A comparison of multi-spectral, multi-angular, and multi-temporal remote sensing datasets for fractional shrub canopy mapping in Arctic Alaska

Abstract Shrub cover appears to be increasing across many areas of the Arctic tundra biome, and increasing shrub cover in the Arctic has the potential to significantly impact global carbon budgets and the global climate system. For most of the Arctic, however, there is no existing baseline inventory of shrub canopy cover, as existing maps of Arctic vegetation provide little information about the density of shrub cover at a moderate spatial resolution across the region. Remotely-sensed fractional shrub canopy maps can provide this necessary baseline inventory of shrub cover. In this study, we compare the accuracy of fractional shrub canopy (> 0.5 m tall) maps derived from multi-spectral, multi-angular, and multi-temporal datasets from Landsat imagery at 30 m spatial resolution, Moderate Resolution Imaging SpectroRadiometer (MODIS) imagery at 250 m and 500 m spatial resolution, and MultiAngle Imaging Spectroradiometer (MISR) imagery at 275 m spatial resolution for a 1067 km2 study area in Arctic Alaska. The study area is centered at 69 °N, ranges in elevation from 130 to 770 m, is composed primarily of rolling topography with gentle slopes less than 10°, and is free of glaciers and perennial snow cover. Shrubs > 0.5 m in height cover 2.9% of the study area and are primarily confined to patches associated with specific landscape features. Reference fractional shrub canopy is determined from in situ shrub canopy measurements and a high spatial resolution IKONOS image swath. Regression tree models are constructed to estimate fractional canopy cover at 250 m using different combinations of input data from Landsat, MODIS, and MISR. Results indicate that multi-spectral data provide substantially more accurate estimates of fractional shrub canopy cover than multi-angular or multi-temporal data. Higher spatial resolution datasets also provide more accurate estimates of fractional shrub canopy cover (aggregated to moderate spatial resolutions) than lower spatial resolution datasets, an expected result for a study area where most shrub cover is concentrated in narrow patches associated with rivers, drainages, and slopes. Including the middle infrared bands available from Landsat and MODIS in the regression tree models (in addition to the four standard visible and near-infrared spectral bands) typically results in a slight boost in accuracy. Including the multi-angular red band data available from MISR in the regression tree models, however, typically boosts accuracy more substantially, resulting in moderate resolution fractional shrub canopy estimates approaching the accuracy of estimates derived from the much higher spatial resolution Landsat sensor. Given the poor availability of snow and cloud-free Landsat scenes in many areas of the Arctic and the promising results demonstrated here by the MISR sensor, MISR may be the best choice for large area fractional shrub canopy mapping in the Alaskan Arctic for the period 2000–2009.

[1]  Collin G. Homer,et al.  Multiscale sagebrush rangeland habitat modeling in southwest Wyoming , 2009 .

[2]  J. Townshend,et al.  Global Percent Tree Cover at a Spatial Resolution of 500 Meters: First Results of the MODIS Vegetation Continuous Fields Algorithm , 2003 .

[3]  Roger A. Pielke,et al.  Land–atmosphere energy exchange in Arctic tundra and boreal forest: available data and feedbacks to climate , 2000, Global change biology.

[4]  J. Muller,et al.  New directions in earth observing: Scientific applications of multiangle remote sensing , 1999 .

[5]  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 .

[6]  F. Stuart Chapin,et al.  Responses of Arctic Tundra to Experimental and Observed Changes in Climate , 1995 .

[7]  M. MacKenzie,et al.  Effects of sensor spatial resolution on landscape structure parameters , 1995, Landscape Ecology.

[8]  C. Tucker Red and photographic infrared linear combinations for monitoring vegetation , 1979 .

[9]  A. J. Richardsons,et al.  DISTINGUISHING VEGETATION FROM SOIL BACKGROUND INFORMATION , 1977 .

[10]  Donald A. Walker,et al.  Landsat MSS-derived land-cover map of northern Alaska: Extrapolation methods and a comparison with photo-interpreted and AVHRR-derived maps , 1999 .

[11]  Bruce T. Milne,et al.  Effects of changing spatial scale on the analysis of landscape pattern , 1989, Landscape Ecology.

[12]  Limin Yang,et al.  Development of a global land cover characteristics database and IGBP DISCover from 1 km AVHRR data , 2000 .

[13]  J. Ross Quinlan,et al.  C4.5: Programs for Machine Learning , 1992 .

[14]  Bernard Pinty,et al.  Multi-angle Imaging SpectroRadiometer (MISR) instrument description and experiment overview , 1998, IEEE Trans. Geosci. Remote. Sens..

[15]  J. Martonchik,et al.  Large area mapping of southwestern forest crown cover, canopy height, and biomass using the NASA Multiangle Imaging Spectro-Radiometer , 2008 .

[16]  M. Sturm,et al.  Climate change: Increasing shrub abundance in the Arctic , 2001, Nature.

[17]  F. E. Nicodemus,et al.  Geometrical considerations and nomenclature for reflectance , 1977 .

[18]  C. Tucker,et al.  North American vegetation patterns observed with the NOAA-7 advanced very high resolution radiometer , 1985, Vegetatio.

