PyRADS is the Python line-by-line RADiation model for planetary atmosphereS. PyRADS is a radiation code that can provide line-by-line spectral resolution, yet is written in Python and so is flexible enough to be useful in teaching.
This version of PyRADS tackles shortwave calculations using the DISORT radiative solver.
(1) Koll & Cronin, 2018, https://doi.org/10.1073/pnas.1809868115.
(2) Koll & Cronin, 2019, https://arxiv.org/abs/1907.13169.
(3) Stamnes et al, 1988, Applied Optics.
Download to your own computer.
Manually compile the MTCKD model:
- cd $PyRADS/DATA/MT_CKD_continuum/cntnm.H2O_N2/build
- (on a Mac) make -f make_cntnm osxGNUdbl
- (on a Mac if you are using gfortran installed with conda) make -f make_cntnm osxGNUCONDAdbl
- Manually install the pyDISORT wrapper, which solves the radiative transfer equations with scattering (=in the shortwave). Steps marked with (x) use conda to create a separate environment, and are optional.
(x) conda create --clone base --name base_w_pyDISORT
(x) source activate base_w_pyDISORT
python setup.py install
To test whether pyDISORT was successfully installed:
If the installation failed, the test scripts will return "ImportError: No module named disort". If the installation worked, the test scripts will print a large slew of output. If using a separate conda environment, later remember to load that environment with 'source activate' before running pyDISORT or importing pyRADS.
- Run test scripts
To compute outgoing longwave radiation (OLR) in W/m2 for a given surface temperature:
- cd $PyRADS/Test01.olr
- python compute_olr_h2o.py
To compute OLRs for a set of surface temperatures and save the resulting output to txt:
- cd $PyRADS/Test02.runaway
- python compute_olr_h2o.01.100RH.py
To compute SW fluxes in W/m2 for a given surface temperature (here, 300 K) over a limited part of the solar spectrum (here, 1000-2000 cm-1) at some resolution (here, 1 cm-1; see note below) and save the resulting output to txt file in the same directory ("."):
- cd $PyRADS/Test03.sw
- python compute_sw_h2o.py 1000. 2000. 1. 300. .
To stitch together the SW fluxes across the entire solar spectrum (takes a while even at low spectral res; see note below):
- cd $PyRADS/Test04.sw_full_spectrum
- python compute_sw_h2o.py 1000. 10000. 1. 300. .
- python compute_sw_h2o.py 10000. 20000. 1. 300. .
- python compute_sw_h2o.py 20000. 30000. 1. 300. .
- python compute_sw_h2o.py 30000. 90000. 10. 300. .
- python merge_spectrum.py
NOTE: computing opacities + running pyDISORT over the entire solar spectrum becomes computationally very costly. It is much faster to split the spectral calculations up over many spectral chunks, distribute those over parallel processors, and them combine the spectral resolved calculations at the end. Use Merge_Spectral_Output.py to combine discrete chunks of the spectrum.
NOTE: spectral resolution should reflect the available data. E.g., HITRAN2016 doesn't contain H2O lines beyond ~25000 cm-1, so there is no need to retain high spectral resolution in the UV.
NOTE: resolution in test scripts was chosen for relative speed, not accuracy. For research-grade output and model intercomparisons, vertical and spectral resolution need to be increased. For some reference values, see Methods in Koll & Cronin (2018) and Koll & Cronin (2019).
Python 2 or 3 with numpy and scipy.
For the MTCKD continuum model: gmake and gfortran.
For the pyDISORT radiation solver: see https://github.com/chanGimeno/pyDISORT.
PyRADS makes use of HITRAN 2016 line lists (http://hitran.org/), AER's MTCKD continuum model (http://rtweb.aer.com/continuum_frame.html), and the PyTran script published by Ray Pierrehumbert as part of the courseware for "Principles of Planetary Climates" (https://geosci.uchicago.edu/~rtp1/PrinciplesPlanetaryClimate/). Brian Rose (http://www.atmos.albany.edu/facstaff/brose/) has helped improve the code. The SW version of PyRADS uses DISORT, developed by Stamnes et al, and the pyDISORT wrapper, developed by chanGimeno (https://github.com/chanGimeno/pyDISORT).