Life is difficult

Blogfa format
Life is difficult
The history of the Earth is only a few billion years ago, before he emerged from the various special economic zone events .danshmndan atmosphere today is sometimes known as the third And.atmvsfyrasly atmosphere of helium and hydrogen was formed at the beginning of it Pashand heat. About 3.5 billion years ago the earth's crust was formed as Srdshdk h strongly by volcanoes that steam was released Mvnyk Mhsvrshd.ayn cause was second in the early atmosphere, including carbon dioxide, water vapor, nitrogen levels had no Ksjn the atmosphere 100 Brabratmvsfyravly greenhouse gas Dasht.bh general this phenomenon Larftn Bzryh that the amount of carbon dioxide is the preservation of the Earth from freezing. In a few million years, water vapor condensed to form rain Vaqyanvs ha revealed that these begin to solve the carbon dioxide absorbed by the oceans were Aksaydkrd.hdvd 50 percent of carbon dioxide in photosynthesis plant opens converting the carbon dioxide was to Ksjn. Reacts with ammonia to form nitrogen special economic zone released Ksjn .afzaysh these bacteria special economic zone can convert ammonia into nitrogen seemed Rsdbyshtr plants are the most important factor Ksjn .drartbat special economic zone with important elements such as iron compounds, but eventually accumulate in the atmosphere as well as Ksjn further special economic zone evolution. Zhvrlayh ozone with UV protection were different special economic zone creatures of the Anmvsfyr nitrogen atmosphere is considered the third -Ksjn. Earth's atmosphere is its classes: Atmvsfyrzmyn uncertainties that extends to a height of several special economic zone gas plays Vksaft made it to the top of the gas slowly by gravity is kept as high as half of the atmosphere located 5.5 km. In general special economic zone atmosphere of the Earth located at an altitude special economic zone of 10 km. The gases in the atmosphere due to the force of gravity, the weight of the upper layers Brlayh final Vfsharbvdh pressure to increase the concentration of 5.6 * 1014 .hjm atmosphere of pressure at sea level Atmvsfyrzmyn 105 mg or time that equal mb1032.2 760 mg Mtrstvn .atmvsfyr mercury is not clear in the upper layers of meteorites special economic zone air as high as 160 km show. Hvara at least as high as 700 km polar Shfqha Nyzvjvd Bhrsabt level of Knnd.ta have different methods for determining levels of scientific research to understand the details of the upper atmosphere is experienced atmosphere continues. Atmvsfyrzmyn now includes combinations of the following gases: the percentage of the element symbol 78.1% 20.9% 0.09% 0.03% 0.0018% 0.0005% 0.0001% 0.00008% 0.00005% 0.00007% N2 O2 Ar CO2 Ne He Kr Xe H O3 carbon nitrogen Oregon Ksjn Exxon Krptvn dyes helium hydrogen dioxide, special economic zone ozone
1. Trvpvsfyr (Troposphere): special economic zone the lowest layer of the atmosphere, which is 17-18 km to 7-8 meters thickness varies from the equator to the poles. Almost all the phenomena special economic zone that affect the development of various special economic zone climate special economic zone zones. Important features of this layer can be found to reduce the temperature of 6 C Hrhzarmtrmy source heat radiation layer of alternating earth surface is .grma Vsrma this layer affects 3 to 4 km altitude Some of the complex is the vertical height of the horizon and the formation of cumulus clouds is Vastratvs. 2. Astratvsfyr (Stratosphere): This layer of Atmvsfyrta height of 60 km of the planet has a clear weather, dry and without Abrast fact Astratvsfyr second layer of cirrus clouds Jvast important in this area is formed. Sharp increase in ultraviolet radiation during special economic zone outbreaks of highly Astratvsfyr sun warms the significant evolution of the weather conditions brings about important features of the Vzvn Astratvsfyr is particularly high in the 20 to 30 km surface Ftvshymayy effect of different reactions caused due to ultraviolet radiation was carried out and therefore dangerous radiation reaching the ground is taken up again when the thermal energy released absorbing atmosphere of the ozone decomposition is which raised atmosphere thermal is. 3. Mzvsfyr (Mesosphere): This layer 85 kilometers above the surface of the planet and its temperature decreases special economic zone rapidly as -80 C at an altitude of 80 km in height reaches temperatures higher than 80 Kylvmtrba height Nyzafzaysh is. 4. Trmvsfyr (thermosphere): This layer has no upper limit is specified temperatures of about 1500 degrees is Calvin aurora effect is a phenomenon of the last Trmvsfyr this area is mainly of nitrogen special economic zone Vaksjn Malykvly special economic zone (O2) and atomic (O) consists of a high temperature due to absorption of ultraviolet radiation by the area where the existing Ksjn due to high concentration of satellites is not able to record high temperatures. 5. Yvnvsfyr (Ionosphere): Azartfa 45 km up to 1000 km area Valktrvnha free ion concentration that causes radio waves are reflected by high-energy radiation (UV, X-rays, as well as particle radiation) from the outside air to the upper classes Vatmha molecules are linked Yvnayzyshn Atmvsfyrvard are causing injury. Drasrmlyh Yvnayzyshn are free electrons in atoms Vbaqymandh special economic zone ion is in this region. In so called Yvnvsfyrnamydh Jvara are usually ultraviolet .tabsh Azartfa 100 km above Oak Malykvl