Journal of Advances in Modeling Earth Systems

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Accepted Articles (Accepted, unedited articles published online and citable. The final edited and typeset version of record will appear in future.)

Online ISSN: 1942-2466

  1. Regular Articles

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      Response of tropical sea surface temperature, precipitation, and tropical cyclone-related variables to changes in global and local forcing

      Kerry Emanue and Adam Sobel

      Accepted manuscript online: 9 MAY 2013 02:55AM EST | DOI: 10.1002/jame.20032

      Key Points

      • Tropical climate is not a unique function of relative or absolute SST
      • Rain forced by changing surface wind is inversely related to SST
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      Development and validation of a hurricane nature run using the joint OSSE nature run and the WRF model

      David S. Nolan, Robert Atlas, Kieran T. Bhatia and Lisa R. Bucci

      Accepted manuscript online: 7 MAY 2013 12:39AM EST | DOI: 10.1002/jame.20031

      Key Points

      • A hurricane nature run has been developed
      • The nature run hurricane reproduces the life cycle of an Atlantic hurricane
      • Validation against observations shows that the simulated hurricane is realistic
  2. Correction

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  3. Regular Articles

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      The land contribution to natural CO2 variability on time scales of centuries

      Rainer Schneck, Christian H. Reick and Thomas Raddatz

      Accepted manuscript online: 9 APR 2013 04:33AM EST | DOI: 10.1002/jame.20029

      Key Points

      • Quantification of natural C cycle variability on centennial time scales.
      • Natural C cycle variability is caused by the land and is buffered by the ocean.
      • Natural C cycle variability is mainly caused by LAI variations.
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      Shock-like structures in the tropical cyclone boundary layer

      Gabriel J. Williams, Richard K. Taft, Brian D. McNoldy and Wayne H. Schubert

      Accepted manuscript online: 9 APR 2013 04:33AM EST | DOI: 10.1002/jame.20028

      Key Points

      • Tropical cyclones produce shock-like structures in the boundary layer
      • There is evidence in observational data for such shock-like structures
      • Previous modelling work also shows such shock-like structures
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      Characteristics of the ocean simulations in MPIOM, the ocean component of the MPI-Earth system model

      J.H. Jungclaus, N. Fischer, H. Haak, K. Lohmann, J. Marotzke, D. Matei, U. Mikolajewicz, D. Notz and J.S. von Storch

      Accepted manuscript online: 2 MAR 2013 09:05AM EST | DOI: 10.1002/jame.20023

      Key Points

      • documentation the performance of MPIOM in the new MPI-ESM coupled system
      • Assessment of impact of ocean resolution
      • Specific investigation of the Agulhas region
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      Seasonal aspects of the quasi-biennial oscillation in MPI-ESM and ERA-40

      Thomas R. Krismer, Marco A. Giorgetta and Monika Esch

      Accepted manuscript online: 2 MAR 2013 08:35AM EST | DOI: 10.1002/jame.20024

      Key Points

      • Phase Alignment of QBO westerly jets at 5 hPa in spring and fall due to SAO
      • Seasonal varying propagation of jets initiated in spring and fall
      • Propagation rates modulated by varying wave forcing and momentum advection
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      The representation of natural and anthropogenic land cover change in MPI-ESM

      C. H. Reick, T. Raddatz, V. Brovkin and V. Gayler

      Accepted manuscript online: 26 FEB 2013 10:56AM EST | DOI: 10.1002/jame.20022

      Key Points

      • Description of models for natural and anthropogenic land cover change
      • Accounting for the preferential allocation of pastures on former grasslands
      • Accounting for land use change induced by changes in natural vegetation
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      Mechanisms of marine low cloud sensitivity to idealized climate perturbations: A single- LES exploration extending the CGILS cases

      Christopher S. Bretherton, Peter N. Blossey and Christopher R. Jones

      Accepted manuscript online: 1 FEB 2013 11:44AM EST | DOI: 10.1002/jame.20019

      Key Points

      • LES low-cloud feedbacks positive due to enhanced vertical humidity gradients
      • Less subsidence in warmer climate counteracts positive low cloud feedbacks
      • Precipitation and cloud droplet number affect cumulus depth, climate feedbacks
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      The global ocean biogeochemistry model HAMOCC: Model architecture and performance as component of the MPI-earth system model in different CMIP5 experimental realizations

      Tatiana Ilyina, Katharina D. Six, Joachim Segschneider, Ernst Maier-Reimer, Hongmei Li and Ismael Núñez-Riboni

      Accepted manuscript online: 30 JAN 2013 02:41AM EST | DOI: 10.1002/jame.20017

      Key Points

      • Evaluation of the model HAMOCC within CMIP5 experiments
      • Ocean biogeochemistry in an Earth system model
      • Ocean carbon cycle in idealized CMIP5 experiments
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      The madden-julian oscillation as simulated by the mpi earth system model: Over the last and into the next millennium

      Jonathan J. Schubert, Bjorn Stevens and Traute Crueger

      Accepted manuscript online: 11 JAN 2013 01:53PM EST | DOI: 10.1002/jame.20010

      Key Points

      • The MJO varies on interannual to interdecadal time scales
      • Solar variability and volcanoes may have influenced the MJO strength marginally
      • CO2 increased by 1% per year over 150 yrs show the MJO to strengthen by 11%
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      Climate and climate change in a radiative-convective equilibrium version of ECHAM6

      D. Popke, B. Stevens and A. Voigt

      Accepted manuscript online: 11 JAN 2013 01:50PM EST | DOI: 10.1002/jame.20009

      Key Points

      • ECHAM6 is configured to run in RCE with a mixed-layer ocean
      • RCE similar to tropics in mean vertical structure and overturning circulation
      • Lower climate sensitivity in RCE than in full GCM although feedbacks are present
  4. Regular Article

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      Analytical solutions of the potential vorticity invertibility principle

      Matthew T. Masarik and Wayne H. Schubert

      Accepted manuscript online: 11 JAN 2013 01:50PM EST | DOI: 10.1002/jame.20011

      Key Points

      • Analytical solutions of the PV invertibilityprinciple are derived
      • Solutions aid in understanding thedynamics of low latitude PV intrusions
      • Illustration of isentropic upglide below positive PV anomalies

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