Essay On Cryosphere And Cosmosphere

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The Earth is made of interacting subsystems referred to as spheres. There are four main spheres: atmosphere, biosphere, geosphere/lithosphere, and hydrosphere. Two other less known spheres are the cryosphere and cosmosphere. The interactions of the four main spheres affect all life on Earth. Some examples are the seasons, rock cycle, water cycle, and how people live in certain regions of the world. Firstly, the atmosphere contains all the air in Earth’s system from the air we breathe to the clouds in the sky. The atmosphere “extends from less than 1m below the surface to more than 10,000km above the planet’s surface. The upper portion of the atmosphere protects the organisms of the biosphere from the Sun’s ultraviolet radiation and absorbs/emits
“The hydrosphere covers 70% of the surface of the earth”(rice). Most of the water on Earth is saltwater. Most of the Earth’s freshwater is frozen, which makes up the cryosphere. The hydrosphere can cause many weather changes when interacting with the geosphere. For example, hurricanes, tsunamis, earthquakes, and more can happen. (ucmp0 Also, the oceans have two main purposes when dealing with climate. “First, it is a large reservoir of chemicals that can contribute to the greenhouse effect in the atmosphere and energy absorbing 90% of the solar radiation which hits the surface. Second, it works with the atmosphere to redistribute the energy received from the sun” (rice) Lastly, the two least known spheres are the cryosphere and cosmosphere. The cryosphere is made up of Earth’s frozen water. There is land ice, such as Greenland, and sea ice, such as floating glaciers that sank the titanic. Recently, there has been concern about the melting glaciers and the Earth’s temperature are warming up. The cosmosphere is the universe surrounding the Earth (ucmp). This includes stars, meteros and other planets we see in the sky. In conclusion, the Earth has many spheres that interact together to create a stable place for all living organisms to live

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