ters, warm summers

Monaco
Mediterranean with mild, wet winters and hot, dry summers

Mongolia
desert; continental (large daily and seasonal temperature
ranges)

Montenegro
Mediterranean climate, hot dry summers and autumns and
relatively cold winters with heavy snowfalls inland

Montserrat
tropical; little daily or seasonal temperature variation

Morocco
Mediterranean, becoming more extreme in the interior

Mozambique
tropical to subtropical

Namibia
desert; hot, dry; rainfall sparse and erratic

Nauru
tropical with a monsoonal pattern; rainy season (November to
February)

Navassa Island
marine, tropical

Nepal
varies from cool summers and severe winters in north to
subtropical summers and mild winters in south

Netherlands
temperate; marine; cool summers and mild winters

Netherlands Antilles
tropical; ameliorated by northeast trade winds

New Caledonia
tropical; modified by southeast trade winds; hot, humid

New Zealand
temperate with sharp regional contrasts

Nicaragua
tropical in lowlands, cooler in highlands

Niger
desert; mostly hot, dry, dusty; tropical in extreme south

Nigeria
varies; equatorial in south, tropical in center, arid in
north

Niue
tropical; modified by southeast trade winds

Norfolk Island
subtropical; mild, little seasonal temperature
variation

Northern Mariana Islands
tropical marine; moderated by northeast
trade winds, little seasonal temperature variation; dry season
December to June, rainy season July to October

Norway
temperate along coast, modified by North Atlantic Current;
colder interior with increased precipitation and colder summers;
rainy year-round on west coast

Oman
dry desert; hot, humid along coast; hot, dry interior; strong
southwest summer monsoon (May to September) in far south

Pacific Ocean
planetary air pressure systems and resultant wind
patterns exhibit remarkable uniformity in the south and east; trade
winds and westerly winds are well-developed patterns, modified by
seasonal fluctuations; tropical cyclones (hurricanes) may form south
of Mexico from June to October and affect Mexico and Central
America; continental influences cause climatic uniformity to be much
less pronounced in the eastern and western regions at the same
latitude in the North Pacific Ocean; the western Pacific is
monsoonal - a rainy season occurs during the summer m