preview

Global Temperature And Climate Change

Better Essays

Global Temperature

The Earth-atmosphere energy cycle is a structure of coordinating atmospheric components. The Köppen classification system is a simple format for generalizing climate patterns, partitioning the planet into malleable regions by average environmental conditions. Terms to describe the atypical fluctuations in the Earth’s climate include both global warming and climate change. While global warming denotes an average escalation of temperature, climate change suggests a shift in the overall pattern. Climatic zone instabilities, temperature variation, and other deviations that may interrelate with climate are described as global change. The state of global climatic equilibrium can be discerned through focusing on observable imbalances such as positive radiative forcing by atmospheric gasses, temperature fluctuations, weather phenomena and anthropologic influences.
The rate of energy change per unit area of the globe is gauged by radiative forcing. The net gain of energy is positive radiative forcing, with the opposite being negative forcing (SEI & GGMI, 2011). According to the National Weather Service (2012), solar energy absorbed by the atmosphere is typically offset by energy released. Positive radiative forcing by atmospheric gasses may amplify imbalances in the global climatic equilibrium.
Unbalanced absorption ratios signify functional discrepancies in the Earth-atmosphere energy cycle. Proportions fluctuate, but carbon dioxide (CO2) methane, ozone, nitrous

Get Access