[19]  David P. Roy,et al.  MODIS land data storage, gridding, and compositing methodology: Level 2 grid , 1998, IEEE Trans. Geosci. Remote. Sens..

[20]  Limin Yang,et al.  COMPLETION OF THE 1990S NATIONAL LAND COVER DATA SET FOR THE CONTERMINOUS UNITED STATES FROM LANDSAT THEMATIC MAPPER DATA AND ANCILLARY DATA SOURCES , 2001 .

[21]  Anne W. Nolin,et al.  Towards retrieval of forest cover density over snow from the Multi‐angle Imaging SpectroRadiometer (MISR) , 2004 .

[22]  T. Painter,et al.  Reflectance quantities in optical remote sensing - definitions and case studies , 2006 .

[23]  Thomas H. Painter,et al.  Time-space continuity of daily maps of fractional snow cover and albedo from MODIS , 2008 .

[24]  F. Stuart Chapin,et al.  Summer Differences among Arctic Ecosystems in Regional Climate Forcing , 2000 .

[25]  Steven F. Oberbauer,et al.  Plant community responses to experimental warming across the tundra biome , 2006, Proceedings of the National Academy of Sciences of the United States of America.

[26]  Alan R. Gillespie,et al.  Vegetation in deserts. I - A regional measure of abundance from multispectral images. II - Environmental influences on regional abundance , 1990 .

[27]  Donald A. Walker,et al.  The Circumpolar Arctic vegetation map , 2005 .

[28]  Guoqing Sun,et al.  Assessing tundra–taiga boundary with multi-sensor satellite data , 2004 .

[29]  Janne Heiskanen,et al.  Assessment of multispectral, -temporal and -angular MODIS data for tree cover mapping in the tundra-taiga transition zone , 2008 .

[30]  F. Chapin,et al.  Role of Land-Surface Changes in Arctic Summer Warming , 2005, Science.

[31]  J. Welker,et al.  Winter Biological Processes Could Help Convert Arctic Tundra to Shrubland , 2005 .

[32]  F. Messier,et al.  Hierarchical habitat selection by barren-ground grizzly bears in the central Canadian Arctic , 2002, Oecologia.

[33]  J. Chen,et al.  Retrieving Leaf Area Index of Boreal Conifer Forests Using Landsat TM Images , 1996 .

[34]  Bernard Pinty,et al.  Determination of land and ocean reflective, radiative, and biophysical properties using multiangle imaging , 1998, IEEE Trans. Geosci. Remote. Sens..

[35]  F. Chapin,et al.  Subgrid-scale variability in the surface energy balance , 1998 .

[36]  Jianguo Wu,et al.  The modifiable areal unit problem and implications for landscape ecology , 1996, Landscape Ecology.

[37]  Gregory P. Asner,et al.  Ecological Research Needs from Multiangle Remote Sensing Data , 1998 .

[38]  Alan H. Strahler,et al.  Global land cover mapping from MODIS: algorithms and early results , 2002 .

[39]  P. S. Chavez,et al.  Automatic detection of vegetation changes in the southwestern United States using remotely sensed images , 1994 .

[40]  Roger A. Pielke,et al.  Modelled changes in arctic tundra snow, energy and moisture fluxes due to increased shrubs , 2002 .

[41]  Roselyne Lacaze,et al.  Retrieval of vegetation clumping index using hot spot signatures measured by POLDER instrument , 2002 .

[42]  G. Gutman,et al.  The derivation of the green vegetation fraction from NOAA/AVHRR data for use in numerical weather prediction models , 1998 .

[43]  Debra P. C. Peters,et al.  Support vector machines for recognition of semi-arid vegetation types using MISR multi-angle imagery , 2007 .

[44]  Thomas S. Pagano,et al.  Prelaunch characteristics of the Moderate Resolution Imaging Spectroradiometer (MODIS) on EOS-AM1 , 1998, IEEE Trans. Geosci. Remote. Sens..

[45]  Debra P. C. Peters,et al.  Mapping woody plant cover in desert grasslands using canopy reflectance modeling and MISR data , 2006 .

[46]  Eric C. Brown de Colstoun,et al.  Improving global scale land cover classifications with multi-directional POLDER data and a decision tree classifier , 2006 .

[47]  W. Oechel,et al.  Energy and trace-gas fluxes across a soil pH boundary in the Arctic , 1998, Nature.

[48]  R. Lacaze,et al.  Global mapping of vegetation parameters from POLDER multiangular measurements for studies of surface-atmosphere interactions: A pragmatic method and its validation , 2002 .

[49]  Robert M. Haralick,et al.  Textural Features for Image Classification , 1973, IEEE Trans. Syst. Man Cybern..

[50]  M. Sturm,et al.  The evidence for shrub expansion in Northern Alaska and the Pan‐Arctic , 2006 .

[51]  Ranga B. Myneni,et al.  The impact of gridding artifacts on the local spatial properties of MODIS data : Implications for validation, compositing, and band-to-band registration across resolutions , 2006 .

[52]  F. Gao,et al.  Detecting vegetation structure using a kernel-based BRDF model , 2003 .

[53]  C. Woodcock,et al.  The factor of scale in remote sensing , 1987 .