Search results
Results from the WOW.Com Content Network
The thermal equator (also known as "the heat equator") is a belt encircling Earth, defined by the set of locations having the highest mean annual temperature at each longitude around the globe.
The equator is the circle of latitude that divides Earth into the Northern and ... which are created by shifting hot spots under Earth's crust as the axis and ...
The climate of Ecuador is generally tropical and varies with altitude and region, due to differences in elevation and, to a degree, in proximity to the equator. [1] [2] Ecuador map of Köppen climate classification. The coastal lowlands in the western part of Ecuador are typically warm with temperatures in the region of 25 °C (77 °F). [3]
At the equator (0° latitude), on the equinoxes, the sun angle is always 90° no matter the axial tilt, while on the solstices the minimum sun angle is equal to 90° minus the tilt. Therefore, greater tilt means a lower minimum for the same maximum: less total annual surface insolation at the equator.
The Köppen climate classification is the most widely used climate classification system. [2] It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). [3]
Both philosophers theorized the Earth divided into three types of climatic zones based on their distance from the equator. Like Parmeneides, thinking that the area near the equator was too hot for habitation, Aristotle dubbed the region around the equator (from 23.5° N to 23.5° S) the "Torrid Zone."
You’re so hot, you make the equator look like the North Pole. Do you believe in love at first sight, or should I walk by again? If being sexy was a crime, you’d be guilty as charged.
The Hadley cell is a closed circulation loop which begins at the equator. There, moist air is warmed by the Earth's surface, decreases in density and rises. A similar air mass rising on the other side of the equator forces those rising air masses to move poleward. The rising air creates a low pressure zone near the equator.