Due to elevation, temperatures become cooler the higher above sea level you go. Elevation, simply defined, is the height above a given level.
Temperatures drop as elevation increases because the air becomes less dense at higher altitudes, making it more difficult for the air to hold onto heat. This results in a decrease in air pressure and temperature with increasing elevation.
Warm surfaces transfer heat to the air molecules above them, making those air molecules move faster and spread out, which decreases their density and increases their temperature. On the other hand, cool surfaces absorb heat from the surrounding air, causing the air molecules above them to move slower and become denser, resulting in cooler air temperatures.
As you ascend higher above sea level, the air pressure and density decrease. With a decrease in air pressure, the air molecules are less tightly packed, making it harder for them to retain heat. This leads to a temperature drop as you go higher above sea level.
Temperatures rise at night because the Earth's surface loses heat through radiation, causing the air near the surface to cool. This cooling process can lead to temperature inversions, where the air near the surface is cooler than the air above it. As a result, the ground absorbs heat from the sun during the day and releases it at night, causing temperatures to rise.
When air moves from land, it is called a land breeze. This occurs because the land cools faster than the water after sunset, causing the air above the land to become cooler and denser, thus flowing towards the warmer air above the water.
Temperatures drop as elevation increases because the air becomes less dense at higher altitudes, making it more difficult for the air to hold onto heat. This results in a decrease in air pressure and temperature with increasing elevation.
Elevation is the reason that tempertures become cooler as you go higher above sea level.
Warm surfaces transfer heat to the air molecules above them, making those air molecules move faster and spread out, which decreases their density and increases their temperature. On the other hand, cool surfaces absorb heat from the surrounding air, causing the air molecules above them to move slower and become denser, resulting in cooler air temperatures.
As you ascend higher above sea level, the air pressure and density decrease. With a decrease in air pressure, the air molecules are less tightly packed, making it harder for them to retain heat. This leads to a temperature drop as you go higher above sea level.
Above 100 0C water become a gas.
Warmer air rises because it is less dense than cooler air. As air is heated, its molecules move faster and spread out, causing the air to become lighter and rise above the cooler, denser air. This process is known as convection.
Temperatures rise at night because the Earth's surface loses heat through radiation, causing the air near the surface to cool. This cooling process can lead to temperature inversions, where the air near the surface is cooler than the air above it. As a result, the ground absorbs heat from the sun during the day and releases it at night, causing temperatures to rise.
I learned this in science class but i forgot it sorry. :( But maybe this will help go to www.google.com type in your question and look for answers if that doesn't work come back to wikianswers and I'll see what i can do. I think i know! as you go higher above sea level the pressure decreases of a substance gets lower.
Yeast typically dies and becomes inactive at temperatures above 140F (60C).
Bats typically come out at night when temperatures are cooler, usually around dusk when it starts to get dark. They are most active when the temperature is above 50 degrees Fahrenheit.
A sea breeze can occur at nearly any temperature. It is caused when the land is warmer than the sea, causing air to rise above the land and cause a low pressure zone over the land that is filled from cooler air from the sea.
The hand placed below the tray of ice would feel cooler. This is because heat transfer occurs from a warmer object (your hand) to a cooler object (the ice), so the hand in contact with the ice will experience a greater cooling sensation.