If the temperatures are increasing in a mountainous region, in order to be sure in that, the evidence can simply be obtained by the vegetation. The mountains tend to be warmer at the lower parts, and as the elevation increases, the temperature decreases. If it is a higher mountain, then we will see that there is certain type of vegetation in the lower parts, above it a belt of another vegetation type, above that one there's usually a belt of grasses, and the highest parts are usually with little to no vegetation. If the temperature increases though, then the vegetation from the bottom will start moving upwards, occupying larger portion, the second layer will move upwards as well, and the grasses will come around the top part of the mountain, with the barren part disappearing from the scene.
20 meters walk south is the <u>short leg</u>. The long leg is 30 meters walk east. Distance from 30 meters east to starting point is a hypotenuse.
Answer:
Heat Islands occur in cities.
Explanation:
The cities, especially the large ones, have managed to totally transform the natural landscape and create something that can not be found in nature. Humans have created large areas with very large populations. This has resulted in the extensive building, pilling up of certain materials, industry, traffic, blocking of winds, pollution, etc.
All of the aforementioned things have managed to create a micro-climate when it comes to the cities, differing from the climate in the surrounding area. Something that is often a characterisitc of the micro-climate in the large cities is the so-called ''heat island''. Basically, the materials that dominate in the cities, like concrete, asphalt, and glass, all manage to amplify the effect of the sun, accumulating and radiating heat, making the cities unbearably hot in some parts of the year.
The warm waters of the north atlantic drift<span> are responsible for modifying the atmospheric conditions </span><span>of western e</span>urope<span>, so that winters are not as cold as they would be at its latitude</span>
Answer: After the hurricane, Galveston raised the elevation of many new buildings by more than 10 feet (3 meters). The city also built an extensive seawall to act as a buffer against future storms. Despite the reconstruction, the city's status as the premier shipping port was lost to Houston a few years after the disaster. Ike, however, is projected to head west on a path that will take it close to Hispaniola, Cuba, and the Florida Straits.”
Explanation:
