Examples of Hot Desert Biomes are the Sahara Desert covering most of South Africa, one country being Sudan, and the Namib Desert in Namibia. Climate: When looking at the climate of the Hot Desert Biome, we have to look at the temperature and the precipitation of the Biome.The temperature of the Hot Desert Biome is on average 30 degrees Celsius- 50 degrees Celsius during the day.High temperatures are due to the desert’s location being close to the equator. Therefore the sun shines almost directly overhead, having a short distance to travel to earth.The temperature of the Hot Desert Biome is 5 degrees Celsius at night. This time is known as the “Winter of the Desert”.The reason for the drastic temperature change is due to cloud cover. There is a lack of cloud cover in Deserts.
Chile, known as republic of Chile is a long narrow coastal strip located along the western coast of South America, bordering Pacific Ocean between the Andes Mountains. It borders Peru to the north, Bolivia to the northeast and Argentina to the east. Chile capital city, Santiago, is located in the central region and compose the political, cultural, and economic center of the country. Geography and Environment The country composes of three distinct natural regions – the Andres, the central lowlands, and the Coast Ranges. Chile is located along an active zone in the earth’s crust and experiences numerous earthquakes.
California has a very hot climate and so tropical storms are extremely rare in the state. Volcanoes occur in both the Philippines and California. The most famous of recent times in the Philippines was the Mount Pinatubo eruption in 1991.
The tropical climate is characterized by constant high temperatures. All twelve months have an average precipitation of at least 60 mm (2.4 in), whereas in the savanna climate, the annual precipitation is contrastingly 25 mm. In the dry climates (group B) contains: arid and semiarid climates. Desert regions on the West coast are much cooler, due to the nearby presence of cold ocean currents and frequent cloud cover. The mesothermal climate (group C) consists: mediterranean, humid-subtropic, and oceanic climates.
Where are the Andes? The Andes Mountains are the longest and one of the highest mountain ranges in the world. They are located in South America and stretch 4,500 miles from north to south, along the west coast of the continent. - What is the landscape like? The landscape is very mountainous and quite bare however it does have a lot of snow at the peaks and high altitudes.
Cultural Analysis of Peru Peru is a Country in central South America bounded on the north by Ecuador and Colombia, on the east by Brazil and Bolivia, on the south by Chile, and on the west by the Pacific Ocean. The climate of Peru varies widely, ranging from tropical in the mountain to arctic in the highest mountains of the Andes. Average temperature decrease about 1.7 Celsius (about 7 Fahrenheit degrees) the peaks are permanently covered by snow and ice. The area of Peru, including several offshore islands, is 1,285,216 sq km (496,225 sq mi), making it third in size (after Brazil and Argentina) of South America countries. Lima is the country’s capital and chief commercial center.
Washington Earthquake Risks Earthquakes can strike any location at any time. But history shows they occur in the same general patterns year after year, mainly in three large zones of the earth. The world's greatest earthquake belt, the circum-Pacific seismic belt, is found along the rim of the Pacific Ocean, where about 81 percent of the world's largest earthquakes occur. It has earned the nickname "Ring of Fire". The belt extends from Chile, northward along the South American coast through Central America, Mexico, the West Coast of the United States, and the southern part of Alaska, through the Aleutian Islands to Japan, the Philippine Islands, New Guinea, the island groups of the Southwest Pacific, and to New Zealand.
These three things plus the sun's heat determine where rain falls on the planet. The sun shines almost vertically on the equator year round, but it shines on the poles at a steep angle. There are two consequences. A beam of sunlight ten square feet shines on about ten square feet of Earth's surface at the equator, but it covers more than twice that area near the poles. The sun's light and heat are less concentrated at higher latitudes.
Depending where you are and what altitude you are at greatly varies in the atmosphere so it is divided into five layers: the Troposphere, Stratosphere, Mesosphere, Thermosphere, and the Exosphere. The Troposphere is the lowest layer, it extends from the ground to around 12 miles up. Also, it is the warmest being closest to the surface where air is the most dense. All weather happens in this layer because evaporated water only reaches to about 50,000 feet above sea level. At 31 miles you run into the Stratosphere.
Carbon dioxide concentrations were about five times higher than they are today and the average global temperature was 6 – 8 degrees higher than it is today. The earth’s temperature depends on the balance between energy entering and energy leaving the planet’s system. Electromagnetic radiation enters the planet’s system, and much of it is converted to infrared radiation (heat) which warms our planet, and sunlight is used by plants for photosynthesis. One has to only look at the example of the Moon to see how vital the Earth’s atmosphere is for the existence of life. The Moon has no atmosphere to block some of the sun’s rays in the day or to trap heat at night, and this is why temperatures on the Moon range from -233 degrees Celsius to 123 degrees Celsius at those respective times.