CONAN.utils.CA_08_PCmodel#
- CONAN.utils.CA_08_PCmodel(phi, Fd, C1, D1, C2, D2)#
Calculate the phase curve of a planet using the Cowan & Agol 2008 model. See also https://iopscience.iop.org/article/10.3847/1538-3881/ae0e52/meta and https://arxiv.org/pdf/2305.06240
The equation is given as F = Fd + C1*(cos(theta) - 1) + D1*sin(theta) + C2*(cos(2*theta) - 1) + D2*sin(2*theta) where theta = phi + pi, and phi is the phase angle of the planet (true anomaly+omega-pi/2) in radians.
- Parameters:
phi (array-like) – phase angle (2*pi*phase for circular orbit) or true anomaly+omega-pi/2 in radians.
Fd (float) – Dayside flux/occultation depth
C1 (float) – first cosine coefficient
D1 (float) – first sine coefficient
C2 (float) – second cosine coefficient
D2 (float) – second sine coefficient
- Returns:
F – planetary flux as a function of phase angle
- Return type:
array-like
Example
>>> from utils import CA_08_PCmodel >>> import numpy as np >>> phases = np.linspace(-0.25, 0.75, 10000) >>> phi = 2 * np.pi * phases >>> Fn, Fd = 50e-6, 400e-6 >>> C1 = (Fd - Fn)/2 >>> D1, C2, D2 = -139e-6, 46e-6, -15e-6 #D1 somehow influences the phase shift. find an expression for it >>> res = CA_08_PCmodel(phi, Fd, C1, D1, C2, D2)
>>> from CONAN.utils import cosine_atm_variation >>> pc = CA_08_PCmodel(phi, Fd, C1, D1, C2, D2) >>> cos = cosine_atm_variation(phi, Fd, Fn,delta).pc >>> plt.figure() >>> plt.plot(phases, pc) >>> plt.plot(phases, cos) >>> plt.axvline(0.5, color='k', ls='--') >>> # plt.axvline(0.5 - np.radians(delta) / (2 * np.pi)) >>> plt.axhline(Fd-2*C1, color='k', ls='--') >>> plt.axvline(0)