The annual global temperature from 2000 to 2009 was 0.61 °C (1.1 °F) higher than the average temperature for 1951 to 1980. The average temperature of empty space between celestial bodies is calculated at 3 kelvins (minus 270.15 degrees Celsius or minus 457.87 degrees Fahrenheit). Whether a raindrop is closer to the cold or warm end of that range depends on a number of things including what temperature it starts at high up in the clouds and what the air temperatures are in the upper atmosphere where those clouds are floating. The increased amounts of water vapor in the atmosphere can then absorb more thermal energy radiated from Earth, and this further warms the atmosphere. Because the air is warm, the water can hold more moisture. As temperatures in the atmosphere increase, evaporation of water increases. Increased CO 2 and other GHG concentrations are likely to raise the Earth's average temperature a considerable amount. Absolute zero, the temperature at which absolutely all activity stops, is zero kelvins (minus 273.15 degrees Celsius or …
Climate scientists estimate that the average temperature on Earth would be colder by approximately 30 degrees Celsius (54 degrees Fahrenheit). Thermosphere .
Stratosphere Above the troposphere is the stratosphere, which extends to about 31 miles (50 km) above the Earth's surface. Climate - Climate - Effects of the atmosphere: Of the radiant energy reaching the top of the atmosphere, 46 percent is absorbed by Earth’s surface on average, but this value varies significantly from place to place, depending on cloudiness, surface type, and elevation. The layer of very rare air above the mesosphere is called the thermosphere. On average, raindrops have temperatures somewhere between 32 F (0 C) and 80 F (27 C).
The average temperature of the atmosphere in the world is approximated as a function of altitude by the relation T atm = 288.15 - 6.5z where Tatm is the temperature of the atmosphere in K and z is the altitude in km with z = 0 at sea level. Evaporation increases at all water reservoir sites—groundwater, rivers, streams, oceans, soils. The air in the mesosphere is far too thin to breathe; air pressure at the bottom of the layer is well below 1% of the pressure at sea level, and continues dropping as you go higher. The temperature of the troposphere decreases with height. If the current rate of increase continues, the world will warm by 2 °C (3.6 °F) in the next century. The coldest temperatures in Earth's atmosphere, about -90° C (-130° F), are found near the top of this layer.
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