Europe
Europe Geography & Climate
Geography
Europe has no single defining landform — it's better understood as a set of bands running roughly north to south. The North European Plain, the continent's most densely populated region, stretches from western France through Germany and Poland into Russia, with little elevation change across enormous distances. South of it, a belt of central uplands rises into the Alps, Europe's highest and most extensive mountain range, running through France, Switzerland, Italy, and Austria, with the Pyrenees forming a second, smaller barrier between France and Spain.
To the north, the Scandinavian Peninsula is shaped by glaciation rather than tectonics — fjords, thin soils, and exposed granite rather than plains. To the east, the Ural Mountains are the conventional line where Europe is considered to end and Asia begins — a political and cultural boundary more than a dramatic physical one.
Water shapes Europe as much as elevation does. The Rhine and Danube are the continent's two major rivers, both historically central to trade and settlement, and Europe's coastline is unusually long relative to its land area — few points on the continent sit far from the sea, which has shaped everything from climate to where its major cities were built.
An indented continent
Europe has more coastline relative to its area than any other continent, because it is made largely of peninsulas hanging off a landmass: Iberia, Italy, the Balkans, Scandinavia, Brittany, Jutland, and thousands of islands. Almost nowhere is more than a few hundred kilometres from salt water, and the enclosed seas — Mediterranean, Baltic, Black, North — have carried trade and armies for three thousand years. That geography is much of why Europe fragmented into so many states and why maritime powers repeatedly dominated it.
Mountains as dividers
Two ranges shape the continent. The Alps curve for around 1,200 kilometres and separate the Mediterranean world from the north, with passes that have been strategically decisive since Hannibal. The Pyrenees close off Iberia. Further east the Carpathians ring the Hungarian plain and the Caucasus marks the south-eastern limit. Between and around them lie the great plains — the North European Plain running unbroken from France to Russia, which is why that corridor has been invaded along its length so often.
Climate Patterns
Europe's climate is set less by latitude than by distance from the Atlantic. The Gulf Stream carries warm water northeast from the tropics, which is why London and Paris have far milder winters than cities at similar latitudes in North America or Asia — Western Europe's climate is maritime: mild, wet, and relatively stable year-round, with rain spread fairly evenly across the seasons rather than concentrated in one.
Moving east, that moderating effect fades. Central and Eastern Europe have a continental climate instead — colder winters, hotter summers, and a much wider gap between the two. Southern Europe, along the Mediterranean coast, follows its own pattern: hot, dry summers and mild, wetter winters, which is why the travel season there peaks opposite to what a visitor might expect from the rest of the continent.
The north is different again. Scandinavia and the Baltic states run cold and often subarctic, with short, intense summers and long winters — worth knowing if "Europe" as a single seasonal idea is doing more harm than good when planning a trip that spans more than one of these zones.
Why Europe is warmer than it should be
The continent sits at latitudes that elsewhere produce a far harsher climate: Edinburgh is north of Moscow, and Rome is level with New York. The Atlantic makes the difference. The Gulf Stream and the North Atlantic Drift carry warm surface water north-east, and the prevailing westerlies pass over it before reaching land, which keeps north-western Europe several degrees milder than comparable latitudes in North America or Asia and keeps its ports ice-free.
Three broad climates
The oceanic north-west — Ireland, Britain, the Low Countries, coastal France and Norway — is mild, damp and changeable, with small seasonal range and rain in every month. The Mediterranean south has hot dry summers and mild wet winters, which is why the vegetation is evergreen and drought-adapted. The continental east, away from the moderating ocean, has hot summers and genuinely cold winters, with the range widening the further from the Atlantic you go. Mountain climates cut across all three.