Disaggregation of LST over India: comparative analysis of different vegetation indices

ABSTRACT The non-availability of high-spatial-resolution thermal data from satellites on a consistent basis led to the development of different models for sharpening coarse-spatial-resolution thermal data. Thermal sharpening models that are based on the relationship between land-surface temperature (LST) and a vegetation index (VI) such as the normalized difference vegetation index (NDVI) or fraction vegetation cover (FVC) have gained much attention due to their simplicity, physical basis, and operational capability. However, there are hardly any studies in the literature examining comprehensively various VIs apart from NDVI and FVC, which may be better suited for thermal sharpening over agricultural and natural landscapes. The aim of this study is to compare the relative performance of five different VIs, namely NDVI, FVC, the normalized difference water index (NDWI), soil adjusted vegetation index (SAVI), and modified soil adjusted vegetation index (MSAVI), for thermal sharpening using the DisTrad thermal sharpening model over agricultural and natural landscapes in India. Multi-temporal LST data from Landsat-7 Enhanced Thematic Mapper Plus (ETM+) and Moderate Resolution Imaging Spectroradiometer (MODIS) sensors obtained over two different agro-climatic grids in India were disaggregated from 960 m to 120 m spatial resolution. The sharpened LST was compared with the reference LST estimated from the Landsat data at 120 m spatial resolution. In addition to this, MODIS LST was disaggregated from 960 m to 480 m and compared with ground measurements at five sites in India. It was found that NDVI and FVC performed better only under wet conditions, whereas under drier conditions, the performance of NDWI was superior to other indices and produced accurate results. SAVI and MSAVI always produced poorer results compared with NDVI/FVC and NDWI for wet and dry cases, respectively.

[1]  T. J. Majumdar,et al.  Surface temperature estimation in Singhbhum Shear Zone of India using Landsat-7 ETM+ thermal infrared data , 2009 .

[2]  Martha C. Anderson,et al.  Estimating subpixel surface temperatures and energy fluxes from the vegetation index-radiometric temperature relationship , 2003 .

[3]  Le Jiang,et al.  A methodology for estimation of surface evapotranspiration over large areas using remote sensing observations , 1999 .

[4]  Bo-Hui Tang,et al.  An application of the Ts–VI triangle method with enhanced edges determination for evapotranspiration estimation from MODIS data in arid and semi-arid regions: Implementation and validation , 2010 .

[5]  Feng Gao,et al.  A Data Mining Approach for Sharpening Thermal Satellite Imagery over Land , 2012, Remote. Sens..

[6]  B. Gao NDWI—A normalized difference water index for remote sensing of vegetation liquid water from space , 1996 .

[7]  James P. Verdin,et al.  A five‐year analysis of MODIS NDVI and NDWI for grassland drought assessment over the central Great Plains of the United States , 2007 .

[8]  William P. Kustas,et al.  A vegetation index based technique for spatial sharpening of thermal imagery , 2007 .

[9]  Peter M. Atkinson,et al.  Evaluating a thermal image sharpening model over a mixed agricultural landscape in India , 2011, Int. J. Appl. Earth Obs. Geoinformation.

[10]  Shunlin Liang,et al.  An improved method for estimating global evapotranspiration based on satellite determination of surface net radiation, vegetation index, temperature, and soil moisture , 2008, IGARSS 2008 - 2008 IEEE International Geoscience and Remote Sensing Symposium.

[11]  Paul D. Colaizzi,et al.  Utility of thermal sharpening over Texas high plains irrigated agricultural fields , 2007 .

[12]  V. Caselles,et al.  Mapping land surface emissivity from NDVI: Application to European, African, and South American areas , 1996 .

[13]  Muddu Sekhar,et al.  A simple model for spatial disaggregation of evaporative fraction: Comparative study with thermal sharpened land surface temperature data over India , 2013 .

[14]  A. Huete A soil-adjusted vegetation index (SAVI) , 1988 .

[15]  Okke Batelaan,et al.  valuation of the DisTrad thermal sharpening methodology for urban areas iesam , 2012 .

[16]  I. Sandholt,et al.  A simple interpretation of the surface temperature/vegetation index space for assessment of surface moisture status , 2002 .

[17]  A. Huete,et al.  A Modified Soil Adjusted Vegetation Index , 1994 .

[18]  P. Chavez Image-Based Atmospheric Corrections - Revisited and Improved , 1996 .

[19]  Julia A. Barsi,et al.  An Atmospheric Correction Parameter Calculator for a single thermal band earth-sensing instrument , 2003, IGARSS 2003. 2003 IEEE International Geoscience and Remote Sensing Symposium. Proceedings (IEEE Cat. No.03CH37477).

[20]  Inge Sandholt,et al.  Accuracy of the Temperature-Vegetation Dryness Index using MODIS under water-limited vs. energy-limited evapotranspiration conditions , 2014 .

[21]  K. P. Sudheer,et al.  Development and verification of a non-linear disaggregation method (NL-DisTrad) to downscale MODIS land surface temperature to the spatial scale of Landsat thermal data to estimate evapotranspiration , 2013 .