pre-industrial and mid-pliocene simulations with noresm-l

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ID: 172944
2012
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Abstract
The mid-Pliocene period (3.3 to 3.0 Ma) is known as a warm climate with atmospheric greenhouse gas levels similar to the present. As the climate at this time was in equilibrium with the greenhouse forcing, it is a valuable test case to better understand the long-term response to high levels of atmospheric greenhouse gases. In this study, we use the low resolution version of the Norwegian Earth System Model (NorESM-L) to simulate the pre-industrial and the mid-Pliocene climate. Comparison of the simulation with observations demonstrates that NorESM-L simulates a realistic pre-industrial climate. The simulated mid-Pliocene global mean surface air temperature is 16.7 °C, which is 3.2 °C warmer than the pre-industrial. The simulated mid-Pliocene global mean sea surface temperature is 19.1 °C, which is 2.0 °C warmer than the pre-industrial. The warming is relatively uniform globally, except for a strong amplification at high latitudes.
Reference Key
zhang2012geoscientificpre-industrial Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Z. S. Zhang;K. Nisancioglu;M. Bentsen;J. Tjiputra;I. Bethke;Q. Yan;B. Risebrobakken;C. Andersson;E. Jansen
Journal international journal of quantum chemistry
Year 2012
DOI
10.5194/gmd-5-523-2012
URL
http://www.geosci-model-dev.net/5/523/2012/gmd-5-523-2012.pdf
Keywords
geology

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