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

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 5 4229–54). 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.

[1]  D. Walker,et al.  Cumulative Impacts of Oil Fields on Northern Alaskan Landscapes , 1987, Science.

[2]  C. Tucker,et al.  Dynamics of aboveground phytomass of the circumpolar Arctic tundra during the past three decades , 2012 .

[3]  D. Stow,et al.  Greenness trends of Arctic tundra vegetation in the 1990s: comparison of two NDVI data sets from NOAA AVHRR systems , 2007 .

[4]  Paul Treitz,et al.  Remote Sensing of Arctic Vegetation: Relations between the NDVI, Spatial Resolution and Vegetation Cover on Boothia Peninsula, Nunavut , 2009 .

[5]  R. Kauth,et al.  The tasselled cap - A graphic description of the spectral-temporal development of agricultural crops as seen by Landsat , 1976 .

[6]  Steven F. Oberbauer,et al.  Plot-scale evidence of tundra vegetation change and links to recent summer warming. , 2012 .

[7]  Guido Grosse,et al.  Hydrogeomorphic processes of thermokarst lakes with grounded‐ice and floating‐ice regimes on the Arctic coastal plain, Alaska , 2011 .

[8]  Vladimir E. Romanovsky,et al.  Permafrost thermal state in the polar Northern Hemisphere during the international polar year 2007–2009: a synthesis , 2010 .

[9]  Guido Grosse,et al.  Modern thermokarst lake dynamics in the continuous permafrost zone, northern Seward Peninsula, Alaska , 2011 .

[10]  Anna Liljedahl,et al.  Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology , 2016 .

[11]  Douglas Stow,et al.  The relationship between tussock tundra spectral reflectance properties and biomass and vegetation composition , 1993 .

[12]  Gaku Kudo,et al.  Global assessment of experimental climate warming on tundra vegetation: heterogeneity over space and time. , 2012, Ecology letters.

[13]  W. Gould,et al.  Phytomass, LAI, and NDVI in northern Alaska: Relationships to summer warmth, soil pH, plant functional types, and extrapolation to the circumpolar Arctic , 2003 .

[14]  M. Torre Jorgenson,et al.  Abrupt increase in permafrost degradation in Arctic Alaska , 2006 .

[15]  E. Crist A TM Tasseled Cap equivalent transformation for reflectance factor data , 1985 .

[16]  Dana R. N. Brown,et al.  Role of ground ice dynamics and ecological feedbacks in recent ice wedge degradation and stabilization , 2015 .

[17]  S. Goetz,et al.  Shrub expansion in tundra ecosystems: dynamics, impacts and research priorities , 2011, Environmental Research Letters.

[18]  David L. Verbyla,et al.  Patterns of Change within a Tundra Landscape: 22-year Landsat NDVI Trends in an Area of the Northern Foothills of the Brooks Range, Alaska , 2013 .

[19]  Ingmar Nitze,et al.  Detection of landscape dynamics in the Arctic Lena Delta with temporally dense Landsat time-series stacks , 2016 .

[20]  D. Hopkins,et al.  Coastal morphology, coastal erosion, and barrier islands of the Beaufort Sea, Alaska , 1978 .

[21]  Guido Grosse,et al.  Recent Arctic tundra fire initiates widespread thermokarst development , 2015, Scientific Reports.

[22]  B. Markham,et al.  Summary of Current Radiometric Calibration Coefficients for Landsat MSS, TM, ETM+, and EO-1 ALI Sensors , 2009 .

[23]  D. Walker,et al.  Geobotanical Atlas of the Prudhoe Bay Region, Alaska , 1982 .

[24]  Mikhail Kanevskiy,et al.  Ground ice in the upper permafrost of the Beaufort Sea coast of Alaska , 2013 .

[25]  Robert H. Fraser,et al.  Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification , 2014, Remote. Sens..

[26]  J. Masek,et al.  The vegetation greenness trend in Canada and US Alaska from 1984–2012 Landsat data , 2016 .

[27]  D. A. Walker Height and growth rings of Salix lanata ssp. richardsonii along the coastal temperature gradient of northern Alaska , 1987 .

[28]  S. Goetz,et al.  Vegetation productivity patterns at high northern latitudes: a multi-sensor satellite data assessment , 2014, Global change biology.

[29]  D. Walker,et al.  Loess Ecosystems of Northern Alaska: Regional Gradient and Toposequence at Prudhoe Bay , 1991 .

[30]  Terry V. Callaghan,et al.  Global change and arctic ecosystems: is lichen decline a function of increases in vascular plant biomass? , 2001 .

[31]  Robert H. Fraser,et al.  Detecting long-term changes to vegetation in northern Canada using the Landsat satellite image archive , 2011 .

[32]  C. Tucker,et al.  A new estimate of tundra-biome phytomass from trans-Arctic field data and AVHRR NDVI , 2012 .

[33]  Niels Martin Schmidt,et al.  Climate sensitivity of shrub growth across the tundra biome , 2015 .

[34]  Mikhail Kanevskiy,et al.  Cumulative geoecological effects of 62 years of infrastructure and climate change in ice‐rich permafrost landscapes, Prudhoe Bay Oilfield, Alaska , 2014, Global change biology.

[35]  Limin Yang,et al.  Derivation of a tasselled cap transformation based on Landsat 7 at-satellite reflectance , 2002 .

[36]  R. Fraser,et al.  Warming-Induced Shrub Expansion and Lichen Decline in the Western Canadian Arctic , 2014, Ecosystems.

[37]  Donald A. Walker,et al.  A map analysis of patterned‐ground along a North American Arctic Transect , 2008 .

[38]  Zhaohua Chen,et al.  Propagation of errors associated with scaling foliage biomass from field measurements to remote sensing data over a northern Canadian national park , 2013 .

[39]  Donald A. Walker,et al.  Plant communities and soils in cryoturbated tundra along a bioclimate gradient in the Low Arctic, Alaska , 2005 .

[40]  C. Tweedie,et al.  High spatial resolution decade-time scale land cover change at multiple locations in the Beringian Arctic (1948–2000s) , 2012 .

[41]  B. Marcot,et al.  Projected changes in diverse ecosystems from climate warming and biophysical drivers in northwest Alaska , 2015, Climatic Change.

[42]  Compton J. Tucker,et al.  Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra , 2013, Remote. Sens..

[43]  Donald A. Walker,et al.  Plant communities of a tussock tundra landscape in the Brooks Range Foothills, Alaska , 1994 .

[44]  Alice Deschamps,et al.  A method for trend-based change analysis in Arctic tundra using the 25-year Landsat archive , 2011, Polar Record.

[45]  D. Walker,et al.  Spatial and Temporal Heterogeneity of Vegetation Properties among Four Tundra Plant Communities at Ivotuk, Alaska, U.S.A , 2005 .

[46]  Darrel L. Williams,et al.  Historical record of Landsat global coverage: mission operations, NSLRSDA, and International Cooperator stations , 2006 .