Abstract

Land Surface Phenology (LSP) metrics are increasingly being used as indicators of climate change impacts in ecosystems. For this purpose, it is necessary to use methods that can be applied to large areas with different types of vegetation, including vulnerable semiarid ecosystems that exhibit high spatial variability and low signal-to-noise ratio in seasonality. In this work, we evaluated the use of hidden Markov models (HMM) to extract phenological parameters from Moderate Resolution Imaging Spectroradiometer (MODIS) derived Normalized Difference Vegetation Index (NDVI). We analyzed NDVI time-series data for the period 2000–2018 across a range of land cover types in Southeast Spain, including rice croplands, shrublands, mixed pine forests, and semiarid steppes. Start of Season (SOS) and End of Season (EOS) metrics derived from HMM were compared with those obtained using well-established smoothing methods. When a clear and consistent seasonal variation was present, as was the case in the rice croplands, and when adjusting average curves, the smoothing methods performed as well as expected, with HMM providing consistent results. When spatial variability was high and seasonality was less clearly defined, as in the semiarid shrublands and steppe, the performance of the smoothing methods degraded. In these cases, the results from HMM were also less consistent, yet they were able to provide pixel-wise estimations of the metrics even when comparison methods did not.

Highlights

  • Land Surface Phenology (LSP), the seasonal pattern of variation in vegetated land surfaces observed from remote sensing [1,2], has been proven in the last decades to be a basic tool to investigate climate change impacts in ecosystems (e.g., References [3,4,5])

  • We evaluated the use of hidden Markov models (HMM) to extract phenological parameters from Moderate Resolution Imaging Spectroradiometer (MODIS) derived Normalized Difference Vegetation Index (NDVI)

  • The results presented in this paper strongly support the potential of HMM as an alternative or complementary method for deriving LSP metrics, opening new lines of research and possible improvements by using many of the variants and extensions of the basic type of HMM used in this work

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Summary

Introduction

Land Surface Phenology (LSP), the seasonal pattern of variation in vegetated land surfaces observed from remote sensing [1,2], has been proven in the last decades to be a basic tool to investigate climate change impacts in ecosystems (e.g., References [3,4,5]). The availability of long time series of vegetation indices derived from different space-borne sensors has allowed for the description of phenology metrics at global, regional, or local scales, and to analyze their spatio-temporal changes in relation to climate trends and human or natural disturbances (e.g., References [4,5,6,7,8,9,10,11,12,13,14]). In the field of remote sensing, the use of HMM has been mainly restricted to image analysis and landscape classification [45,46,47,48,49,50,51,52,53]

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