What is an Equatorial climate?
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a climate similar to those found on and around the equator.
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The ocean currents are a major factor in the climate of this planet. Many regions experience weather patterns and temperatures that are related primarily to the effect of ocean currents. Other weather patterns like hurricanes and El Niño events are also strongly affected by ocean currents.\n\nOcean currents in the Northern Hemisphere circulate in clockwise patterns around the basins. These are known as gyres. The Gulf Stream which moves northward up the western side of the Atlantic Ocean basin is responsible for moderating and warming the climate of Ireland, England, and northern Europe. The equatorial currents that move westward across the Pacific Ocean are an intrinsic part of the climate patterns known as El Niño and the Southern Oscillation. This climate pattern effects North and South America, Australia, India, eastern Asia, and even parts of Africa. Even Western Europe can statistically relate flooding events to El Niño. In years when El Niño is active hurricanes in the Atlantic have been found to be less active. \nhttp://typhoon.atmos.colostate.edu/\n\nOne scientist proposed that sub sea eruptions along the East Pacific Rise might be creating large volumes of rising heated water that would periodically mess up the ocean currents and cause the changes of weather patterns associated with El Niño/Southern Oscillation events. Another scientist attempting to verify this discovered that the El Niño events actually precede swarms of seismic activity in that area, and suggested the El Niño may actually be triggering the sub sea volcanic eruptions by slight changes in sea level and water pressure over the mid-ocean ridges. \nhttp://ess.geology.ufl.edu/usra_esse/ENSO_Oceans.html\n\nAnother important ocean current circulates deep in the oceans and actually moves through each of the world’s oceans in a continuous slow-moving belt known as the Conveyor. This is driven by cold, salty, North Atlantic water that sinks and moves southward to the Antarctic, where it moves eastward into the Pacific, and then northward to the North Pacific, where it turns and moves back through the Indian Ocean and toward the North Atlantic again.  It is estimated that if the Conveyer were to shut down, the North Atlantic region would be 20 degrees F. colder within ten years, and much of Europe would have a climate more like northern Norway has today.\nhttp://www.columbia.edu/cu/record/23/11/13.html
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The tropics or the equatorial regions,   are the geographic region of the Earth centered on the equator (parallel 0) and limited in latitude by the Tropic of Cancer in the northern hemisphere, at approximately 23°26' (23.4°) N latitude, and the Tropic of Capricorn in the southern hemisphere at 23°26' (23.4°) S latitude. This region is also referred to as the tropical zone and the torrid zone.\n\nThis area includes all the areas of the Earth where the sun reaches a point directly overhead at least once during the solar year. (In the temperate zones, north of the Tropic of Cancer and south of the Tropic of Capricorn, the sun never reaches an altitude of 90° or directly overhead.) The word "tropics" comes from Greek tropos meaning "turn", because the apparent position of the Sun oscillates between the two tropics with a period that defines the average length of a year.\n\nTropical plants and animals are those species native to the tropics. Tropical is also sometimes used in a general sense for a tropical climate, a climate that is warm to hot and moist year-round, often with the sense of lush vegetation. However, there are places in the tropics that are anything but "tropical" in this sense, with even alpine tundra and snow-capped peaks, including Mauna Kea, Mt. Kilimanjaro, and the Andes as far south as the northernmost parts of Chile and Argentina. Places in the tropics which are drier with low humidity are such as the Sahara Desert and Central Africa and Northern Australian Outback.\n\nTropical ecosystems may consist of rainforests, dry deciduous forests, spiny forests, desert and other habitat types. There are often significant areas of biodiversity and species endemism present particularly in rainforests and dry deciduous forests. Some examples of important biodiversity and/or high endemism ecosystems are: Costa Rican rainforests, Madagascar dry deciduous forests, Waterberg Biosphere of South Africa and eastern Madagascar rainforests. Often the soils of tropical forests are low in nutrient content making them quite vulnerable to slash-and-burn techniques, which are sometimes an element of shifting cultivation agricultural systems-.
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The equator get more direct sunlight for longer periods of time, whereas the polar regions get a little sunlight for six months and none for six more.
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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
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Climate is the weather for a specific place over a certain amount of time and weather is what is happening outside right now.
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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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Latitude measures how far you are north or south of the equator. Latitude determines the amount of solar energy received by that region. Regions close to the equator receive direct rays of the sun and therefore receive more radiant energy and are warmer. At the areas closer to the poles, the suns rays are at an angle so these areas receive less radiant energy and are cooler.
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Hope this helps\n\nhttp://kids.earth.nasa.gov/archive/nino/intro.html
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try this\n\nhttp://en.wikipedia.org/wiki/Climate_of_India
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The climate (ancient Greek: κλίμα) is the commonly considered to be the weather averaged over a long period of time, typically 30 years. Somewhat more precisely, the concept of "climate" also includes the statistics of the weather - such as the degree of day-to-day or year-to-year variation expected. The Intergovernmental Panel on Climate Change (IPCC) glossary definition is:\n\nClimate in a narrow sense is usually defined as the “average weather”, or more rigorously, as the statistical description in terms of the mean and variability of relevant quantities over a period of time ranging from months to thousands or millions of years. The classical period is 30 years, as defined by the World Meteorological Organization (WMO). These quantities are most often surface variables such as temperature, precipitation, and wind. Climate in a wider sense is the state, including a statistical description, of the climate system.[1] \n\nWeather is an all-encompassing term used to describe all of the many and varied phenomena that can occur in the atmosphere of a planet. The term is normally taken to mean the activity of these phenomena over short periods of time, usually no more than a few days in length. Average atmospheric conditions over significantly longer periods are known as climate. Usage of the two terms often overlaps and the concepts are obviously very closely related.
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The areas north and south of the equator to 30 degrees.
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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.
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Tropical/torrid regions--basically anything between 24 degrees north and 24 degrees south of the equator
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Latitude, altitude, prevailing winds.
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do u mean el niño and la niña?\n\nthey're weather phenomena\n\nel niño is a disruption of the ocean-atmosphere system in the tropical pacific having important consequences for weather and climate around the globe\n\nla niña is associated with cooler than normal water temperatures in the equatorial pacific ocean
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www.ineedajobandgirlinthis climate.com