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Research Article

Temporal and spatial dynamics of phenology along the North–South Transect of Northeast Asia

, , , &
Pages 7922-7940 | Received 25 Jun 2018, Accepted 24 Feb 2019, Published online: 18 Apr 2019
 

ABSTRACT

Vegetation phenology is sensitive to climate change and, as such, is often regarded as an indicator of climate change. It is a common practice to extract vegetation phenological indicators based on satellite remote sensing data. In this study, we used the Advanced Very High Resolution Radiometer (AVHRR) Global Inventory Modeling and Mapping Study (GIMMS) Third-Generation normalized difference vegetation index (NDVI3G) to investigate temporal and spatial changes in phenology in Northeast Asia. Based on the maximum rate of change in the NDVI and dynamic threshold, we used the Asymmetric Gaussian model, Double Logistic method, and Savitzky-Golay filter to extract the start of the growing season (SOS), the end of the growing season (EOS), and the length of the growing season (LOS), respectively, along the North–South Transect of Northeast Asia (NSTNEA) from 1982 to 2014. We then compared the differences in SOS, EOS, and LOS and considered their spatio-temporal dynamics and relationship with temperature. The results show that the Asymmetric Gaussian model has the highest stability among the three methods. Dynamic thresholds corresponding to the maximum change rate of NDVI were mainly between 0.5 and 0.6. From 1982 to 2014, the SOS in the NSTNEA region occurred approximately 0.19 days earlier each year; the trends in EOS and LOS were not significant. In general, temperature and latitude have a strong linear relationship, both of which significantly impact vegetation phenology in the NSTNEA region. In addition, elevation also significantly impacts on vegetation phenology in the NSTNEA region.

Acknowledgements

We thank the NASA GIMMS team for providing the AVHRR GIMMS NDVI3G dataset, the Global Land Cover Facility for providing the MODIS Land Cover, and the European Centre for Medium-Range Weather Forecasts (ECMWF) for providing the ERA-Interim dataset. We appreciate anonymous referees for their valuable suggestions to make the manuscript better. This research was jointly supported by the National Natural Science Foundation of China (No. 41501212 & 41601442) and the fundamental research project of MOST (2005DKA32306).

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

This work was supported by the National Natural Science Foundation of China [41501212,41601442];the fundamental research project of MOST [2005DKA32306].

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