Modeling Net Ecosystem Exchange for Grassland in Central Kazakhstan by Combining Remote Sensing and Field Data
Propastin, Pavel
Kappas, Martin
1, 3: 159 - 183
DOI: https://doi.org/10.3390/rs1030159
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/6808
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/6808
Propastin, Pavel; Kappas, Martin, 2009: Modeling Net Ecosystem Exchange for Grassland in Central Kazakhstan by Combining Remote Sensing and Field Data. In: Propastin, Pavel; Kappas, Martin (2009): Modeling Net Ecosystem Exchange for Grassland in Central Kazakhstan by Combining Remote Sensing and Field Data, DOI: 10.3390/rs1030159.
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Carbon sequestration was estimated in a semi-arid grassland region in Central
Kazakhstan using an approach that integrates remote sensing, field measurements and
meteorological data. Carbon fluxes for each pixel of 1 × 1 km were calculated as a product
of photosynthetically active radiation (PAR) and its fraction absorbed by vegetation
(fPAR), the light use efficiency (LUE) and ecosystem respiration (Re). The PAR is
obtained from a mathematical model incorporating Earth-Sun distance, solar inclination,
solar elevation angle, geographical position and cloudiness information of localities. The
fPAR was measured in field using hemispherical photography and was extrapolated to
each pixel by combination with the Normalized Difference Vegetation Index (NDVI)
obtained by the Vegetation instrument on board the Satellite Pour l’Observation de la Terra
(SPOT) satellite. Gross Primary Production (GPP) of the aboveground and belowground
vegetation of 14 sites along a 230 km west-east transect within the study region were
determined at the peak of growing season in different land cover types and linearly related
to the amount of PAR absorbed by vegetation (APAR). The product of this relationship is
LUE = 0.61 and 0.97 g C/MJ APAR for short grassland and steppe, respectively. The Re is
estimated using complex models driven by climatic data. Growing season carbon
sequestration was calculated for the modelling year of 2004. Overall, the short grassland
was a net carbon sink, whereas the steppe was carbon neutral. The evaluation of the
modelled carbon sequestration against independent reference data sets proved high
accuracy of the estimations.
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