Global Warming Research Papers

Discontinuous permafrost's upper layers thaw during the warm seasons (Glossary, 2004).

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Permafrost consists of several frozen soils ranging from gravel to clay (Heidorn, 2004).

The ability for the water to move within the permafrost enables the water to migrate and accumulate, forming large bodies of ice called ice lenses (Stidger, 2001). Continuous permafrost does not thaw at all during the year.

The problem of global warming is not something that can be solved in a finger snap; it will take many years to fix the damage that we have done.

Stopping the production of green house gases now will help greatly in the future.

Global warming is affecting the world at an alarming rate.

The average temperatures of the world over the past 100 years have risen 0.6 ° C (about 1 ° F).

Continuous permafrost has a top layer called the active layer which thaws every year.

The melting of this ice-rich permafrost is extremely harmful to the earth's surface.

The temperatures haven't just been rising at an average rate each year; they are increasing exponentially.

The Arctic Climate Impact Assessment has proven that global warming is a danger that needs to be dealt with now and that the global warming crisis is aggravated even further by human activity (Berner etc. The Arctic provides important natural resources to the rest of the world; these resources would be greatly affected by the global warming crisis (Berner etc. Areas where water is prevalent in its frozen state are affected the most by the rising temperatures (Armstrong).

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