Journal cover Journal topic
Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Model description paper
29 Nov 2017
Review status
This discussion paper is a preprint. It is a manuscript under review for the journal Geoscientific Model Development (GMD).
The NUIST Earth System Model (NESM) version 3: Description and preliminary evaluation
Jian Cao1,2, Bin Wang1,2, Young-Min Yang2, Libin Ma1,2, Juan Li1,2, Bo Sun1,2, Yan Bao1,2, Jie He1,2, and Xiao Zhou2 1Earth System Modeling Center, the Nanjing University of Info rmation Science and Technology, Nanjing 210044, China
2China-US joint Atmosphere-Ocean Research Center and Internat ional Pacific Research Center, University of Hawaii, Honolulu Hawaii 96822 USA
Abstract. The Nanjing University of Information Science and Technology Earth System Model version 3 (NESM v3) has been developed, aiming to provide a numerical modeling platform for cross-disciplinary earth system studies, project future Earth's climate and environment changes, as well conduct subseasonal-to-seasonal prediction. While the previous model version NESM v1 simulates well the internal modes of climate variability, it has no vegetation dynamics and suffers considerable radiative energy imbalance at the top of the atmosphere and surface, resulting in large biases in the global mean surface air temperature, which limit its utility to simulate past and project future climate changes. The NESM v3 upgraded the atmospheric and land surface model components and improved physical parameterization and conservation of coupling variables. Here we describe the new version's basic features and how the major improvements were made. We demonstrate the v3 model's fidelity and suitability to address the global climate variability and change issues. The 500-year PI experiment shows negligible trends in the net heat flux at the top of atmosphere and the Earth surface. Consistently, the simulated global mean surface air temperature, land surface temperature and sea surface temperature (SST) are all in a quasi-equilibrium state. The conservation of global water is demonstrated by the stable evolution of the global mean precipitation, sea surface salinity (SSS) and sea water salinity. The sea ice extents (SIEs), as a major indication of high latitude climate, also maintain a balanced state. The simulated spatial patterns of the mean outgoing longwave radiation, SST, precipitation, SSS fields are realistic, but the model suffers from a cold bias in the North Atlantic, a warm bias in the Southern Ocean and associated deficient Antarctic sea ice area, as well as a delicate sign of the double ITCZ syndrome. The estimate radiative forcing of quadrupling carbon dioxide is about 7.24 W m-2, yielding a climate sensitivity feedback parameter of −0.98 W m-2 K-1, and the equilibrium climate sensitivity is 3.69 K. The transient climate response from the 1 pct/year increasing CO2 experiment is 2.16 K. The model's performance on internal modes and responses to external forcing during the historical period will be documented in an accompanying paper.
Citation: Cao, J., Wang, B., Yang, Y.-M., Ma, L., Li, J., Sun, B., Bao, Y., He, J., and Zhou, X.: The NUIST Earth System Model (NESM) version 3: Description and preliminary evaluation, Geosci. Model Dev. Discuss.,, in review, 2017.
Jian Cao et al.
Jian Cao et al.
Jian Cao et al.


Total article views: 382 (including HTML, PDF, and XML)

HTML PDF XML Total BibTeX EndNote
299 64 19 382 4 21

Views and downloads (calculated since 29 Nov 2017)

Cumulative views and downloads (calculated since 29 Nov 2017)

Viewed (geographical distribution)

Total article views: 378 (including HTML, PDF, and XML)

Thereof 378 with geography defined and 0 with unknown origin.

Country # Views %
  • 1



Latest update: 18 Mar 2018
Publications Copernicus
Short summary
The development of version 3 of the Nanjing University of Information Science and Technology (NUIST) Earth System Model (NESM v3) aims at building up a comprehensive numerical modeling laboratory for multi-disciplinary studies of the Climate System and Earth System. The model evaluation shows the model obtained stable long-term integrations and reasonable global mean states under the preindustrial (PI) forcing and simulated reasonable climate responses to transient and abrupt CO2 forcing.
The development of version 3 of the Nanjing University of Information Science and Technology...