After applying the water body mask to both temperature images, we performed a change analysis on the water body temperatures. We saw greater temperature increases for inland bodies of water than nearshore. The temperature change difference map is overlaid on the NDVI difference map for the years 1999 and 2016. Despite the temperature increasing more inland, the vegetation experienced less growth than the nearshore vegetation where it was colder. The reason for this may be that as overall temperature increases, the nearshore permafrost is melting much more than before and allows for much more new vegetation growth than inland areas where vegetation competes for space. The inland vegetation reaches a peak of growth while the nearshore vegetation has more ability to grow. If temperature continues to rise in this region, eventually the nearshore vegetation will be capped at this peak just like the inland vegetation and the inland graminoid vegetation growth will resemble the nearshore vegetation growth. This will result in the maroon inland color moving out towards shore gradually.
Overall, there was a positive increase in vegetation in the entire region.