TY - JOUR
T1 - Can upscaling ground nadir SIF to eddy covariance footprint improve the relationship between SIF and GPP in croplands?
AU - Wu, Genghong
AU - Guan, Kaiyu
AU - Jiang, Chongya
AU - Kimm, Hyungsuk
AU - Miao, Guofang
AU - Yang, Xi
AU - Bernacchi, Carl J.
AU - Sun, Xiangmin
AU - Suyker, Andrew E.
AU - Moore, Caitlin E.
N1 - Funding Information:
GW, KG, and HK acknowledged the support from NASA Carbon Monitoring System program managed by the NASA Terrestrial Ecology Program. GW, KG CJ, CB and CE acknowledge the support from DOE Center for Advanced Bioenergy and Bioproducts Innovation (U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research under Award Number DE-SC0018420 ). Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author (s) and do not necessarily reflect the views of the U.S. Department of Energy. KG, CJ, CB and XS acknowledge the support from the Advanced Research Projects Agency–Energy (ARPA-E) , US Department of Energy, under award number DE- AR0001382 . GW and KG acknowledged the support from NASA Future Investigators in NASA Earth and Space Science and Technology (FINESST) Program. We thank Dr. Andy Suyker for the Nebraska field sites management and support, and Dr. Carl Bernacchi for the Illinois field sites support. We thank M. Pilar Cendrero-Mateo for sharing code for iFLD SIF retrieval.
Publisher Copyright:
© 2023 Elsevier B.V.
PY - 2023/7/15
Y1 - 2023/7/15
N2 - Ground solar-induced chlorophyll fluorescence (SIF) is important for the mechanistic understanding of the dynamics of vegetation gross primary production (GPP) at fine spatiotemporal scales. However, eddy covariance (EC) observations generally cover larger footprint areas than ground SIF observations (a bare fiber with nadir), and this footprint mismatch between nadir SIF and GPP could complicate the canopy SIF-GPP relationships. Here, we upscaled nadir SIF observations to EC footprint and investigated the change in SIF-GPP relationships after the upscaling in cropland. We included 13 site-years data in our study, with seven site-years corn, four site-years soybeans, and two site-years miscanthus, all located in the US Corn Belt. All sites’ crop nadir SIF observations collected from the automated FluoSpec2 system (a hemispheric-nadir system) were upscaled to the GPP footprint-based SIF using vegetation indices (VIs) calculated from high spatiotemporal satellite reflectance data. We found that SIF-GPP relationships were not substantially changed after upscaling nadir SIF to GPP footprint at our crop sites planted with corn, soybean, and miscanthus, with R2 change after the upscaling ranging from -0.007 to 0.051 and root mean square error (RMSE) difference from -0.658 to 0.095 umol m − 2 s − 1 relative to original nadir SIF-GPP relationships across all the site-years. The variation of the SIF-GPP relationship within each species across different site-years was similar between the original nadir SIF and upscaled SIF. Different VIs, EC footprint models, and satellite data led to marginal differences in the SIF-GPP relationships when upscaling nadir SIF to EC footprint. Our study provided a methodological framework to correct this spatial mismatch between ground nadir SIF and GPP observations for croplands and potentially for other ecosystems. Our results also demonstrated that the spatial mismatch between ground nadir SIF and GPP might not significantly affect the SIF-GPP relationship in cropland that are largely homogeneous.
AB - Ground solar-induced chlorophyll fluorescence (SIF) is important for the mechanistic understanding of the dynamics of vegetation gross primary production (GPP) at fine spatiotemporal scales. However, eddy covariance (EC) observations generally cover larger footprint areas than ground SIF observations (a bare fiber with nadir), and this footprint mismatch between nadir SIF and GPP could complicate the canopy SIF-GPP relationships. Here, we upscaled nadir SIF observations to EC footprint and investigated the change in SIF-GPP relationships after the upscaling in cropland. We included 13 site-years data in our study, with seven site-years corn, four site-years soybeans, and two site-years miscanthus, all located in the US Corn Belt. All sites’ crop nadir SIF observations collected from the automated FluoSpec2 system (a hemispheric-nadir system) were upscaled to the GPP footprint-based SIF using vegetation indices (VIs) calculated from high spatiotemporal satellite reflectance data. We found that SIF-GPP relationships were not substantially changed after upscaling nadir SIF to GPP footprint at our crop sites planted with corn, soybean, and miscanthus, with R2 change after the upscaling ranging from -0.007 to 0.051 and root mean square error (RMSE) difference from -0.658 to 0.095 umol m − 2 s − 1 relative to original nadir SIF-GPP relationships across all the site-years. The variation of the SIF-GPP relationship within each species across different site-years was similar between the original nadir SIF and upscaled SIF. Different VIs, EC footprint models, and satellite data led to marginal differences in the SIF-GPP relationships when upscaling nadir SIF to EC footprint. Our study provided a methodological framework to correct this spatial mismatch between ground nadir SIF and GPP observations for croplands and potentially for other ecosystems. Our results also demonstrated that the spatial mismatch between ground nadir SIF and GPP might not significantly affect the SIF-GPP relationship in cropland that are largely homogeneous.
KW - Cropland
KW - Footprint
KW - Gross primary productivity
KW - Ground
KW - Solar-induced chlorophyll fluorescence
UR - http://www.scopus.com/inward/record.url?scp=85162209567&partnerID=8YFLogxK
U2 - 10.1016/j.agrformet.2023.109532
DO - 10.1016/j.agrformet.2023.109532
M3 - Article
AN - SCOPUS:85162209567
SN - 0168-1923
VL - 338
JO - Agricultural and Forest Meteorology
JF - Agricultural and Forest Meteorology
M1 - 109532
ER -