TY - JOUR
T1 - The variability and seasonality in the ratio of photosynthetically active radiation to solar radiation
T2 - A simple empirical model of the ratio
AU - Akitsu, Tomoko Kawaguchi
AU - Nasahara, Kenlo Nishida
AU - Ijima, Osamu
AU - Hirose, Yasuo
AU - Ide, Reiko
AU - Takagi, Kentaro
AU - Kume, Atsushi
N1 - Funding Information:
The authors thank the staff members of the Ozone and Radiation Division of the Aerological Observatory, JMA. We appreciate the solar radiation data provided by BSRN and the climate data provided by JMA at Tateno. We are grateful to OpenCLASTR project for using the Rstar6b package in this research. This work was supported by the JAXA under contract 102, “Development of integrative information of the terrestrial ecosystem” (PI: Kenlo Nishida Nasahara). This work was also supported by the Japan Society for the Promotion of Science, KAKENHI Grant Number JP19K20433.
Funding Information:
The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Tomoko Kawaguchi Akitsu reports financial support was provided by Japan Society for the Promotion of Science. Kenlo Nishida Nasahara reports financial support was provided by Japan Aerospace Exploration Agency.
Funding Information:
The authors thank the staff members of the Ozone and Radiation Division of the Aerological Observatory, JMA. We appreciate the solar radiation data provided by BSRN and the climate data provided by JMA at Tateno. We are grateful to OpenCLASTR project for using the Rstar6b package in this research. This work was supported by the JAXA under contract 102, ?Development of integrative information of the terrestrial ecosystem? (PI: Kenlo Nishida Nasahara). This work was also supported by the Japan Society for the Promotion of Science, KAKENHI Grant Number JP19K20433.
Publisher Copyright:
© 2022 The Author(s)
PY - 2022/4
Y1 - 2022/4
N2 - A constant ratio of photosynthetically active radiation (PAR) to solar radiation (SR) (about 0.45–0.46) has been used in many ecological studies to convert SR into PAR by multiplication. The constant ratio is useful and convenient. However, there is no general agreement on whether the ratio is 0.45 or 0.46 and how distributed globally. Accordingly, many local empirical ratios have been reported. This study aims to demonstrate a global distribution of the ratio and its changing range. Thus, we created two simple empirical models to estimate the ratio based on the in-situ climatic data to achieve the aim. The models were created based on accurate data of SR and PAR observed using a direct and diffuse separation method at Tateno in Tsukuba, Japan. At three validation sites in Japan, the ratio could be estimated with an error within 3%, a considerable reduction from 15% in using a constant. The numerical model also produced the ratio within approximately 3% errors. Using the proposed model, we demonstrated that the annual mean of the ratio had a range from 0.409 to 0.477. The results will contribute to the uncertainty estimation when using a constant ratio.
AB - A constant ratio of photosynthetically active radiation (PAR) to solar radiation (SR) (about 0.45–0.46) has been used in many ecological studies to convert SR into PAR by multiplication. The constant ratio is useful and convenient. However, there is no general agreement on whether the ratio is 0.45 or 0.46 and how distributed globally. Accordingly, many local empirical ratios have been reported. This study aims to demonstrate a global distribution of the ratio and its changing range. Thus, we created two simple empirical models to estimate the ratio based on the in-situ climatic data to achieve the aim. The models were created based on accurate data of SR and PAR observed using a direct and diffuse separation method at Tateno in Tsukuba, Japan. At three validation sites in Japan, the ratio could be estimated with an error within 3%, a considerable reduction from 15% in using a constant. The numerical model also produced the ratio within approximately 3% errors. Using the proposed model, we demonstrated that the annual mean of the ratio had a range from 0.409 to 0.477. The results will contribute to the uncertainty estimation when using a constant ratio.
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U2 - 10.1016/j.jag.2022.102724
DO - 10.1016/j.jag.2022.102724
M3 - Article
AN - SCOPUS:85125522391
VL - 108
JO - International Journal of Applied Earth Observation and Geoinformation
JF - International Journal of Applied Earth Observation and Geoinformation
SN - 1569-8432
M1 - 102724
ER -