4.7 Article

Changes in different land cover areas and NDVI values in northern latitudes from 1982 to 2015

Journal

ADVANCES IN CLIMATE CHANGE RESEARCH
Volume 12, Issue 4, Pages 456-465

Publisher

KEAI PUBLISHING LTD
DOI: 10.1016/j.accre.2021.04.003

Keywords

Air temperature; Arctic; Climate change; Precipitation; NDVI

Funding

  1. National Key Research and Development Program of China [2020YFA0608501, 2019YFA0607003]
  2. National Natural Science Foundation of China [41941015, 32061143032, 41961144021]
  3. State Key Laboratory of Cryospheric Science [SKLCS-ZZ-2021]
  4. West Light Foundation of the Chinese Academy of Sciences
  5. Swedish Research Council FORMAS [2016-01201]
  6. Swedish National Space Agency [209/19]
  7. Russian Fund for Basic Research [N 18-05-60080, AAAA-A16-116032810095-6]
  8. Formas [2016-01201] Funding Source: Formas

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Climate warming in the northern high-latitude regions has led to significant changes in land cover types, with shrubland and tree lines moving northwards, and different land cover types showing varying responses to climate change.
Climate warming leads to vast changes in the land cover types and plant biomass in the northern high-latitude regions . The overall trend is of shrubland and tree lines moving northwards, while changes in different land cover types and vegetation growth in response to climate change are largely unknown. Here, we selected land areas with latitudes higher than 50 degrees N as the study area. We compared the land cover type changes and explored relationships between the normalized difference vegetation index (NDVI) values of different land cover types, air temperature, and precipitation during 1982-2015 based on dynamic grid. The results indicated that forest and shrubland areas increased as a large area of grassland shifted to forest and shrubland. The snow/ice, tundra and grassland largely have decreased from 1982 to 2015. Although approximately 277.3 x 10(3) km(2) of barren land (6.2% of the total barren land area in 1982) changed to tundra, the tundra area still decreased because some tundra shifted to forest and grassland. The NDVI values of tundra significantly increased, but the shrubland showed a decreasing trend. Temperature in the growing season (June to September) showed the largest positive correlation coefficients with the NDVI values of forest, tundra, grassland, and cropland. However, due to shrubification processes and plant mortality in shrubland areas, the shrubland NDVI showed negative relationship with annual temperature but positively correlated with monthly t. Taken together, although there is large room for improvement of the land cover type data accuracy, our results suggested that the land cover types in high-latitude regions changed significantly, while the NDVI values of the different land cover types showed different responses to climate change.

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