Feedback attribution of the land-sea warming contrast in a global warming simulation of the NCAR CCSM4

One of the salient features in both observations and climate simulations is a stronger land warming than sea. This paper provides a quantitative understanding of the main processes that contribute to the land-sea warming asymmetry in a global warming simulation of the NCAR CCSM4. The CO 2 forcing alone warms the surface nearly the same for both land and sea, suggesting that feedbacks are responsible for the warming contrast. Our analysis on one hand confirms that the principal contributor to the above-unity land-to-sea warming ratio is the evaporation feedback; on the other hand the results indicate that the sensible heat flux feedback has the largest land-sea warming difference that favors a greater ocean than land warming. Furthermore, the results uniquely highlight the importance of other feedbacks in establishing the above-unity land-to-sea warming ratio. Particularly, the SW cloud feedback and the ocean heat storage in the transient response are key contributors to the greater warming over land than sea

Atmospheric sciences · Climate change · Climatology · Effects of global warming on oceans · Forcing (mathematics · Global warming · Greenhouse gas · Sensible heat · Atmospheric and Environmental Gas Dynamics · Climate variability and models · Environmental Science · Meteorological Phenomena and Simulations · Geology · Oceanography

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