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World Climate Patterns 9th Grade Geography It’s a great day to be a Falcon!!! Review Write down 3 things we have discussed from class, that can effect climate. Climate Regions What is a region? Climates are organized into regions. – tropical, dry, midlatitude, high latitude, and highland. Characteristics of Tropical Climates Located in or near the low Tropical wet = tropical rain latitudes. “Think Tropiclow (sounds like Tropical).” Tropical Climates can be divided into tropical wet and tropical dry. Tropical wet: average temp 0f 80 degrees F, Rain daily. 80 in. of rain/ year. UT= 15.31 forest Largest tropical rain forest is the Amazon River basin. Tropical Dry Dry winters and wet summers. High year-round temperatures. Few trees. Think Savannas. Tropical savannas = Africa, Central and South America, Australia. Dry Climates Two types: Desert and Steppe occur in low latitudes and mid-latitudes. Desert = sparse plant life, less than 10 inches of rainfall yearly. Very hot days- Very cool nights. Dry Climate Steppe Steppes are dry, largely treeless grasslands that border deserts. Yearly rainfall in a steppe area is between 10 to 20 inches. The world’s largest steppe stretches across eastern Europe and western and central Asia. Mid-latitude Climates Include four temperate climate regions. Marine west coast climate. (Pacific coast) Cool summers, and cool damp winters. Lots of rainfall. Mediterranean: mild, rainy winters and hot, sunny summers. Humid sub-tropical climate brings short, mild winters and nearly year-round rain. Think Florida. Humid Continental climate: regions that do not experience the moderating effects of ocean winds because of their northerly continental, or inland, locations. Think Midwest (Ohio, Nebraska.) High-Latitude Climates Freezing temperatures are common throughout the year due to the lack of sunlight. Amount and variety of vegetation are limited. Permanently frozen ground or permafrost is common in this region. Arctic, Northern Canada Highland Climates High mountain areas, even along the equator, share some of the same characteristics of high latitude climates because of the thinning of the atmosphere at high altitudes. Remember every 1000 ft up we loose 3-4 degrees. Quito, Ecuador in the heart of the Andes Mt. South America