Climatic types and their causes are four types of climate in the tropics: 1. Tropical rainforest climate: distribution patterns: causes between latitudes of 10 degrees north and south: distribution areas controlled by equatorial low-pressure bands over the years: the amazon basin, congo basin, indonesia: high temperatures, low annual temperature, small temperatures: 16-30 mm and above precipitation: 2,000 mm vegetation: tropical rainforest animals: chimps, hippotypical soil: brickshaw, 2 tropical monsoon climate: distribution patterns: eastern coast of the continent between latitudes of 10 degrees north and south and the regression line: wind belt, air-pressure zone seasonal movement and variation in the heat properties of the sea and surface: indian peninsula, central south peninsula (the country's grand cloud and south-east corner of tibet) characteristics: high temperature, two dry wet seasons: 16° to 30° precipitation: 1,500 mm to 2000 mm vegetation: tropical monsoon rainforests: elephants, peacock soil: red edge (brick red border), tropical grassland climate: patterns: north-south latitude 10° to north-south return routes due to the equatorial low-pressure belt and wind-control areas: central africa, brazil, large part of south america, northern and eastern australia: annual high temperature, dry wet season alternate control temperature: 16°-30° precipitation: 750mm-100mm vegetation: tropical savannah soil: long savannah, antelope soil: dry red earth 4, tropical desert climate: distribution pattern: north-south regression to 30° continental internal and western factors: distribution areas controlled by subtropical high-pressure belts: characteristics of northern africa, the asian arabian peninsula and the australian desert: high temperature and low rainfall: 16°-30° precipitation: around 100 mm vegetation: desert fauna: kangaroo, desert fox, single-capper soils: three types of desert subtropical area: 1: subtropical monsoon climate: pattern: cause of subtropical continent's east coast: differences in the distribution of heat properties by sea and land: our eastern qinjing - south of the wye river, south-east of the north american continent, eastern and south-eastern australians: high summer temperatures, warm and low winter temperatures: 0 degrees-30 degrees precipitation: more than 1,000 mm vegetation: subtropical green forest fauna: haemorrhages, leopards: red border, mediterranean climate: distribution patterns: west bank causes of 30 degrees to 40 degrees north and south: subtropical high-pressure belts and western wind belts are controlled areas: mediterranean coast, north and south american latitudes 30 degrees to 40 degrees west bank, australian and continent: hot and south-west african continent: hot and dry in the north-south pacific ocean: long and cold in the south of japan: far east, 30 mm vegetation: green and transient, long east of japan: long east: long, long, long, long, long, long, long, long, long, long, long, long, long, temperature-leaved broad-leaved forest animals: squirrels, black bear soils: brown lobe, brown soil 2, temperate marine climate: distribution patterns: western continental cause of 40-60 degrees latitude north-south: west wind zone controlled distribution throughout the year: western europe, north america and the west bank of south america feature: winter mildness, summer coolness, annual wet temperature: 0-30 degrees precipitation: 700 mm-1,000 mm vegetation: temperature-leaved forest animals: squirrels, black bear soils: brown lobe, brown soil 3, temperate continental climate: distribution patterns: internal causes in the continent at latitudes 40-60: deep in the interior of the continent: within asia and europe, the interior of the continent is characterized by hot summers, cold winters and low precipitation, with a slight concentration on summer temperatures: minimum temperature 0 degrees to decrease water: vegetation below 200 mm: grasslands, desert black calcium soil (temperate grasslands) - animals: yellow sheep, dry otter deserts (temperature desert belts) - animals: double camels, midday sand rats。
