What is the climate in Uruguay?
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The climate in Uruguay is usually normal. No extreme temperatures or anything like that. Occasionally there's a lot of wind.\n\nRead more at the website cited.
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I have lived in Florida for 22 years and the warmest I've seen it get is 91 degrees F.  It is possible that it could get a degree or 2 warmer than that, but it requires the right conditions of getting it up to that temp, for example, a long period of direct heating by the sun and next to no rainfall to run off into the Gulf to lower the temp near the coast. So basically an area of High pressure dominating the weather patterns and also the proximity to a warm current such as the Gulf Loop Current, the Florida Straights which in turn becomes the Gulf Stream.
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Tropical/torrid regions--basically anything between 24 degrees north and 24 degrees south of the equator
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One of the primary explanations for why Northern Europe, including France, Germany, and the British Isles have such a mild climate in comparison to other lands at their latitude is the Gulf Stream current.\n\nThe Gulf Stream is a very strong ocean current in the Atlantic Ocean, that carries warm water from the Caribbean, northward along the North American Coast, and then eastward towards northern Europe. This warm water helps keep the weather patterns more temperate over Europe, by keeping the seas a bit warmer, helping push warmer air fronts from the south (to compete against cooler air front from the Arctic).
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south america, between chile, bolivia, paraguay, brazil, uruguay and the atlantic ocean.
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Kenya is a country about as large as France and situated in East Africa between 5°N and 5°S. It has a very diverse relief with a low coastal plain on the Indian Ocean shore, extensive inland plateaux regions between 915 m/3,000 ft and 1,500 m/5,000 ft and several mountain ranges and isolated peaks such as Mount Kenya, which rises to 5,200 m/17,000 ft and has a permanent snow-cap.\n\nIt is bordered on the north by Ethiopia and Somalia, on the south by Tanzania, and on the west by Uganda and the shores of Lake Victoria.\n\nAlthough Kenya lies athwart the equator, annual rainfall over most of the country is surprisingly low and rather variable from year to year. This is because the intertropical belt of cloud and rain passes rather quickly across Kenya in April and October and because the predominant seasonal winds, the north and south monsoons as they are called in East Africa, have a track parallel to the coast and have already passed over large areas of land before reaching Kenya.\n\nTemperatures over much of Kenya are subtropical or temperate, because of the reduction of temperature with altitude, and are similar to those in California, summer in France or southern Britain rather than those elsewhere in equatorial Africa.\n\nOnly the coastal lowlands experience the constant high temperatures and humidity associated with equatorial latitudes. Even here they are less oppressive than one might expect, because of the regular daytime sea breezes and longer hours of sunshine.\nThe variety of relief and the range of altitude in Kenya produce a considerable number of distinctive local climates and local weather too numerous to be detailed here. The country can be divided broadly into four climatic regions, each with certain features of equatorial climates.\n\nThere is a double rainy season between March and May and between November and December, with two intervening dry seasons. There is a small difference in temperature from month to month through the year. Both these features can be seen in the three tables for Kenya included here. The four climatic regions are:\n\nThe Coastal Region\nThe average annual rainfall is over 1,000 mm/40 in, except in the north where it is rather less. The wettest months are April and May as the intertropical rain-belt moves north. The second rainy season in October and November, sometimes called the 'little rains' in Kenya, is less conspicuous. Some rain, often in the form of night or early morning showers, occurs in all months.\n\nTemperatures remain quite high around the year as does humidity; but the weather is less oppressive than might be thought because of the regular and strong onshore winds in the daytime and the greater number of sunshine hours which average seven to eight a day in all months. The weather, however, can feel sultry, particularly at night.\nThe Northern Frontier Districts and the Lower Inland Plateau\nMuch of this region has a very low annual rainfall for an equatorial region. Rainfall is generally below 500 mm/20 in and in the far north is often below 250 mm/10 in.\n\nIn the lower districts temperatures are high round the year, there is much sunshine, and the region is a typical hot desert like the adjoining southern parts of Somalia and Ethiopia. Humidity is low and, apart from occasional excessive heat, it is a healthy climate.