Earth's atmosphere is a unique reservoir of gases, the product of nearly 5 billion years of development. It sustains us and protects us from hostile radiation and particles from the Sun and beyond-the atmosphere serves as an efficient filter.When astronauts work in space, they must wear a bulky spacesuit that does everything to sustain and protect them that the atmosphere does for us all the time.Atmosphere is a gaseous mixture of ancient origin, the sum of all the exhalations and inhalations of life on Earth throughout time.
The principal substance of this atmosphere is air, the medium of life as well as a major industrial and chemical raw material. Air is a simple mixture of gases that is naturally odorless, colorless,
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Even though the atmosphere rapidly changes density in the homosphere - increasing toward Earth's surface - the blend (proportion) of gases is nearly uniform throughout the homosphere.The stable mixture of gases comprising air in the homosphere evolved slowly. The present proportion, which includes oxygen, evolved approximately 500 million years ago.
5.The homosphere is a vast reservoir of relatively inert nitrogen, originating principally from volcanic sources.Nitrogen is a key element of life, yet we exhale all the nitrogen we inhale.The explanation for this contradiction is that nitrogen integrates into our bodies not from the air we breathe but through compounds in food.In the soil, nitrogen is bound to these compounds by nitrogen-fixing bacteria, and it returns to the atmosphere by denitrifying bacteria that remove nitrogen from organic materials.The other main constituent gases are Oxygen, Argon and Carbon dioxide.Although it forms about one fifth of the atmosphere, oxygen forms compounds that forms half of Earth’s crust
Atmospheric Temperature Criterion
Shifting to temperature as a criterion, the atmosphere has four distinct temperature zones - the thermosphere, mesosphere, stratosphere, and troposphere.
1.Thermosphere: we define the thermosphere ("heat sphere") as roughly corresponding to the heterosphere.The upper limit of the thermosphere is called the thermopause (the suffix -pause means
The biosphere consists of a compound infusion of gases; the main components are oxygen, nitrogen, and carbon dioxide. The concentration of these gases have been changing for many years. For the most part, this is influenced by human activity. In a persistent effort to improve the quality and longevity of life, humans (particularly in industrialized societies) have tendencies to negatively impact the environment, and at the same time, we strive to replenish what we have nearly depleted to balance the scale.
The atmosphere in a place and time in regards to heat, dryness, sunshine, wind, rain, etc.
What are the different layers of the atmosphere? What are some characteristics of each? I mentioned in class that you should focus on knowing about two of these atmospheric layers in particular.
Weather and climate are separate but related terms. The term weather refers to short-run atmospheric conditions that exist for a
The element of air gives humans life. Air represents new life and new possibilities. Life is what allows humans to think, feel, see and have emotions. In The Wars by Timothy Findley the element of air pushes humans to reach their full potential. Robert Ross illustrates this with his desire to live, desire to leave a mark and his desire to overcome hardships. Soldiers did not want to just live; but to live for something and leave a legacy in history.
Nitrogen fixation = Nitrogen gas is combined (fixed) with hydrogen by nitrogen-fixing bacteria to become ammonium
Movements and interactions in the lithosphere and the internal Earth processes that drive them are referred to as the _____ cycle.
*Nitrogen, which accounts for 78 percent of the atmosphere, exists in the atmosphere in a form unusable by living organisms.
There are three different weather bands in each hemisphere, they are trade winds, polar easterlies, and prevailing westerlies.
Higher altitudes are cooler than lower altitudes, which is explained by the lapse rate. On local scales, temperature differences can occur because different surfaces (such as oceans, forests, ice sheets, or man-made objects) have differing physical characteristics such as reflectivity, roughness, or moisture content.
It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 6 mi and 30 mi altitude above the surface at moderate latitudes, while at the poles it starts at about 5 mi altitude.
The Earth formed 4.6 billion years ago through collisions in the giant disked shape cloud created from the Bing Bang. It is a dynamic planet, with
1) The ozone layer is a layer of ozone high up in the Earth's atmosphere stratosphere.
I. (Main Point = Need) According to NASA climate is made up of two things. Those two things are the climates of certain locations during the different seasons and the Earth’s climate which is a combination of all those different induvial climates.
“The atmosphere holds carbon dioxide and other gases that keep the planet warm and protect its surface from radiation.” Again, radiation is a bad thing, so the atmosphere helps with that as well. It keeps the good gasses in (the bad, too, unfortunately, though I think it keeps some gasses out as well) that would otherwise make Earth impossible to be sustain life.