, where it brushes two parts

of the south and west facing coasts, firstly around Perth, the most isolated city in the

world, in the far west, and again, around the mid-southern city of Adelaide.

Despite its dispersal across so many continents of the globe, the Mediterranean climate is

proven as a particular and consistent type by comparing temperature and rainfall graphs

across each of these areas.

Note the 6-month switch between the northern and southern hemisphere in terms of temperature

and rainfall, demonstrating the reversal of seasons on each side of the globe.

So what kind of landscapes and vegetation do we find in the Mediterranean climate?

Throughout the world, plants have adapted to survive the drought of summer, which, occurring

at the hottest time of the year, places a particular challenge due to very high evapotranspiration

rates.

The Csa Hot Summer areas all have a similar and distinctive look – one similar to a

semi-arid desert, where shrubs form the dominant plant life separated by patches of hardy grasses,

bare earth and rock.

A distinctive hallmark of Mediterranean plants is the greyish-green appearance, a product

of the hard, waxy layer of leaves designed to hold in moisture during the hot summer

drought.

In the cooler and wetter Csb areas, shrubland gives way to forest, and it is in such areas

within California that we find the tallest trees in the world – the sequoias or redwoods.

In Australia, the Eucalyptus tree has adapted particularly well to summer droughts and is

found throughout that continent.

So successful is this family of trees in this climate that it has been exported to other

Mediterranean climate zones where it has thrived.

In terms of agriculture, the Mediterranean areas have two world famous crops.

Grapes and olives.

The drinking of wine, from the fermented juice of grapes has gone on in the Mediterranean

and Near-East since ancient times, and in the last two centuries has been exported to

all other Mediterranean climate areas, as wine drinkers will know, from seeing bottles

originating from California, Chile, South Africa and Australia.

The pressing of olives to produce olive oil has also gone on since ancient times, and

to this day the oil is valued across the world for its health properties as well as its distinctive

flavour.

Many other crops are grown in these regions, of course, particularly wheat and citrus fruits,

but these are more common in other climates than grapes and olives.

The Mediterranean climate type is an example where climate has directly had an impact on

humanity outside the world of agriculture.

In one case, the Mediterranean itself is the world’s most popular tourist area, seeing

a third of a billion visitors per year.

With its endless coastlines and historical and cultural attractions, tourists come here

in the summer knowing that they can enjoy guaranteed sunshine and warm weather.

A second example is less obvious, and that is the world movie capital of Hollywood, California.

In the early days of movie production, when film needed bright light, production companies

located to Los Angeles where for most of the year they could be guaranteed bright sunshine

and no rain that would otherwise interrupt the shooting of movies.

So there you have it, the Mediterranean climate zone.

Unique in so many ways, and if I may say, my personal favourite, having spent over a

decade living in such zones, both in Australia and California.

If you enjoyed the video, please share with your friends and subscribe to this YouTube

channel so you don’t miss future episodes.

And please leave your comments, particularly if you have experienced life in one of the

five Mediterranean climate zones around the globe.

I want to thank the many photographers and drone pilots who gave permission for their

footage to be shown this video, as well as those making their work available through

the Creative Commons.

Thanks again for watching, and I’ll see you in the next episode and the Oceanic climate

zone, where these videos are made!

I look forward to seeing you then.