Environmental Research Letters (Jan 2016)

Increased wetness confounds Landsat-derived NDVI trends in the central Alaska North Slope region, 1985–2011

  • Martha K Raynolds,
  • Donald A Walker

DOI
https://doi.org/10.1088/1748-9326/11/8/085004
Journal volume & issue
Vol. 11, no. 8
p. 085004

Abstract

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Satellite data from the circumpolar Arctic have shown increases in vegetation indices correlated to warming air temperatures (e.g. Bhatt et al 2013 Remote Sensing http://dx.doi.org/10.3390/rs5094229 5 http://dx.doi.org/10.3390/rs5094229 http://10.3390/rs5094229 ). However, more information is needed at finer scales to relate the satellite trends to vegetation changes on the ground. We examined changes using Landsat TM and ETM+ data between 1985 and 2011 in the central Alaska North Slope region, where the vegetation and landscapes are relatively well-known and mapped. We calculated trends in the normalized difference vegetation index (NDVI) and tasseled-cap transformation indices, and related them to high-resolution aerial photographs, ground studies, and vegetation maps. Significant, mostly negative, changes in NDVI occurred in 7.3% of the area, with greater change in aquatic and barren types. Large reflectance changes due to erosion, deposition and lake drainage were evident. Oil industry-related changes such as construction of artificial islands, roads, and gravel pads were also easily identified. Regional trends showed decreases in NDVI for most vegetation types, but increases in tasseled-cap greenness (56% of study area, greatest for vegetation types with high shrub cover) and tasseled-cap wetness (11% of area), consistent with documented degradation of polygon ice wedges, indicating that increasing cover of water may be masking increases in vegetation when summarized using the water-sensitive NDVI.

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