Processing of MODIS Data

25 to 0.7 mm that a canopy absorbs. MOD15A2 FPAR has 1 km resolution and provided in 8 day basis. MODIS FPAR are biophysical variables which describe canopy structure and are related to functional process rates of energy and mass exchange. MODIS FPAR have been used extensively as satellite derived parameters for calculation of surface photosynthesis and annual net primary production. These products are essential in calculating terrestrial energy, carbon, water cycle processes, and biogeochemistry of vegetation. For preprocessing the MODIS images in a format compatible with others software it was necessary to obtain software code from the US Geological Survey USGS http:LDPAAC.usgs.gov, which are available for different users‟ operating systems. In the case, we used software programs MODIS Reprojection Tool MRT. The MODIS Reprojection Tool is software designed to help individuals work with MODIS data by reprojecting MODIS images Level-2G, Level-3, and Level-4 land data products into more standard map projections. The main function of the MODIS Reprojection Tool is the resampler and mrtmosaic, executable programs that may be run either from the command-line or from the MRT Graphical User Interface GUI. Resampling is the mathematical technique used to create a new version of the image with a different width andor height in pixels. Increasing the size of an image is called up-sampling; reducing its size is called down-sampling. Many different resampling schemes are possible. Most techniques work by computing new pixels as a weighted average of the surrounding pixels. The weights depend on the distance between the new pixel location and the neighboring pixels. The simplest methods consider only the immediate neighbors; more advanced methods examine more of the surround pixels to attempt to produce a more accurate result. Following are the most common resampling methods:  Nearest neighbor: Each pixel in the output image receives its value from the nearest pixel in the input reference image.  Bilinear: Each estimated pixel value in the output image is based on a weighted average of the four nearest neighboring pixels in the input image. 26  Cubic convolution: Each estimated pixel value in the output image is based on a weighted average of 16 nearest neighboring pixels in the input image. Cubic convolution is the slowest method, but it yields the smoothest results Mosaicking images involves combining multiple images into a single composite image. The MRT provides a mosaic tool mrtmosaic for mosaicking tiles together prior to resampling. The mosaic tool requires that all input files are of the same product type and they must contain the same Scientific Data Set SDS names, SDS sizes number of lines and samples, SDS projection types and projection information, SDS pixel size, etc. If the SDS characteristics for each input tile do not match, then the mosaic tool will exit with an error. The mosaic tool requires an input parameter file which lists the full path and filename of each input file to be mosaicked. The input files can be listed in any order and the mosaic tool will determine how they fit together in the mosaic. The mosaic tool also requires an output filename. The file type of the output file must match that of the input files. Thus, if the input files are HDF-EOS then the output file extension must be .hdf. If the input files are raw binary then the output file extension must be .hdr.

3.4.4. Estimation of Net Primary Production

The approach for estimation NPP used NASA Carnegie Ames Stanford Approach CASA on the basis of light-use efficiency is conducted using relationship of monthly production of plant biomass is estimated as a product of time-varying surface solar irradiance S r and EVI from the MODIS satellite, plus a constant light utilization efficiency term e max that is modified by time-varying stress scalar terms for temperature T and moisture W effects. The equitation for estimation annually NPP values is : NPP = Sr EVI e max TW ………………………………………………… 14 Where : NPP = Net primary production gC m -2 year -1 27 Sr = Solar irradiance EVI = Enhanced Vegetation Index from MODIS e max = Constant Light Utilization Efficiency Term T = Optimal temperature for plant production W = Monthly water deficit The e max term is set uniformly at 0.39 g C MJ-1 PAR, a value that derives from calibration of predicted annual NPP to previous field estimates Potter et al., 1993. T is computed with reference to derivation of optimal temperatures T opt for plant production. W is estimated from monthly water deficits, based on a comparison of moisture supply precipitation and stored soil water to potential evapotranspiration PET. T and W value based on the estimation data from climatic data. The equitation for estimation monthly NPP values is : NPP = EVI e max FPAR TW …………………….………………… 15 NPP = Net primary production gC m -2 year -1 e max = Constant Light Utilization Efficiency Term EVI = Enhanced Vegetation Index from MODIS FPAR = Fraction Photosynthetically Active Radiation from MODIS T = Optimal temperature for plant production W = Monthly water deficit

3.4.5. Ground Truth

Ground truth refers to information that is collected on location. In remote sensing, this is especially important in order to relate image data to real features and materials on the ground. The collection of ground-truth data enables calibration of remote-sensing data, and aids in the interpretation and analysis of what is being sensed. More specifically, ground truth may refer to a process in which a pixel on a satellite image is compared to what is there in reality at the present time in order to verify the contents of the pixel on the image.