The thermosphere, one of the outer layers of Earth's atmosphere, has high temperatures but does not feel hot to us because of the extremely low density of molecules in this layer. The lack of molecules means that there is not enough matter to transfer heat to our bodies, making it feel cold even though the temperatures are high.
The hottest layer of the atmosphere is the thermosphere. In this layer, temperatures can soar up to 2,500 degrees Celsius (4,500 degrees Fahrenheit) or higher, primarily due to the absorption of intense solar radiation. However, despite these high temperatures, the thermosphere would not feel hot to a human because the air is extremely thin, meaning there are very few air molecules to transfer heat.
The Earth's solid inner layer is surrounded by the hot molten metal of the outer core. This outer core is composed mostly of iron and nickel, and its high temperatures and pressure give it the ability to flow in a liquid state.
The atmosphere is divided into several layers, each with distinct temperature characteristics. In the troposphere, temperatures decrease with altitude, typically ranging from warm at the surface to cold at higher elevations. The stratosphere experiences a temperature increase due to the absorption of UV radiation by the ozone layer, making it warmer at higher altitudes. In the mesosphere, temperatures again drop, becoming quite cold, while the thermosphere is characterized by extremely high temperatures due to solar radiation, although it would not feel hot to a human because of the low density of air.
The Earth's inner core is extremely hot and is considered the thickest layer. It is composed of solid iron and nickel and can reach temperatures of up to 9,000 degrees Fahrenheit (5,000 degrees Celsius).
Magma is molten rock. Rocks have very high melting temperatures.
The only layer I could think of would be the Thermosphere. The reason why this part of the atmosphere is so hot is that it is the top layer of the atmosphere.
The upper layer of the atmosphere is called the thermosphere because temperatures in this region can reach very high values, up to thousands of degrees Celsius. This is due to the absorption of solar radiation by gases in the thermosphere. Despite the high temperatures, the thermosphere would not feel hot to our skin because the air density is so low.
The layer of the atmosphere that can reach temperatures up to 1800 degrees Celsius is the thermosphere. In this layer, temperatures increase significantly with altitude due to the absorption of high-energy solar radiation. Although the thermosphere can reach such extreme temperatures, it would not feel hot to a human because the air is so thin that there are not enough air molecules to transfer heat effectively.
Yes, photos can melt in a hot car due to the high temperatures causing the emulsion layer to soften and distort.
Air temperatures can reach up to 1800 degrees Celsius in the thermosphere, which is the layer of the atmosphere located above the mesosphere, starting around 85 kilometers (53 miles) above the Earth's surface and extending to about 600 kilometers (373 miles). In this layer, solar radiation causes the sparse air molecules to become highly energized, leading to extremely high temperatures. However, despite the high temperatures, the thinness of the air means that it would not feel hot to a human.
The hottest layer of the atmosphere is the thermosphere. In this layer, temperatures can soar up to 2,500 degrees Celsius (4,500 degrees Fahrenheit) or higher, primarily due to the absorption of intense solar radiation. However, despite these high temperatures, the thermosphere would not feel hot to a human because the air is extremely thin, meaning there are very few air molecules to transfer heat.
High air pressure is typically associated with hot temperatures.
The uppermost layer of the atmosphere is the thermosphere. It feels cold because even though there are few gas molecules present to transfer heat, the few molecules that are present can have very high energies due to high temperatures created by solar radiation. This means that even though the temperature is high, it may not feel hot due to the lack of molecules to transfer that heat.
Tin foil can get as hot as 1,220 degrees Fahrenheit when exposed to high temperatures.
High pressure is typically associated with hot temperatures.
you feel hot. you feel hot.
The thermosphere is the warmest layer of the atmosphere primarily due to its absorption of high-energy solar radiation, particularly ultraviolet (UV) and X-ray radiation. This energy excites the sparse gas molecules present in this layer, leading to significantly higher temperatures, which can reach up to 2,500°C (4,500°F) or more. However, despite these high temperatures, the thermosphere would not feel hot to a human because of the extremely low density of the air, meaning there are very few molecules to transfer heat.