what are 6 factors that control climate in a region?
452179
Latitude, Ocean currents, Winds, Elevation, Relief and Nearness to water.
834058
warm arid and tropical regions
15616
Climate exists because weather is dominated by several quasi-permanent weather systems (including a high-pressure over Bermuda which oscillates and low pressures near the poles).  These weather systems do not move much (except for annual oscillations), so weather patterns will emerge from this quasi-stationary setup, and hence we have climates.
749653
try this site, sometimes you have to pay a couple bucks to get the info\n\nhttp://www.ncdc.noaa.gov/oa/climateresearch.html
137486
Clean air.\nClean water.\nShelter from the elements.\nNourishing food.\nOther people to communicate with and share the workload.
580144
well the rain shadow effect of the mountains is a biggie. air gets trapped on the eastern side of mountains, and pollution just hangs out. climate would be the fact that it is a moist climate... I am noot sure about that, but I would assume the wind patterns.... western easterlies? I would look up those terms in a high school geography book or online and go from there.
991041
Climate describes the general weather pattern for a region, and weather is specific to a time i.e. today it is raining, that is the weather but to say that New England summers are moderately warm and humid that would be the climate.
950450
Climate:\nAlthough 90% of the country is within the tropical zone, the climate of Brazil varies considerably from the mostly tropical North (the equator traverses the mouth of the Amazon) to temperate zones below the Tropic of Capricorn (23°27' S latitude), which crosses the country at the latitude of the city of São Paulo. Brazil has five climatic regions: equatorial, tropical, semiarid, highland tropical, and subtropical.\nhttp://en.wikipedia.org/wiki/Geography_of_Brazil#Climate\n\nTopography:\nBrazil covers a total area of 8,514,215 km² (3,287,357 sq. mi) which includes 8,456,510 km² (3,265,076 sq. mi) of land and 55,455 km² (21,411 sq. mi) of water. The highest point in Brazil is Pico da Neblina at 2,994 m (9,823 ft).\nhttp://en.wikipedia.org/wiki/Geography_of_Brazil\n\nNatural resources:\nBrazil is endowed with vast agricultural resources. Brazil is the world's largest producer of sugarcane and coffee, and a net exporter of cocoa, soybeans, orange juice, tobacco, forest products, and other tropical fruits and nuts.\nhttp://en.wikipedia.org/wiki/Economy_of_Brazil#Agriculture_and_forestry\nProven mineral resources are extensive. Large iron and manganese reserves are important sources of industrial raw materials and export earnings. Deposits of nickel, tin, chromite, bauxite, beryllium, copper, lead, tungsten, zinc, gold, and other minerals are exploited.\nhttp://en.wikipedia.org/wiki/Economy_of_Brazil#Industry\n\nHope this helps.\n\nAndy
586003
Air Pressure.  The humidity and such in the air is higher and therefore holds more warmth.\n\nAt higher altitudes, where the air is less dense, there is greater distance between particulates and heat is lost faster.
20345
Taken from http://en.wikipedia.org/wiki/Seasons\n\nThe ultimate cause of the seasons is the fact that the Earth's axis is not perpendicular to its orbital plane; it deviates by an angle of approximately 23.5 degrees of arc. Thus, at any given time during the summer or winter, one part of the planet is more directly exposed to the rays of the Sun. This exposure alternates as the Earth revolves in its orbit. At any given time, regardless of season, the northern and southern hemispheres experience opposite seasons.\n\nSeasonal weather fluctuations also depend on factors such as proximity to oceans or other large bodies of water, currents in those oceans, El Niño/ENSO and other oceanic cycles, and prevailing winds.\n\nIn the temperate and polar regions, seasons are marked by changes in the amount of sunlight, which in turn often cause cycles of dormancy in plants and hibernation in animals. These effects vary with latitude, and with proximity to bodies of water. For example, the South Pole is in the middle of the continent of Antarctica, and therefore a considerable distance from the moderating influence of the southern oceans. The North Pole is in the Arctic Ocean, and thus its temperature extremes are buffered by the presence of all that water. The result is that the South Pole is consistently colder during the southern winter than the North Pole during the northern winter.\n\nThe cycle of seasons in the polar and temperate zones of one hemisphere is opposite to that in the other. When it is summer in the Northern hemisphere, it is winter in the Southern hemisphere, and vice versa, and when it is spring in the Northern hemisphere it is autumn in the Southern hemisphere, and vice versa.\n\nIn the tropics, there is no noticeable change in the amount of sunlight. However, many regions (famously the northern Indian Ocean) are subject to monsoon rain and wind cycles. Curiously, a study of temperature records over the past 300 years (David Thompson, Science, April 1995) shows that the climatic seasons, and thus the seasonal year, are governed by the anomalistic year rather than the tropical year.
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Climate and Weather:\nhttp://www.gov.pe.ca/infopei/index.php3?number=856&lang=E\n\nAnything else can probably be found in the links below.
451209
Climate is more of a long-term, permanent state. For example, a rain forest climate would be wet and warm year-round. Weather is constantly changing; weather includes temporary states like rain or cloudiness. Weather is affected by winds, temperature and humidity.
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Climate is a TYPICAL WEATHER in a REGION,\nwhile\nWeather is merely the state of Atmosphere.\n\nYou can say about the climate in Australia, but if you say about the weather, it only refers to the state of atmosphere on a particular day.\n\nClimate change is when the typical weather in a region experiences changes, usually something that might bring danger. For example, global warming, in which the region becomes hotter, may cause the glaciers in the North Pole to melt.
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The dominant role of the latitudinal peak of the sea surface temperature (SST) in determining the latitudinal location of the intertropical convergence zone (ITCZ) is well-known. However, the roles of the other factors are less well-known\n These other factors include the inertial stability, the interaction between convection and surface fluxes and the interaction between convection and radiation. Since these interactions involve convection, in a model they involve the cumulus parameterization scheme. These factors are studied with a general circulation model with uniform SST and solar angle. Under such model settings the ITCZ can be a single one over the equator or a double one straddling the equator. How this outcome is determined by these factors will be described.
661859
try this\n\nhttp://en.wikipedia.org/wiki/Climate_of_India
358658
El Nino.  It really is fascinating because there are long periods where the weather has changed and caused civilizations to crumble in the past.  It kinda puts into perspective how dependent we are on our climate.\n\nhttp://www.elnino.noaa.gov/\nhttp://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/eln/home.rxml\nhttp://www.pmel.noaa.gov/tao/elnino/el-nino-story.html\nhttp://www.pmel.noaa.gov/tao/elnino/nino-home.html\nhttp://www.coaps.fsu.edu/lib/elninobib/\nhttp://www.eurekalert.org/pub_releases/2001-06/UoM-EfEN-1706101.php\nhttp://www.umaine.edu/news/Archives/2001/June01/elnino.htm
44372
most important factors are : the plan ,how to organize ,contorle & inviroments