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Relevant bibliographies by topics / Aquaplanet

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Journal articles

Academic literature on the topic 'Aquaplanet'

Author: Grafiati

Published: 6 September 2023

Last updated: 7 September 2023

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Journal articles on the topic "Aquaplanet"

1

Yano, Jun-Ichi, and John L. McBride. "An Aquaplanet Monsoon." Journal of the Atmospheric Sciences 55, no. 8 (1998): 1373–99. http://dx.doi.org/10.1175/1520-0469(1998)055<1373:aam>2.0.co;2.

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2

Medeiros, Brian, Bjorn Stevens, Isaac M. Held, et al. "Aquaplanets, Climate Sensitivity, and Low Clouds." Journal of Climate 21, no. 19 (2008): 4974–91. http://dx.doi.org/10.1175/2008jcli1995.1.

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Abstract Cloud effects have repeatedly been pointed out as the leading source of uncertainty in projections of future climate, yet clouds remain poorly understood and simulated in climate models. Aquaplanets provide a simplified framework for comparing and understanding cloud effects, and how they are partitioned as a function of regime, in large-scale models. This work uses two climate models to demonstrate that aquaplanets can successfully predict a climate model’s sensitivity to an idealized climate change. For both models, aquaplanet climate sensitivity is similar to that of the realistic

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3

Geen, Ruth, F. H. Lambert, and G. K. Vallis. "Regime Change Behavior during Asian Monsoon Onset." Journal of Climate 31, no. 8 (2018): 3327–48. http://dx.doi.org/10.1175/jcli-d-17-0118.1.

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Abstract As the ITCZ moves off the equator on an aquaplanet, the Hadley circulation transitions from an equinoctial regime with two near-symmetric, significantly eddy-driven cells to a monsoon-like regime with a strong, thermally direct cross-equatorial cell, intense low-latitude precipitation, and a weak summer hemisphere cell. Dynamical feedbacks appear to accelerate the transition. This study investigates the relevance of this behavior to monsoon onset by using primitive equation model simulations ranging from aquaplanets to more realistic configurations with Earth’s continents and topograp

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4

Merlis, Timothy M., and Isaac M. Held. "Aquaplanet Simulations of Tropical Cyclones." Current Climate Change Reports 5, no. 3 (2019): 185–95. http://dx.doi.org/10.1007/s40641-019-00133-y.

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5

Zappa, Giuseppe, Valerio Lucarini, and Antonio Navarra. "Baroclinic Stationary Waves in Aquaplanet Models." Journal of the Atmospheric Sciences 68, no. 5 (2011): 1023–40. http://dx.doi.org/10.1175/2011jas3573.1.

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Abstract An aquaplanet model is used to study the nature of the highly persistent low-frequency waves that have been observed in models forced by zonally symmetric boundary conditions. Using the Hayashi spectral analysis of the extratropical waves, the authors find that a quasi-stationary wave 5 belongs to a wave packet obeying a well-defined dispersion relation with eastward group velocity. The components of the dispersion relation with k ≥ 5 baroclinically convert eddy available potential energy into eddy kinetic energy, whereas those with k &lt; 5 are baroclinically neutral. In agreemen

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6

Williams, Gareth P., and Kirk Bryan. "Ice Age Winds: An Aquaplanet Model." Journal of Climate 19, no. 9 (2006): 1706–15. http://dx.doi.org/10.1175/jcli3766.1.

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Abstract Factors controlling the position and strength of the surface winds during the Last Glacial Maximum (LGM) are examined using a global, multilevel, moist, atmospheric model. The idealized aquaplanet model is bounded below by a prescribed axisymmetric temperature distribution that corresponds to an ocean-covered surface. Various forms of this distribution are used to examine the influence of changes in the surface cooling and baroclinicity rates. The model omits seasonal variations. Increasing the cooling lowers the tropopause and greatly reduces the moist convection in the Tropics, ther

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7

Bhattacharya, Ritthik, Simona Bordoni, Kay Suselj, and João Teixeira. "Parameterization Interactions in Global Aquaplanet Simulations." Journal of Advances in Modeling Earth Systems 10, no. 2 (2018): 403–20. http://dx.doi.org/10.1002/2017ms000991.

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8

Shi, Xiaoming, Daehyun Kim, Ángel F. Adames, and Jai Sukhatme. "WISHE‐Moisture Mode in an Aquaplanet Simulation." Journal of Advances in Modeling Earth Systems 10, no. 10 (2018): 2393–407. http://dx.doi.org/10.1029/2018ms001441.

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9

Hertwig, Eileen, Frank Lunkeit, and Klaus Fraedrich. "Low-frequency climate variability of an aquaplanet." Theoretical and Applied Climatology 121, no. 3-4 (2014): 459–78. http://dx.doi.org/10.1007/s00704-014-1226-8.

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10

Geen, Ruth, F. Hugo Lambert, and Geoffrey K. Vallis. "Processes and Timescales in Onset and Withdrawal of “Aquaplanet Monsoons”." Journal of the Atmospheric Sciences 76, no. 8 (2019): 2357–73. http://dx.doi.org/10.1175/jas-d-18-0214.1.

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Abstract Aquaplanets with low-heat-capacity slab-ocean boundary conditions can exhibit rapid changes in the regime of the overturning circulation over the seasonal cycle, which have been connected to the onset of Earth’s monsoons. In spring, as the ITCZ migrates off the equator, it jumps poleward and a sudden transition occurs from an eddy-driven, equinoctial regime with two weak Hadley cells, to a near-angular-momentum-conserving, solstitial regime with a strong, cross-equatorial winter-hemisphere cell. Here, the controls on the transition latitude and rate are explored in idealized moist aqu

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