Thermospere
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
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The coldest layer of the Earth's atmosphere is the Mesosphere. At an altitude of 31 miles up to, 53 miles (85 km) from the surface of the Earth. Its temperature ranges from 5 degrees fahrenheit to -184 degrees fahrenheit. Or in terms of Celsius -15 degrees to -120 degrees.
The temp of ionosphere increases when we go upper succesively because it lies in the thermosphere . It's actually 37 degrees celsius.
Thermospere
Thermospere
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
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The approximate height of the stratopause is between 50 to 55 km. The temperature is about negative15 degrees Celsius or 5 degrees Fahrenheit.
1111 Km. The circumference of the earth is about 40,000 kilometers and the earth has a total of 360 degrees. If you want to know what 10 degrees is equal to, use a simple proportional equation. 10 X ------ = ------- 360 40,000 km Then, solve for X.... (cross multiply) (10*40,000)/360= 1111.1111111
It Decreases by 6.5 degrees Celsius per KM. Most weather occurs here where we live. Convection Currents. At the surface it extends out 6-8 km at the poles and 17 km at the equator. Even though the temperature decreases by 6.5 degrees celsivus per KM, it stabilizes at 12 km
The weather in Rio de Janeiro, Brazil in January tends to be hot, rainy, and windy. The average high temperature in January is 90 degrees Fahrenheit [32 degrees Celsius]. The average number of days is 20 for temperatures above 90 degrees Fahrenheit [32 degrees Celsius] and 29 for temperatures over 80 degrees Fahrenheit [26 degrees Celsius]. The average precipitation is 5.1 inches [13 centimeters]. The average windspeed is 10 mph [16 km/h].
if you mean 10km above ground, then it depends where, but -50 Celsius is not unheard of