Highland climates are cool to cold, and are found in mountains and high plateaus. The climate of a highland area is closely related to the climate of the surrounding region. The highlands have the same seasons and wet and dry periods as the region they are in.
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Maritime climates receive high annual precipitation because they are influenced by nearby bodies of water, which evaporate moisture into the air. This moisture then falls back to the ground as precipitation. The constant interaction between the water and the air in maritime climates leads to a higher amount of rainfall throughout the year.
A climate that has warm summers and cold winters is called a continental climate.
Highland climates are cool to cold, found in mountains and high plateaus. Climates change rapidly on mountains, becoming colder the higher the altitude gets. The climate of a highland area is closely related to the climate of the surrounding biome. The major highland regions of the world (the Cascades, Sierra Nevadas, and Rockies of North America, the Andes of South America, the Himalayas and adjacent ranges and the Plateau of Tibet of Asia, the eastern highlands of Africa, and the central portions of Borneo and New Guinea) cannot be classified realistically at this scale of consideration, since the effects of altitude and relief give rise to myriad mesoclimates and microclimates. This diversity over short horizontal distances is unmappable at the continental scale. Very little of a universal nature can be written about such mountain areas except to note that, as a rough approximation, they tend to resemble cooler, wetter versions of the climates of nearby lowlands in terms of their annual temperature ranges and seasonality of precipitation. Otherwise, only the most general characteristics may be noted.
Continental climates typically have greater temperature variations between summer and winter compared to coastal climates due to their inland location and distance from moderating ocean influences. Coastal climates tend to have milder and more stable temperatures year-round due to the nearby ocean, which helps regulate the temperature by absorbing and releasing heat more slowly than land. Additionally, continental climates may experience more extreme weather events such as droughts or severe storms compared to coastal areas.
because it is big
Good question! You could go online to find nearby breeders.
it could make the weather can be different in some places or another
Smart shoppers will compare prices at all of their nearby stores.
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Croatians dress normally, much like in the States. You can compare the fashion to the nearby Italy.
I Have No Idea What So Ever?🤨🤔
Maritime climates receive high annual precipitation because they are influenced by nearby bodies of water, which evaporate moisture into the air. This moisture then falls back to the ground as precipitation. The constant interaction between the water and the air in maritime climates leads to a higher amount of rainfall throughout the year.
If you can find the respective locations on Google Earth, it will give you the elevations for both.
A climate that has warm summers and cold winters is called a continental climate.
A wild horse would seek out the best pastures with water nearby, these could be in moderate elevations in warmer months, while winters would see them on only the lowest elevations where grass can be readily uncovered from snow. Horses are foraging animals so they must travel to seek pasture and water during difficult times.
Highland climates are cool to cold, found in mountains and high plateaus. Climates change rapidly on mountains, becoming colder the higher the altitude gets. The climate of a highland area is closely related to the climate of the surrounding biome. The major highland regions of the world (the Cascades, Sierra Nevadas, and Rockies of North America, the Andes of South America, the Himalayas and adjacent ranges and the Plateau of Tibet of Asia, the eastern highlands of Africa, and the central portions of Borneo and New Guinea) cannot be classified realistically at this scale of consideration, since the effects of altitude and relief give rise to myriad mesoclimates and microclimates. This diversity over short horizontal distances is unmappable at the continental scale. Very little of a universal nature can be written about such mountain areas except to note that, as a rough approximation, they tend to resemble cooler, wetter versions of the climates of nearby lowlands in terms of their annual temperature ranges and seasonality of precipitation. Otherwise, only the most general characteristics may be noted.