When radiative forcing is greater than 1, the excess energy is absorbed by the Earth's surface, oceans, and atmosphere, leading to long-term increases in global temperatures.

Authors

• Person: Not available Organization: mrgscience.com
  ESS Subtopic 6.2: Climate change – Causes and Impacts

Sources

• ESS Subtopic 6.2: Climate change – Causes and Impacts www.mrgscience.com mrgscience.com via serper

Referenced by nodes (5)

• atmosphere concept
• radiative forcing concept
• global average temperatures concept
• Earth location
• oceans concept