Journal of Advances in Modeling Earth Systems

Cover image for Vol. 6 Issue 2

Early View (Online Version of Record published before inclusion in an issue)

Impact Factor: 4.114

ISI Journal Citation Reports © Ranking: 2012: 7/74 (Meteorology & Atmospheric Sciences)

Online ISSN: 1942-2466

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  1. Research Articles

    1. You have full text access to this OnlineOpen article
      Self-organization of the Earth's climate system versus Milankovitch-Berger astronomical cycles

      Lev A. Maslov

      Article first published online: 23 JUL 2014 | DOI: 10.1002/2014MS000312

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      Key Points

      • Temperature curve is decomposed into two parts: “cyclic” and “stochastic”
      • Two mathematical models are created and studied
      • “Cyclic” and “stochastic” components are two types of self-organization
    2. You have full text access to this OnlineOpen article
      Technical note: Introduction to MIMICA, a large-eddy simulation solver for cloudy planetary boundary layers

      J. Savre, A. M. L. Ekman and G. Svensson

      Article first published online: 23 JUL 2014 | DOI: 10.1002/2013MS000292

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      Key Points

      • Introduction of a new LES solver developed at Stockholm University
      • Evaluation based on a former LES intercomparison of a marine stratocumulus
      • Evaluation based on a low-level mixed-phase Arctic cloud from ISDAC
    3. You have full text access to this OnlineOpen article
      A slab model of the Great Salt Lake for regional climate simulation

      C. Strong, A. K. Kochanski and E. T. Crosman

      Article first published online: 22 JUL 2014 | DOI: 10.1002/2014MS000305

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      Key Points

      • Great Salt Lake represented as slab model coupled to regional climate model
      • Framework accounts for 97% of variance in observed lake surface temperature
      • Shallowness renders lake highly sensitive to projected air temperature changes
    4. You have full text access to this OnlineOpen article
      Damping of glacial-interglacial cycles from anthropogenic forcing

      Jacob Haqq-Misra

      Article first published online: 22 JUL 2014 | DOI: 10.1002/2014MS000326

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      Key Points

      • Anthropogenic forcing can damp the 100,000 year glacial-interglacial cycle
      • A stochastic model is developed to simulate long-term climate variability
      • The cessation of ice age cycles may indicate the anthropocene epoch
    5. You have full text access to this OnlineOpen article
      Large-scale character of an atmosphere in rotating radiative-convective equilibrium

      Xiaoming Shi and Christopher S. Bretherton

      Article first published online: 22 JUL 2014 | DOI: 10.1002/2014MS000342

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      Key Points

      • Multiple tropical cyclone-like vortices coexist in rotating RCE on a sphere
      • Self-aggregation and baroclinic instability limit the spacing of vortices
      • The tropics is dominated by a Hadley circulation driven by eddy momentum flux
    6. You have full text access to this OnlineOpen article
      How does the Redi parameter for mesoscale mixing impact global climate in an Earth System Model?

      Marie-Aude Pradal and Anand Gnanadesikan

      Article first published online: 22 JUL 2014 | DOI: 10.1002/2013MS000273

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      Key Points

      • Increasing isopycnal stirring warms the planet
      • Changes in heat transport do not explain this well
      • Changes in salt transport are the primary driver
    7. You have full text access to this OnlineOpen article
      Improved dust representation in the Community Atmosphere Model

      S. Albani, N. M. Mahowald, A. T. Perry, R. A. Scanza, C. S. Zender, N. G. Heavens, V. Maggi, J. F. Kok and B. L. Otto-Bliesner

      Article first published online: 16 JUL 2014 | DOI: 10.1002/2013MS000279

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      Key Points

      • Refined physical parameterizations of dust in the Community Atmosphere Model
      • Improved soil erodibility, size distributions, wet deposition, and optics
      • Better representation of dust cycle, size distributions, and radiative forcing
    8. You have full text access to this OnlineOpen article
      High cloud increase in a perturbed SST experiment with a global nonhydrostatic model including explicit convective processes

      Yoko Tsushima, Shin-ichi Iga, Hirofumi Tomita, Masaki Satoh, Akira T. Noda and Mark J. Webb

      Article first published online: 16 JUL 2014 | DOI: 10.1002/2013MS000301

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      Key Points

      • Larger positive longwave feedback in NICAM than in conventional GCMs
      • High cloud fraction increases in NICAM in increased SST experiments
      • Possibility of larger high cloud fraction feedback in future models
    9. You have full text access to this OnlineOpen article
      Dependency of parameter values of a crop model on the spatial scale of simulation

      Toshichika Iizumi, Yukiko Tanaka, Gen Sakurai, Yasushi Ishigooka and Masayuki Yokozawa

      Article first published online: 16 JUL 2014 | DOI: 10.1002/2014MS000311

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      Key Points

      • The dependency of parameters of a crop model to spatial scales is examined
      • Parameters representing the yield response to temperature showed the dependency
      • Results indicate the importance of appropriate parameters for regional scale
    10. You have full text access to this OnlineOpen article
      Influence of low-cloud radiative effects on tropical circulation and precipitation

      Solange Fermepin and Sandrine Bony

      Article first published online: 12 JUL 2014 | DOI: 10.1002/2013MS000288

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      Key Points

      • Radiative effects of low clouds enhance tropical precipitation and circulation
      • Low clouds influence precipitation through their coupling to surface fluxes
      • Impacts of low-cloud radiative effects on the tropical climate occur in days
    11. You have full text access to this OnlineOpen article
      Some aspects of the problem of secondary eyewall formation in idealized three-dimensional nonlinear simulations

      K. Menelaou, M. K. Yau and Y. Martinez

      Article first published online: 10 JUL 2014 | DOI: 10.1002/2014MS000316

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      Key Points

      • Sustained rainband heating alone can initiate a secondary eyewall
      • Vertical wind shear may disrupt the process of secondary eyewall formation
      • Boundary layer dynamics contribute rather than initiate a secondary eyewall

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