\n\nThe Kenya Highlands\nMost of this region lies between 1,220 m/4,000 ft and 2,150 m/7,000 ft and occupies the centre and west of the country on either side of the eastern Rift valley, extending to the Ugandan border. It is the most densely populated part of the country and contains the most productive agricultural land.\n\nThere is a double rainy season but rainfall is moderate and only exceeds 1,250 mm/50 in a year on the higher parts. Over most of the region the sunniest time of the year is from December to March. The cloudiest period is from June to September when there is much drizzle but little heavy rain. This period is often called &#
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Wiki to the rescue:\n\n"The climate of Alabama is best described as being a humid subtropical climate. This is especially true in the southern part of the state with its close proximity to the Gulf of Mexico, while the Northern parts of the state, especially in the Appalachian Mountains in the Northeast, tend to be much closer to a Continental climate. Generally, Alabama has very hot summers and mild winters with copious precipitation throughout the year. March is typically the wettest month and October is the driest month."\n\nMore info at this link:
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www.ineedajobandgirlinthis climate.com
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average temperature in the winter is around -72f.  lowest temperature recorded is -129f.  it can feel a lot colder than its actual temperature, because antarctica is not only the coldest, but also the windiest in the world on average.
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Uruguay..... 4 - 2 over Argentina
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Uruguay, 1st Worldcup which they won..
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the typical food in Uruguay is :\nroasted meat \nchicken \npastes \nroasted pig\netc
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http://www.bom.gov.au/climate/dwo/IDCJDW0300.shtml\n\nfind your city, then pick may 06
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Temperature differential between warmer, sunlight parts of the earth and colder, darker parts of the earth.
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1) What do you mean by "a climate graph"? Rainfall, temperature, air pressure, evaporative demand, humidity, cloud cover, incident radiation and a million other variables all combine to make up climate. You can't have graph that shows them all.\n\n2) Have you tried simply putting [canungra climate] or [ Lamington National Park climate] into Google? That seems to provide a hell of a lot of information without expecting to be spoon fed.
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In geography, temperate latitudes of the globe lie between the tropics and the polar circles. The changes in these regions between summer and winter are generally subtle, warm or cool, rather than extreme, burning hot or freezing cold. However, a temperate climate can have very unpredictable weather. One day it may be sunny, the next it may be raining, and after that it may be cloudy. These erratic weather patterns occur in summer as well as winter.\n\nThe north temperate zone extends from the Tropic of Cancer at about 23.5 degrees north latitude to the Arctic Circle at about 66.5 degrees north latitude. The south temperate zone extends from the Tropic of Capricorn at about 23.5 degrees south latitude to the Antarctic Circle at about 66.5 degrees south latitude.\n\nWithin these borders there are many individual climate types, which are generally grouped into two categories: continental and maritime.\n\nThe maritime climate is clearly affected by the oceans, which help to sustain somewhat stable temperatures throughout the year. In the temperate zones, the prevailing winds are to the west, the western edge of temperate continents most commonly experience this maritime climate. Such regions include Western Europe, especially the UK, and western North America at latitudes between 40° and 60° north (65°N in Europe).\n\nThe continental climate is usually situated inland, with warmer summers and colder winters. The large land mass increases its effects on heat reception and loss. In North America, the Rocky Mountains act as a climate barrier to the maritime air blowing from the west, creating a continental climate to the east. In Europe, the maritime climate is able to stabilize temperatures further inland, because the major mountain range - the Alps - is oriented east-west.
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Channel Islands \nHeadline\nSunny periods. \n\nRest of today\nSunny periods. Feeling cooler with a moderate westerly wind. Maximum temperature 17 deg C (63 deg F). \n\nTonight\nTurning misty overnight with fog patches. Light westerly breeze. Minimum temperature 9 deg C (48 deg F). \n\nOutlook for Sunday\nFine with some sunshine.