In matters of height i will assume you are talking about a rather size-able mountain, along the lines of something like Mt. Rainier In Washington state. or Mt. Saint Hellens ( before she blew her top )
The reason the top of a mountain is colder than the bottom is quite simple. The air you breathe is called Atmosphere the closer to the surface of the earth the denser the Atmosphere. As you ascend a mountain, or gain altitude the Atmospheric Pressure reduces.
This reduction in the density of the atmosphere does not allow for the storage of the same amount of heat as lower altitudes. There are many layers of atmosphere, and some Mountains can penetrate several of them.
I have included a link to an image pulled from Google image search to further illustrate. See Related Link
It is cooler on top of a mountain than it is below because the sun's rays do not heat the atmosphere directly. The sun's rays bump into dust particles, splitting into different directions. therefore, as the sun ray's reach the the crust, the soil on the ground insulates more heat as it is located near the timberline where the soil insulates more heat.
because the air at the top of the mountain ha s a lot less oxygen in it at the bottom of it. also the air particles have less room to move then at the bottom of the mountain
The temperature of 85 degrees Fahrenheit is 25 degrees cooler than a temperature of 110 degrees Fahrenheit.
11 Celsius is cooler than 9 Celsius because the lower the temperature, the cooler it is.
Your body is generally warmer than the spoons. The average human body temperature is around 98.6°F (37°C), while spoons, being made of metal, typically take on the ambient temperature of their surroundings, which is usually cooler than body temperature. Thus, when you touch a spoon, it will feel cooler to your skin.
i dont know
Almost always cooler than the rim.
It is cooler on top of a mountain than it is below because the sun's rays do not heat the atmosphere directly. The sun's rays bump into dust particles, splitting into different directions. therefore, as the sun ray's reach the the crust, the soil on the ground insulates more heat as it is located near the timberline where the soil insulates more heat.
because the air at the top of the mountain ha s a lot less oxygen in it at the bottom of it. also the air particles have less room to move then at the bottom of the mountain
The temperature of 85 degrees Fahrenheit is 25 degrees cooler than a temperature of 110 degrees Fahrenheit.
In a wine cooler, red wine should generally be stored on the bottom shelf, as it is typically kept at a slightly warmer temperature than white wine. The bottom shelf can help maintain the ideal temperature for reds, while whites can be placed on the upper shelves where it's cooler. Additionally, storing reds horizontally can help keep the cork moist, preventing it from drying out.
because mountains are closer to the poles
Because 0 oC is a lower value (cooler) than 20 oC - 25 oC (room temperature)
The temperature is cooler in the mountains than in the valleys because of the higher elevation in the mountains, which causes the air to be less dense and therefore cooler. Additionally, cold air tends to sink and accumulate in the valleys, further contributing to the temperature difference.
Could be that there is geothermal activity in the hotter location and could be that the cooler location is on the opposite side of a mountain from an ocean.
Yes, it is true that sperm can develop normally only in sightly cooler temperature than normal body temperature. Sperm need a cooler temp than the rest of the body. The scrotum keeps sperm lower than the body, but tight shorts can keep the testicles too warm for the sperm.
The bottom of the mountain is hotter than the top because as elevation increases, air pressure decreases, causing the air molecules to spread out and the temperature to drop. Conversely, at lower elevations, the air is more densely packed, leading to higher temperatures. Additionally, the bottom of the mountain receives more direct sunlight and heat due to its proximity to the ground.