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Moderating Effects - effect that large climate over nearby land areas. Winter temperatures are warmer and summer temperatures are warmer and summer temperatures are cooler than areas located away from large water bodies. The result is a small annual temperature range.
water temperatures change more slowly than land temperatures.
Sea breezes come from land and over the water, and happen in daytime. Land breezes come from water and over the land, and happen at night.
The heat capacity of ocean water is about four times that of air. The ocean's heat capacity is also much greater than that of land. Therefore, it takes a lot of energy to warm the oceans, but not as much to warm the land. So when the air temperature is warm, it warms the land surface rapidly. The ocean takes much longer to warm, but it holds heat longer. Generally, in summer the land is warmer than the ocean, and in winter the ocean is warmer than the land.
large amounts of water stabilize temperatures
In most cases, the water temperature only affects land temperatures when the land is in relatively close proximity to the water. The winds will flow accross the warmer water and carry the radiated heat over the land closest to the shoreline. As the wind blows further inland, the affects of the water are slowly dropped off. In contrast, the air temperatures can SLOWLY affect the water temperatures. Over time, cooler/warmer air temps will cool/warm the waters if the temps are fairily consistent for a period of time. The larger the body of water, the longer it takes for the air to affect it.
Moderating Effects - effect that large climate over nearby land areas. Winter temperatures are warmer and summer temperatures are warmer and summer temperatures are cooler than areas located away from large water bodies. The result is a small annual temperature range.
has a higher density
the water gets warmer because it has fewer particle's
Oceans cause the land masses near by to have more moderate temperatures. (Cooler summers and warmer winters.)
Bodies of water have a moderating effect on land temperatures because in a moderate climate, such as Vancouver, Canada, the air from the oceans in the summertime is cooler and blows onto the adjacent land, whereas in the wintertime, the air masses from the warmer waters blows onto the nearby land and causes the land to warm up. Although, for a continental climate, such as Winnipeg, Canada, the exact oppostie happens. The cold air from the oceans blows onto the nearby land and thus makes everything cooler, and in the summer, the warmer air masses blows onto the land and makes everything warmer. This is also considered an extreme climate. Therefore, bodies of water regulate temperatures of the nearby land, and in cases of El Nino, have affects temperatures on a global scale.
water temperatures change more slowly than land temperatures.
The sea has a constant temperature and as a result keeps the temperatures on the coast more constant. it is warmer in the winter and cooler in the summer.
Land heats more rapidly and to higher temperatures than water. Land also cools more rapidly and to lower temperatures than water
Land heats more rapidly and to higher temperatures than water. Land also cools more rapidly and to lower temperatures than water
at night the air over the water is warmer than the air over the land
Sea breezes come from land and over the water, and happen in daytime. Land breezes come from water and over the land, and happen at night.