Here are the answers to your questions:
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Weather refers to the atmospheric conditions at a specific place and time, such as temperature, humidity, precipitation, and wind. It changes frequently, sometimes within hours. Climate describes the average weather patterns of a region over a long period, typically 30 years or more, and is relatively stable.
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Latitude affects the climate of a place primarily by influencing the amount of solar radiation it receives. Areas closer to the Equator (lower latitudes) receive more direct sunlight and are generally hotter, while areas closer to the poles (higher latitudes) receive less direct sunlight and are generally colder.
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Altitude affects the climate of a place by causing temperatures to decrease with increasing height above sea level. For every 1,000 meters of ascent, the temperature typically drops by about 6.5∘C. This is why mountain tops are often covered in snow, even in tropical regions.
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Sea breezes are local winds that blow from the sea towards the land during the day. This occurs because land heats up faster than water, causing the air above the land to rise and cooler, denser air from the sea to move in. Land breezes are local winds that blow from the land towards the sea during the night. This happens because land cools down faster than water, causing the air above the sea to rise and cooler, denser air from the land to move out.
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The three heat zones of the Earth are:
- The Torrid Zone (or Tropical Zone) is located between the Tropic of Cancer (23.5∘ N) and the Tropic of Capricorn (23.5∘ S). It receives direct sunlight throughout the year and is generally very hot.
- The Temperate Zones are located between the Tropic of Cancer and the Arctic Circle (66.5∘ N) in the Northern Hemisphere, and between the Tropic of Capricorn and the Antarctic Circle (66.5∘ S) in the Southern Hemisphere. These zones experience moderate temperatures with distinct seasons.
- The Frigid Zones (or Polar Zones) are located between the Arctic Circle and the North Pole, and between the Antarctic Circle and the South Pole. These zones receive slanting sun rays, resulting in very cold temperatures and long periods of daylight or darkness.
Hots:
No, the sea breeze does not blow in the evening. In the evening and night, the land cools faster than the sea, leading to a land breeze blowing from the land towards the sea.
Activity:
To complete this activity, you would need to record the daily temperature for seven consecutive days.
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