TY - JOUR
T1 - The δ-six-stream spherical harmonic expansion adding method for solar radiative transfer
AU - Xue, Dan
AU - Zhang, Feng
AU - Shi, Yi Ning
AU - Iwabuchi, Hironobu
AU - Li, Jiangnan
AU - Hu, Shuai
AU - Han, Wei
N1 - Funding Information:
The work is supported by the National Natural Science Foundation of China ( 41675003 ). Appendix A
Publisher Copyright:
© 2019
PY - 2020/3
Y1 - 2020/3
N2 - A δ-six-stream spherical harmonic expansion adding method (δ-6SDA) for solar radiative transfer is proposed. δ-6SDA has similar accuracy as δ-six-stream discrete ordinates method (δ-6DOM) but it is almost three orders of magnitude faster than δ-6DOM in flux calculation. In addition, δ-6SDA is extended to calculate the azimuthally dependent intensity in this study. The truncated-plus-single-scattering (TMS) correction is introduced to improve accuracy. Two single-layer cases with the Cloud C1 phase function and Henyey-Greenstein phase function are considered to investigate the accuracy of δ-6SDA for intensity calculation. The relative errors of these two cases for δ-6SDA are generally less than 2% and 5%, respectively. The root-mean-square errors for δ-6SDA are generally smaller than δ-6DOM. The computing time of δ-6SDA is 3–4 orders of magnitude less than δ-6DOM. Due to its high accuracy and efficiency, δ-6SDA can be widely used in remote sensing for simulating satellite observations.
AB - A δ-six-stream spherical harmonic expansion adding method (δ-6SDA) for solar radiative transfer is proposed. δ-6SDA has similar accuracy as δ-six-stream discrete ordinates method (δ-6DOM) but it is almost three orders of magnitude faster than δ-6DOM in flux calculation. In addition, δ-6SDA is extended to calculate the azimuthally dependent intensity in this study. The truncated-plus-single-scattering (TMS) correction is introduced to improve accuracy. Two single-layer cases with the Cloud C1 phase function and Henyey-Greenstein phase function are considered to investigate the accuracy of δ-6SDA for intensity calculation. The relative errors of these two cases for δ-6SDA are generally less than 2% and 5%, respectively. The root-mean-square errors for δ-6SDA are generally smaller than δ-6DOM. The computing time of δ-6SDA is 3–4 orders of magnitude less than δ-6DOM. Due to its high accuracy and efficiency, δ-6SDA can be widely used in remote sensing for simulating satellite observations.
KW - Azimuthally dependent intensity
KW - Rapid solar radiative transfer
KW - TMS correction
KW - δ-six-stream spherical harmonic expansion adding method
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U2 - 10.1016/j.jqsrt.2019.106818
DO - 10.1016/j.jqsrt.2019.106818
M3 - Article
AN - SCOPUS:85077502644
SN - 0022-4073
VL - 243
JO - Journal of Quantitative Spectroscopy and Radiative Transfer
JF - Journal of Quantitative Spectroscopy and Radiative Transfer
M1 - 106818
ER -