This mass of air―extending over a vertical distance of about 6200 miles―is basically divided into five zones or layers. Anthrosphere: Anthrosphere constitutes the fifth sphere of the environment along with the geosphere, hydrosphere, atmosphere and biosphere. Temperature: hot zones, cold zones. Earth is the only planet in the solar system with an atmosphere that can sustain life. Zone of Atmosphere # 5. Going by the simplest definition possible, atmosphere is the mass of air surrounding the Earth.

As variation of solar radiation is the single most important factor affecting climate, it is considered here first. Temperature increases with height and can rise to as high as 3,600 degrees Fahrenheit (2000 C).

A change in temperature with distance is called a temperature gradient.

It is also the layer where the majority of our weather occurs (Figure 7b-2).

A: independent of temperature. Visible minute water particles suspended in the atmosphere that reduce visibility to fewer than 7 miles (11 km) but more than or equal to 5/8 th mile (1 km). The mathematical average of the two figures gives the average daily temperature.

(2008) and he asserts that “carbon dioxide levels and temperature track identically ” (emphasis added) with the implication that rising carbon dioxide levels increase the Earth’s temperature. The atmosphere is divided into layers based on how the temperature in that layer changes with altitude, the layer’s temperature gradient. Here's a good example of this effect. Scientists divided the atmosphere into four layers according to temperature: troposphere, stratosphere, mesosphere, and thermosphere. The coldest temperatures in Earth's atmosphere, about -90° C (-130° F), are found near the top of this layer. The air is so thin that a molecule will travel 1 kilometer before striking another molecule (Compare that with less than a millionth of a centimeter at the earth's surface). The average temperature of outer space around the Earth is a balmy 283.32 kelvins (10.17 degrees Celsius or 50.3 degrees Fahrenheit). Nonetheless, the air would feel cold because the hot molecules are so far apart.

This layer is known as the upper atmosphere, and it is where the auroras occur ( northern and southern lights). CIt has greater pressure at the top than at the bottom. There is often not much difference in the appearance of 'haze' and 'mist'.

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 coldest temperatures in Earth's atmosphere, about -90° C (-130° F), are found near the top of this layer. High relative humidity of the air occurs when the air temperature approaches the dew point value. When temperatures drop, relative humidity increases. A: At mid night. On average, the temperature gradient of the troposphere is 6.5°C per 1,000 m (3.6°F per 1,000 ft.) of altitude. Our bodies rely on the constant bombardment of air molecules to detect temperature. Climate - Climate - Solar radiation and temperature: Air temperatures have their origin in the absorption of radiant energy from the Sun. Answer- Just before sun rise.

However, because the air is so thin, our bodies would not be able to detect this heat.

Zones of atmosphere based on the air temperature diagram Ask for details ; Follow Report by ... stratosphere, mesosphere, and thermosphere. B: At 3 a.m. C: Just before sun rise. BIt is located 75 kilometers above sea level. About 80% of the total mass of the atmosphere is contained in troposphere. More heat is lost to the atmosphere as the rays travel a longer distance through the atmosphere. Starting from the surface of the Earth, these layers are troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Troposphere. However, because the air is so thin, our bodies would not be able to detect this heat. Argon, carbon dioxide and various trace gases make up the remainder.