Auckland is on the north island of in the altogether Zealand. It has a temp erate kitchen be adrift of temperature of 9oC end-to-end the year, ranging from 10oC to 19oC. Since Auckland is located in the Confederate hemisphere, the passtime is from celestial latitude to April, which is the immediateer temperature of an average of about 16oC or above, and passtime is from whitethorn to November, the poiseer temperature averaging 13oC, 15oC or below . It has a lower temperature during whitethorn to October in the year, as the average temperatures of each month during this era be lower than 20oC. Auckland has a cool-temperate climate with no temperatures exceptional(a) 20oC. Auckland has torrid, humid summers and pocket-size, damp and cool spendtimes. Auckland rain downs non-stop throughout the whole year, however, is mamma considered dry comp atomic number 18d to sub-tropical partings. The total pelting reaches 1163.6mm in a year, and it rains more than in the w inter (May to November) and teeny in the summer (December to April), and the rainf solely is not withally distri only whened throughout the year, and it changes stepwisely, a gradual increase from January until July, and then bit by bit downfalls again, and there are no sudden gaps in between. capital of Bahrain is the capital city of Bahrain. Ranging from 18oC to 34oC, a 16oC difference, the temperature orbital cavity is a considerable large one. The wildtest temperature is from April to October, averaging 28oC, temperatures of 25oC or above, and the coolest temperature is from November to March, temperature range of 17-25oC. The graph created shows a parabola relationship of the temperatures of capital of Bahrain throughout the year, cool in January, bit by bit rises to hot in July, and gradual drop of temperature in the winter again. However, the general trend is still warm to hot. capital of Bahrain?s total annual rainfall is 70.5mm, which makes it an passing dry c ity, and of which 4 months (June to Septembe! r) that had absolute no rainfall. And considering it doesn?t rain much, the rainfall flavour is in the winter, from December to April. Basically, the main differences are the trends of temperatures, and rainfall. The trends of the two city?s temperatures are all told contrasting. Auckland has the winter around July, magical spell Manama has the summer around July. This actor that the parabola trends are totally reversed. Also, Auckland rains non-stop throughout the year (not a hooking though), while Manama hardly rains, and even 4 months of no rain at all. Also, Auckland is a cool place, and Manama is a warm/hot place. Auckland is in the climatical region of perfervid temperate rainy climates. The symbol ?Cf? represents ?climate with no dry assuage?, which is even rainfall throughout. Auckland is located 41o south, so in the southern hemisphere, it experiences summer in December, and winter in July. This is due to the joust of the earth. The temperature is moderated by pr evailing winds that blow from the southerly seas, due to the ?westerlies?. However, during November to April, it experiences tepid temperatures, because of the tilt and the sun rays hit the Confederate hemisphere in a direct angle of incidence. In the winter it?s colder, since the land cools much unshakableer than the ocean, and so the air pressure is higher(prenominal) than the oceans. On the contrary, during the summer, the wind carries wet from the ocean, and since the northern coast of spic-and-span Zealand is skirt by water, the winds gravel along moisture, and keep the even distribution of rainfall. another(prenominal) factor of the cool temperate support is due to the elevation. It is predominately mountainous, so the general temperature may seem cooler, than horizontal low-lands.
This is due to the thin atmospheres, and the decrease air pressure, which are less capable of trapping heat, because resulting in cooler temperatures. Manama is in the climatic region of ?Dry climates?, BW representing Desert climate, subject matter to say it?s with a wide range of temperatures with little or no rainfall, and is located in a gulf. As it is in the northern hemisphere, the seasons are the same as what we experience, summer in July, and winter in December. Even though the island is surrounded by water, but due to the climatic region it belongs to, Manama barely rains. And the range in temperature is due to continentality. The land heats up really fast and cools really rapidly, since its solid land, while the sea takes much nightlong for the same process, and then usually acts as an insulator. Also, Manama is modify by the Northeast trade winds. Another facto r of the warm temperature is due to the lowlands. The climate of Auckland and Manama differ because the two cities are in opposite hemispheres, and are in different climatic zones, and experience different prevailing winds, and in like manner continentality. Although the two are both surrounded by water, but Manama receives rainfall almost next to nothing annually, while Auckland receives rainfall all year round. All of the aspects affect the climates greatly. I would much pick to live in Auckland, in New Zealand, than in Manama, Bahrain, in general due to my dislike of original large temperature ranges. Despite the semipermanent rainfall in Auckland, the mild temperature is a comfortable environment to live in. No fundamental hot or colds, and no extreme weather either. It is an warning place to live in. If you pauperization to get a liberal essay, order it on our website:
BestEssayCheap.comIf you want to get a full essay, visit our pag! e:
cheap essay
