| 5 things about Tropical ecosystems | |
5 things about Tropical ecosystemsThe Tropics s ã the Strip that é located between tr ó peak of cancer and Capricorn tr ó peak. É determined by the movement of the course of the earth around the Sun and the tilt ç ã the Earth's axis to the plane of the ecl í \"in which our planet moves. Could be defined as the strip of Earth in latitudinal that s ó is radiate vertically impacted (Sun Zenith) at least once a year. Geoastron. The intertropical zone presents the character í á special features clim policies that are different from the other four areas of geoastron á. Over time, the zone intertropical received several calls ç õ es, mainly the T. The name of the zone T. This é because ç ã the à lasts longest insola ç ã during full View õ es in temperate zones, so that the heat accumulated can be greater than in the intertropical zone, in which the days and nights ú last approximately the same throughout the year. And secondly, the á intertropical area contains large amount of vegeta ç ã and á é rica atmospheric water (both as the State l í liquid gas), which serves as a temperature regulator factor.The climates of the intertropical zone s ã the isotherm, thus showing varies ç õ es limited temperatures throughout the year (2-5 . However, the amplitude t é á ria é polyglandular di far greater than the annual amplitudes of monthly means and can be at é 10-15 . This scale di á ria é due to per í odo similar of day and night: Humboldt was referring to the American zone intertropical as regi õ es equinociais new continent, so that means that these regi õ es the harsh ç ã of day and night é very similar throughout the year. Because é l ó gico, if during the 12 hours of Sun (approximately) temperatures can come completely ç, along the intertropical night causes a decreases ç ã not á vel ç by temperature radiates ã the. In the intertropical zone's ã the ã the ç the precipitates and no temperature, climate element that presents the largest annual variability. In fact, because the climates of the isotherm n ã t ê ã this ç no t é polyglandular real throughout the year, s ã the espa ç and different time precipitates the ç ãthat cause different types of tropical climate. Rain the seasonality, i.e. ç ã dos distin months dry and h ú mido with xerot. In short, the character í feature clim á tica the intertropical zone's most important é its extraordinary stability á ria over time, as evidenced today by the presence of ferns of ç the á tree, very primitive plants that have no ã the ç the changing evolucion á ria main since preliminaryAccording to the õ es ç indicates the image. According to the K. S ã the climates whose annual temperature day est á é m above 18 . climate with this ç ã the drought that corresponds to the per í odo de baixo of sunlight, or savanna climate) and Am, type of climate that corresponds to a ç ã the transitions between the climate Aw and Af: Despite this ç ã the rainy season and a dry, ú last é t ã the short also allows ê of a exist forest vegeta ç ã or a ã (Af) (warm and rainy climate with vegeta ç ã of the forest). In á areas near Tropics (especially the western coasts of continents) s ã the displayed parts of climates (climates BS á ferred and BW, i. semi-desert and leaves, respectively), in ü ê of consequences. sea-temperature.com, Cuba sea temperature, Meteo France 15 jours, en.hribi.net, http://blog.achat.me | |