Output of aquaplanet idealized GCM simulations under perpetual solstice-like forcing from Singh 2019, J. Atmos. Sci.

# Overview

This directory contains the output from simulations in the idealized aquaplanet GCM that were originally reported in Singh 2019, J. Atmos Sci.  The contents are as follows:

```
├── Omega0.125_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega0.25_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega0.5_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega0.66_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega0.75_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega1.5_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega1_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega2_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega3_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega4_y0005-y0010.mean.1x5days.zonal_avg.nc
├── Omega8_y0005-y0010.mean.1x5days.zonal_avg.nc
└── README.md
```

where `Omega*x` indicates the rotation rate multiplicative factor, with 1x being Earth's rotation rate.  All simulations are performed with time-invariant northern solstice insolation.  A full description of the simulation setups is available in Singh 2019.

# References

Idealized GCM formulation: Frierson, Dargan M. W., Isaac M. Held, and Pablo Zurita-Gotor. “A Gray-Radiation Aquaplanet Moist GCM. Part I: Static Stability and Eddy Scale.” Journal of the Atmospheric Sciences 63, no. 10 (October 1, 2006): 2548–66. https://doi.org/10.1175/JAS3753.1.

Simulations: Singh, Martin S. “Limits on the Extent of the Solsticial Hadley Cell: The Role of Planetary Rotation.” Journal of the Atmospheric Sciences 76, no. 7 (April 30, 2019): 1989–2004. https://doi.org/10.1175/JAS-D-18-0341.1.