This type of climate is normally located along leeward lower east coasts of continents such as in southeast and central Argentina, Uruguay and south of Brazil, the southeast portions of East Asia, the southern United States, South Africa, and eastern Australia. Some CWA areas in southern China reported more than 80% of annual precipitation in the 5 warmest months (southwest monsoon).
They occur mostly at the western edges and coasts of the continents and are bounded by arid deserts on their equatorward sides that cause the dry season of summer, and oceanic climates to the poleward sides that are influenced by cool ocean currents and air masses that bring the rainfall of winter. The five main Mediterranean regions of the world are the Mediterranean Basin in northwestern Afro-Eurasia, coastal California in the United States, the southwest of Australia, the Western Cape of South Africa and the south and southwestern coast of Chile.
In these the temperatures remain relatively cool through most of the year, as opposed to mild and warm in the subtropics and cold in the subpolar zone. As a result of their location, these regions tend to be on the cool end of oceanic climates.
This variant of an oceanic climate is found in parts of coastal Iceland, the Fare Islands, parts of Scotland, northwestern coastal areas of Norway such as Often and reaching to 70° north on some islands, uplands near the coast of southwestern Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle, some parts of Southern Argentina and Chile (though most regions are still classified as continental subantarctic), and a few highland areas of Tasmania, and the Australian and Southern Alps / A Tritium o the Mona. This type of climate is even found in the very remote parts of the Japan Highlands in Indonesia.
In the most marine of those areas affected by this regime, temperatures above 20 °C (68 °F) are extreme weather events, even in the midst of summer. The vast majority of the world's human population resides in temperate zones, especially in the Northern Hemisphere, due to its greater mass of land.
The biggest described number in temperate region in the world is found in Southern Africa, where some 24,000 taxa (species and infra specific taxa) have been described, but the native fauna and flora of this region does not have much cultural importance for the majority of the human population of the world that lives in Temperateness and that live in the Northern Hemisphere, only environmental importance. Farming is a large-scale practice in the temperate regions (except for boreal/subarctic regions) due to the plentiful rainfall and warm summers, because most agricultural activity occurs in the spring and summer, cold winters have a small effect on agricultural production.
Temperate regions have the majority of the world's population, which leads to large cities. One factor is the strength of the absorption rate of builds and asphalt, which is higher than natural land.
These factors have led to the average climate of cities to be warmer than surrounding areas. However, there is a gradual change from polar to tropical climates across the middle latitude temperate zones.
Normally, in the Northern Hemisphere, the northern portions of the temperate zone feature Boreal, Continental, and Oceanic climates, while the southern portions of the temperate zone are often Mediterranean and humid subtropical climates. Additionally, both temperate and tropical species can be found side by side in the far southern portions of the temperate zone (for example in central Florida), while subarctic species might be found growing in northern portions of the continental zone (for example in Northwest Europe).
Class Class Class Class D Humid continental (DFA, DA, DFB, Dub, DSA, DSB) Subarctic (AFC, DWC, Did, Did, DSC, DSD) Temperate zone | Definition of Temperate zone at Dictionary.com the part of the earth's surface lying between the tropic of Cancer and the Arctic Circle in the Northern Hemisphere or between the tropic of Capricorn and the Antarctic Circle in the Southern Hemisphere, and characterized by having a climate that is warm in the summer, cold in the winter, and moderate in the spring and fall.
Either of two regions of the Earth of intermediate latitude, the North Temperate Zone, between the Arctic Circle and the Tropic of Cancer, or the South Temperate Zone, between the Antarctic Circle and the Tropic of Capricorn. The American Heritage® Science Dictionary Copyright © 2011.
Latitude is the main factor in classifying zones because it correlates to the amount of sunlight an area receives. Wladimir Köppen has identified and defined the various climate zones of Earth.
Latitude, elevation and the presence of nearby mountains or large water bodies help to determine the climate zone. The temperate zone mainly lies between the tropics and the Polar Regions.
It experiences a wide range of temperatures and precipitation where four distinct seasons are common. Every continent but except Antarctica has at least a small portion of land in the temperate zone.
Regions that are covered exclusively in the temperate zone include the continental U.S., most of Canada and Europe, Central Asia, southern South America, and southern Australia. It's generally having has four different seasons such as spring, summer, autumn, and winter.
The ability to grow a large variety of crops and fruit is a major source of income in these regions. Pears, apples, strawberries and other soft fruit are grown to consume as well as sell.
Britain is a good and balanced example as a country with a maritime temperate climate. This is due to the fact that the sea has a moderating effect, which keeps the land cooler in summer and warmer in winter.
Rain often comes in the form of storms that develop in the North Atlantic and blow across Britain from west to east at all times of the year. Even in such small Island weather and up to some extent the climate, differs from north to south and east to west.
Mountainous areas get much more rain than the lowlands and this has a large effect on what can be grown. Lowland areas generally tend to be warmer and more suitable for large-scale agriculture.
China has a vast territory, and it has more than one type of climate due to different geographical zones. Some good examples are Mexico City (2,250 m above sea level), Bogotá, Colombia (2,650 m) and Addis Ababa, Ethiopia (2,350 m).
Looking closely at the biome map below, you'll see that the temperate deciduous forests are located primarily in the eastern half of the United States, Canada, Europe, parts of Russia, China, and Japan. In the two temperate zones, consisting of the tepid latitudes, the Sun is never directly overhead, and the climate is mild, generally ranging from warm to cool.
The basis of this division is variations in climate, vegetation, air pressure and the average temperature. These mixed forests are located in the eastern United States, Central Europe, and northeast Asia (including northeast China, Korea and Japan), making up the majority of the temperate forest biome.
With its warm and gentle trade winds, mild temperatures and sunny skies, Hawaii is an ideal vacation destination throughout the year. Generally speaking, the state of Hawaii is tropical, but the temperature and climate can vary dramatically depending on where you are located on a particular island.
The region from the southern Plains, to the lower Midwest, eastward to the central East Coast (the New York City/coastal Connecticut region southward to Virginia) has a temperate climate with cool to cold winters and hot, humid summers. India's climate can be classified as a hot tropical country, except the northern states of Himachal Pradesh and Jammy & Kashmir in the north and Sikkim in the northeastern hills, which have a cooler, more continental influenced climate.
Global climates are often divided into five types: tropical, dry, temperate, cold and polar. These climate divisions take a variety of factors into consideration, including altitude, pressure, wind patterns, latitude and geographical characteristics, such as mountains and oceans.
These regions may be generally supposed to have temperate, or mild, climates without extremes of temperature; however, the definition is of very limited use regarding weather. Temperature and rainfall are strongly influenced by factors other than latitude, such as topography and nearness to the ocean.
As a result, extreme temperatures can occur within a temperate zone, and some areas outside them have mild climates. Within this type, there are further subdivisions, relating to the seasonal distribution of rainfall and temperatures, and indicated by lower case letters.
As relatively warm, moist air from the ocean flows inland, it may be forced to rise by a range of mountains. Conversely, in summer, they are slow to heat up, and so the effect of a large body of relatively cool water tends to prevent very high temperatures in areas near the coast.
At the same time, the region experiences fairly hot summers, allowing it to meet the temperature range requirement for this zone. There are no true continental temperate zones in the Southern Hemisphere because there are no masses of land large enough allow such temperature swings.
This region experiences cyclonic rainfall, often as much as five to ten times greater than a continental zone. Global Distribution Surprisingly little land mass falls within the southern temperate zone.