The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
The temperature decreases by about 6.5 degrees Celsius per kilometer in the troposphere, so the total temperature change between 3 km and 7 km above the Earth's surface would be approximately 26 degrees Celsius.
The temperature of the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
The geothermal gradient is approximately 25 degrees Celsius per kilometer of depth below Earth's surface. This means that the temperature increases by about 25 degrees Celsius for every kilometer closer to the Earth's core. This gradient is used to estimate subsurface temperatures for geothermal energy extraction and other geological studies.
The surface of the sun is around 10,000 degrees Fahrenheit.
The average rate of temperature increase below the Earth's surface is about 25 to 30 degrees Celsius per kilometer of depth. This increase is known as the geothermal gradient and varies depending on factors such as location, tectonic activity, and local geology.
The surface temperature of the sun is about 10,000 degrees Fahrenheit. However, there is an increase in temperature from the surface to the sun's core, where the temperature can reach nearly 27,000,000 degrees Fahrenheit.
The temperature 2 meters under the Earth's surface varies depending on location, but generally, it can be estimated to increase by about 25-30 degrees Fahrenheit for every kilometer in depth due to the geothermal gradient. Therefore, it would be slightly warmer than the surface temperature.
From the surface of the sun to its center, temperatures can be assumed to increase. The surface temperature of the sun is around 5500 degrees Celsius, while the core temperature is estimated to be around 15 million degrees Celsius.
The temperature in the troposphere can vary depending on factors such as altitude and location, but on average it decreases by about 6.5 degrees Celsius per kilometer of altitude. Near the Earth's surface, the average temperature of the troposphere is around 15 degrees Celsius.
The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
The temperature decreases by about 6.5 degrees Celsius per kilometer in the troposphere, so the total temperature change between 3 km and 7 km above the Earth's surface would be approximately 26 degrees Celsius.
The answer depends on the temperature of what. An increase of 6 degrees C in the body temperature would, in most cases, prove to be very serious. A similar increase in the temperature of the sun would go unnoticed. An increase of that magnitude in the average surface temperature on earth is likely to be catastrophic for human beings though not all life forms.
It can vary greatly depending on location, but generally, the temperature increases by about 25-30 degrees Celsius per kilometer of depth. So at 100 meters, the temperature could be around 25-30 degrees Celsius higher than the surface temperature.
The surface temperature of Omega varies slightly. On average, the maximum surface temperature is 760 degrees Celsius, which converts to 1400 degrees Fahrenheit.
surface tension decreases with the increase of temperature
The temperature of the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.