Analysis of the global vegetation dynamic metrics using MODIS Vegetation Index and land cover products

Climate change has important implications on the global distribution and dynamics of vegetation that, in turn, impacts the global carbon cycle. Irrespective of the forcings driving these changes, a characterization of global vegetation dynamics and the establishment of accurate metrics that can be linked to forcings are paramount to addressing questions related to climate change and its bearings on the terrestrial biosphere. Terrestrial ecosystems affect the climate through a complex system of interactions among water, carbon and energy. An increase, or decrease in these fluxes forces new equilibrium states and feedbacks to the climate system, which in turn impacts the ecosystems. NDVI-based time series analysis of satellite imagery from the NOAA-AVHRR sensor, collected during the last two decades narrates an enhanced vegetation activity over key areas of the Earth (high and mid latitudes). Most of this increase in activities has been indirectly linked to an increase in the Earth's temperature and CO2 concentration. In this study, we assessed the relationships between vegetation dynamic metrics and climate-ecosystem parameters. We analyzed 3 years of MODIS Vegetation Index (VI) data augmented by a global land cover map derived from the same sensor, and the GTOPO DEM data. Using a stratified spatial analysis, we assessed the role of the following characteristics on vegetation: 1) Latitude: to isolate temperature regimes and seasonality, 2) Elevation: to isolate land cover and precipitation distribution, 3) Land cover: to isolate phenological characteristics. A combinatorial analysis using the above stratification was applied in successive orders to generate compound results. The results yielded coherent time series profiles depicting vegetation dynamics as it relates to elevation, latitude and land cover

[1]  C. Tucker,et al.  Increased plant growth in the northern high latitudes from 1981 to 1991 , 1997, Nature.

[2]  Alan H. Strahler,et al.  The Moderate Resolution Imaging Spectroradiometer (MODIS): land remote sensing for global change research , 1998, IEEE Trans. Geosci. Remote. Sens..

[3]  Ranga B. Myneni,et al.  The interpretation of spectral vegetation indexes , 1995, IEEE Transactions on Geoscience and Remote Sensing.

[4]  C. J. Tucker,et al.  Relationship between atmospheric CO2 variations and a satellite-derived vegetation index , 1986, Nature.

[5]  D. Schimel,et al.  Terrestrial ecosystems and the carbon cycle , 1995 .

[6]  A. Huete,et al.  Overview of the radiometric and biophysical performance of the MODIS vegetation indices , 2002 .

[7]  C. D. Keeling,et al.  Increased activity of northern vegetation inferred from atmospheric CO2 measurements , 1996, Nature.

[8]  Ranga B. Myneni,et al.  Effect of orbital drift and sensor changes on the time series of AVHRR vegetation index data , 2000, IEEE Trans. Geosci. Remote. Sens..

[9]  C. Justice,et al.  Atmospheric correction of visible to middle-infrared EOS-MODIS data over land surfaces: Background, operational algorithm and validation , 1997 .

[10]  C. Tucker,et al.  Variations in northern vegetation activity inferred from satellite data of vegetation index during 1981 to 1999 , 2001 .

[11]  Ruth S. DeFries,et al.  Proportional estimation of land cover characteristics from satellite data , 1996, IGARSS '96. 1996 International Geoscience and Remote Sensing Symposium.

[12]  R. Myneni,et al.  The interpretation of spectral vegetation indexes , 1995 .

[13]  Thomas R. Loveland,et al.  The IGBP-DIS global 1 km land cover data set , 1997 .