CLIMATE
The climate of the island is of an extreme Mediterranean type with very hot dry summers and relatively cold winters. Most of the rainfall is concentrated between December and January.
The climate of the coastal parts is less extreme than farther inland, due to the fact that the effect of the sea jon atmospheric humidities is always present there. The sea temperature itself never falls below 16ºC. (January and February); in August it can rise to 28 ºC.

Spring and autumn are short, typified by changeable weather, with occasional heavy storms battering the coast in spring and a westerly wind, called "meltem" carrying the influence of Atlantic depressions to this far eastern end of the Mediterranean.

From mid-May to mid-September the sun shines on a daily average of around 11 hours. Temperatures can reach 40º C. On the Mesaoria Plain, although lower on the coasts, with a north-westerly breeze called "Poyraz" prevailing. The skies are cloudless with a low humidity, 40 - 60 per cent, thus the high temperatures are easier to bear. The hot, dry, dust-laden "sirocco" wind blowing from Africa also finds its way to the island.

Short-lived stormy conditions resulting from fairly frequent small depressions prevail throughout the winter, with 60 per cent of rain falling between December and February. The Northern Range receives around 550 mm of rain per year, whereas the Mesaoria Plain receives only around 300-400 mm.

Frost and snow are almost unknown in Northern Cyprus, although night temperatures can fall to very low levels in winter.

The chief rain-bearing air currents reach the island from the south-west, so that precipitation and atmospheric humidity is at its greatest on the western and south-western sides of the Southern Range. Eastwards, precipition and humidity are reduced by the partial rain-shadow effect of the Southern Range, a similar effect is also caused by the Northern Range which cut off the humidity associated with proximity to the sea from much of the northern Mesaoria Plain. Eastwards of the Northern Range, towards the bays of the Karpaz Peninsula, where the land narrows and the effect of sea influence increases accordingly, humidity increases progressively towards the end of the peninsula.

Most of the rivers are simply winter torrents, only flowing after heavy rain, the rivers running out of the Northern and Southern Ranges rarely flowing all the year round.

During the wet winter months Cyprus is a green island. However, by the time June arrives the landscape at the lower levels assumes the brown, parched aspect which characterises its summer face. The forests and the vineyards in the mountains, plus the stips of irrigated vegatation in the valleys remain green.