TY - JOUR
T1 - The effect of estimated PAR uncertainties on the physiological processes of biosphere models
AU - Cho, Jaeil
AU - Oki, Taikan
AU - Yeh, Pat J.F.
AU - Kanae, Shinjiro
AU - Kim, Wonsik
N1 - Funding Information:
This work was partly supported by the Global Environment Research Fund of the Ministry of Environment (S-5), and by the Innovation Program of Climate Change Projection for 21st Century of the Ministry of Education, Culture, Sports, Science, and Technology of Japan. We also thank Dr. Fubao Sun, for his most helpful comments and suggestions.
Copyright:
Copyright 2021 Elsevier B.V., All rights reserved.
PY - 2010/6/24
Y1 - 2010/6/24
N2 - Photosynthetically active radiation (PAR) energy reaching on the vegetated surface is a key determinant of plant physiological processes. Most of biosphere or crop models use the ratio of PAR to incoming solar radiation (Rs), PAR/Rs, to convert Rs into PAR in order to reduce weather data-input requirements. Several existing models simply specify a constant ratio, PAR/Rs = 0.5. However, some field experiments have reported that the ratio PAR/Rs may not be constant. Previous empirical equations of PAR/Rs were derived based on the data of monthly or daily timescales collected from only a few measurement sites, hence they may not be appropriate to be used in current global biosphere models usually with hourly simulation time steps. Here, we represent the exponential correlation between PAR/Rs and sky clearness index (0-1) using hourly data from 54 Ameriflux measurement sites. It is found that PAR/Rs increases up to 0.6 in cloudy conditions when the clearness index (CI) is below ~0.2, whereas it is nearly constant at ~0.42 when CI is above 0.2. When the identified empirical equation is used in the model simulation, it results in -4 to 2% difference in the stomatal conductance compared to that using the constant ratio PAR/Rs = 0.5.
AB - Photosynthetically active radiation (PAR) energy reaching on the vegetated surface is a key determinant of plant physiological processes. Most of biosphere or crop models use the ratio of PAR to incoming solar radiation (Rs), PAR/Rs, to convert Rs into PAR in order to reduce weather data-input requirements. Several existing models simply specify a constant ratio, PAR/Rs = 0.5. However, some field experiments have reported that the ratio PAR/Rs may not be constant. Previous empirical equations of PAR/Rs were derived based on the data of monthly or daily timescales collected from only a few measurement sites, hence they may not be appropriate to be used in current global biosphere models usually with hourly simulation time steps. Here, we represent the exponential correlation between PAR/Rs and sky clearness index (0-1) using hourly data from 54 Ameriflux measurement sites. It is found that PAR/Rs increases up to 0.6 in cloudy conditions when the clearness index (CI) is below ~0.2, whereas it is nearly constant at ~0.42 when CI is above 0.2. When the identified empirical equation is used in the model simulation, it results in -4 to 2% difference in the stomatal conductance compared to that using the constant ratio PAR/Rs = 0.5.
KW - Biosphere model
KW - Photosynthetically active radiation (PAR)
KW - Solar radiation
KW - Stomatal conductance
UR - http://www.scopus.com/inward/record.url?scp=79953051537&partnerID=8YFLogxK
U2 - 10.1016/j.ecolmodel.2010.03.009
DO - 10.1016/j.ecolmodel.2010.03.009
M3 - Article
AN - SCOPUS:79953051537
SN - 0304-3800
VL - 221
SP - 1575
EP - 1579
JO - Ecological Modelling
JF - Ecological Modelling
IS - 12
ER -