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EUROPEAN WEATHER

Most of Europe has a relatively mild climate which is largely due to its oceanic exposure to the north, west, and south. The east-west orien-tation of the mountains in Europe normally prevents extremely cold arctic air from penetrating southward to the Mediterranean. As a result, very cold weather is limited to the northern limits. The southern coast and Mediterranean countries enjoy moderate temperatures year round because relatively warm maritime air masses move inland from the Atlantic and because of the moderating influence of the Mediterranean Sea. However, this inflow of maritime air also brings frequent cloudiness, considerable precipitation, and high humidity.

When continental air masses dominate, Europe is subjected to low-temperature extremes, low humidity, and clear skies much the same as North America. This is especially true north of the Alpine Mountains. South of this region, somewhat normal migratory patterns do exist. The end result is relatively dry summers and wet winters characteristic of the western coastal region of North America and Canada. Temperatures are highest in Europe during the summer; Athens, Greece averages 80F; Granada, Spain 77F; Greenwich, England 63F; and Paris, France 65F Farther north, summer temperatures average as much as 20 to 25 degrees less. During the winter, the Medi-terranean temperatures average in the upper 40F to low 50F range while the extreme northern sections average 10F or less. The Atlantic coastal countries with their predominantly maritime climates maintain far less temperature extremes between summer and winter. Precipitation in the form of rain and drizzle is common along the European Atlantic coast and near the Mediterranean Sea. Snow does occur at times in areas east of Spain and north of the Mediterranean Sea. At higher elevations inland, snow is common and frequently abundant. Central Spain and southern Russia, by contrast, experience semiarid and arid climates.

ASIATIC WEATHER

Asias climate is predominantly continental. The only exceptions are the heavily populated coastal areas that have tropical and maritime climates during the summer. This primarily con-tinental climate results in limited precipitation and large temperature ranges both daily and seasonally.

Asia is a huge continent with large expanses of land extending far northward. The Himalaya Mountains stretch across the southern portion in an east-west direction; mountains also parallel the eastern coast. These geographical features often contain continental arctic and polar air inland, resulting in the most extreme temperature ranges found in the Northern Hemisphere. Northeastern Siberias temperatures often range from 60F in the winter to above 60F in the summer. Extremes range as high as 98F and as low as 90F. The large interior of Asia also results in extreme pressure difference. In the winter the con-tinent is dominated by a cold high-pressure area and in the summer by a warm low-pressure area. This accounts for the northeast winter monsoons and southwest summer monsoons.

In the winter the interior is dry, receiving less than 1 inch of precipitation. Coastal areas under maritime influence receive normal amounts (about 8 inches) of precipitation. In the summer, precipitation is plentiful except well inland. Rain is so abundant in some regions, such as India, that the yearly rainfall average (425 inches or more) is among the highest in the world.

The extreme south and southeast regions of Asia differ sharply from its northern neighbors. These southern regions enjoy the tropical and maritime climates that feature only minor seasonal temperature variations. Eastern Asia enjoys a climate very similar to that found along the eastern coast of North America from the Florida Keys to eastern Canada. East and southeast Asia, like the eastern and southeastern United States, is also subject to an occasional tropical cyclone (typhoon) in the summer and in the fall.

SOUTH AMERICAN WEATHER

South America has a variety of climates but lacks the severe weather of North America. Con-tinental polar air does not exist here because the continent tapers sharply from north to south. The larger northern area is close to the equator and does not experience the influx of cold maritime polar air from the south. Tropical climates prevail over much of the continent. Yet, due to the high Andes Mountains along the western coast, there are areas that are extremely dry and others that are extremely wet.

Northeastern Climate

The South American northeasts climate con-sists mainly of high temperature and humidity and copious rainfall throughout the year. September is the warmest month with average temperatures of around 82F. January is the coolest month with average temperatures of around 79F. Nighttime temperatures rarely fall below 65F. Rainfall averages 87 inches annually with 12 inches falling in June and just over 2 inches falling in October. The higher elevations of northeastern South America have greater ranges of temperature, humidity, and precipitation; however, these ranges are not extreme.

Southern Climate

In the southern region, below 20 south latitude, South America has distinct seasons very similar to those in the southeastern United States. These seasons, however, are reversed. The warmest month is January, which averages 74F; July, which averages 49F is the coolest month. Precipitation occurs fairly evenly throughout the year and averages 38 inches. There is no distinct rainy season.

Below 40 south latitude, the climate is pro-gressively drier and cooler. However, the extreme southern tip of South America is characterized by year round cold and damp climate due to a strong maritime influence.

West Coast Climate

The west coast, from northern Peru to the middle of Chile, is a desert. North and south of this desert midsection, the climate is quite humid. The northwest coast has atypical tropical climate with wet and dry seasons, Below central Chile, the climate again shows atypical Southern Hemisphere seasonal reversal of that found in North America. The weather in this region is similar to that found along the northwest coast of North America. The climate is generally rainy and cool. Summer does not seem to exist as we know it. Yet, winter temperatures average above freezing.

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