Abstract
Numerous ecological studies, including of the polar environment, are now using the remotely sensed normalized difference vegetation index (NDVI, e.g. PAL-NDVI or MODIS-NDVI) as a proxy of vegetation productivity rather than performing direct vegetation assessments. Even though previous data strongly suggested a saturation of NDVI at high biomass values, few studies have explicitly included this characteristic in the modelling process. Here, we developed a generalized non-linear model to explicitly model the relationship between temporal variations of NDVI (Pathfinder AVHRR Land 8 km dataset) and empirical field data. We illustrated our approach on the Kerguelen archipelago by using a green biomass index (point-intercept protocol) sampled at a small scale relative to PAL-NDVI data, and in presence of spatial (water) and temporal (cloud contamination, snow) heterogeneity, i.e. field conditions encountered in many ecological studies. We showed a strong relationship (r pred.obs = 0.89 [0.77; 0.95]95%) between this index and the seasonal component of NDVI time series (NDVIcomp). Despite the absence of lignified species in the stand, the NDVIcomp reached an asymptote (0.54 ± 0.05) for high values of green biomass index stressing the need to account for non-linearity when relating NDVI and plant measurements. We provided here a new methodological framework to standardize comparisons between studies assessing performance of NDVI as a proxy of vegetation data.
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National Oceanic and Atmospheric Administration.
National Aeronautics and Space Administration.
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Acknowledgments
We thank the French Polar Institute Paul-Emile Victor (IPEV) for financial support (programmes 279 and 136). Many thanks are due to J.-M. Gaillard, P. Aubry, R. Ecochard, M.-L. Delignette-Muller, I. Herfindal, J.-D. Lebreton, A. Avril and S. Hamel for their helpful suggestions on an earlier version of the manuscript. We also thank N. G. Yoccoz, S. Ryan and one anonymous referee for their comments that greatly improve the manuscript.
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Appendix
Appendix
This appendix describes the 3 steps of the statistical procedure used to compute prediction intervals of the model presented in this study (see Eqs. 2, 3),
Step 1: Computation of the mean model predictions
We obtained maximum likelihood estimation of {β0, β1, β1, θ} noted \(\{\hat{\beta_{0}},\hat{\beta_{1}},\hat{\beta_{1}}, \hat{\theta}\}\) and computed the means \((\hat{\mu}_{i})\) predicted by the fixed part of the model:
where
Step 2: Parametric bootstrapping of the fixed part of the model
We computed 1,000 vectors of bootstrap observations of length n = 27,
where each μ *j i was sampled in
We fitted the non-linear model (see Eq. 2) on each Q *j to obtain 1,000 bootstrap vectors of parameter estimations,
Using Eq. 7, we computed the 1,000 bootstrap vectors of predictions,
Then, to compute the 95% bootstrap confidence intervals of the ith predicted mean \((\hat{\mu}_{i}),\) we have taken the 0.025 and 0.975 quantiles of the corresponding \(\hat{\mu}^{{\ast}}_{i}\) bootstrap distribution.
Step 3: Monte Carlo generation of the posterior distribution of individual predictions
In order to obtain the 95% prediction intervals, we included the random part of the model in the bootstrap procedure. Thus, we had a noise (Negative Binomial) to the 1000 bootstrap vectors of predicted means \((\hat{P}^{{\ast}j},\) see Eq. 11) to take into account the individual variability,
where each \(\hat{y}^{{\ast}j}_{i}\) (see Eq. 2) was sampled in
Then, to compute the 95% bootstrap prediction interval of the ith predicted observation \((\hat{y}_{i}),\) we took the 0.025 and 0.975 quantiles of the corresponding \(\hat{y}^{{\ast}}_{i}\) bootstrap distribution.
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Santin-Janin, H., Garel, M., Chapuis, JL. et al. Assessing the performance of NDVI as a proxy for plant biomass using non-linear models: a case study on the Kerguelen archipelago. Polar Biol 32, 861–871 (2009). https://doi.org/10.1007/s00300-009-0586-5
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DOI: https://doi.org/10.1007/s00300-009-0586-5