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    <responseDate>2026-10-15T21:47:18Z</responseDate>
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                <identifier>oai:data.mendeley.com/x8pdwgrykj.1</identifier>
                <datestamp>2019-10-18T06:46:04Z</datestamp>
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            <metadata><oai_dc:dc xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <dc:creator>sha, zongyao</dc:creator>
    <dc:title>Data for: How Much More Carbon Can Be Realistically Captured from Grassland Vegetation? Quantitative Assessment Using Focal Analysis on Soil-Topography-Vegetation Unit in the Inner Mongolia</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc:description>The data provided in this work were processed from five original datasets, including 1) soil map from the Harmonized World Soil Database (ver. 1.2) (http://www.fao.org/soils-portal), 2) topography data (DEM from http://earthexplorer.usgs.gov), 3) Climate dataset (http://cdc.cma.gov.cn), 4) vegetation type map (from http://www.nsii.org.cn/chinavegetaion), and 5) MODIS net primary productivity (NPP) (MODIS 17A3, http://e4ftl01.cr.usgs.gov/MOLT), which were downloaded for the Inner Mongolia Autonomous Region (IMAR) of China. The time window for most of the datasets was during 2000-2014. Topography, after classifying the DEM into three groups (&lt;500m, 500m~1500m, and &gt;1500m), and monthly precipitation and temperature data collected from about 680 weather stations from the climate dataset were applied to make climate grid maps at 1 km×1 km using an ANUSPLIN approach (Price et al., 2000). The climate grid maps were used to model potential NPP (PNPP) using the Miami NPP model (Adams et al., 2004; Gang et al., 2014; Lieth, 1973).  Tiles from MODIS 17A3 were mosaicked and taken to represent actual NPP (ANPP) of the grassland vegetation. A differential analysis between PNPP and ANPP at pixel level, was presented to represent a theoretical potential space in carbon capture. The maps of soil (S), topography (T), and vegetation (V) were overlaid to segment the area into spatially homogeneous S-T-V patches. Three types of focal statistics, including mean (Mean), maximum (Max), and 95% percentile threshold (95%PCT), of ANPP for each S-T-V unit were computed as the target level for ANPP. The gap from ANPP to each target level for each S-T-V patch was computed as being the practically realistic potential space. The gaps for the entire IMAR area were aggregated. The temporally averaged maps of the gaps derived from the pixel-based and focal analysis approaches along with ANPP and PNPP were provided. The temporal trajectories of spatially averaged gaps as well as ANPP and PNPP were illustrated. </dc:description>
    <dc:subject>Remote Sensing</dc:subject>
    <dc:subject>Grassland Ecosystem</dc:subject>
    <dc:subject>Climate Change</dc:subject>
    <dc:subject>Modelling</dc:subject>
    <dc:subject>Carbon Balance</dc:subject>
    <dc:contributor>Bai, Yongfei </dc:contributor>
    <dc:contributor>Lan, Hai </dc:contributor>
    <dc:contributor>Liu, Xuefeng </dc:contributor>
    <dc:contributor>Xie, Yichun </dc:contributor>
    <dc:type>Dataset</dc:type>
    <dc:identifier>doi:10.17632/x8pdwgrykj.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/x8pdwgrykj.1</dc:identifier>
    <dc:rights>Creative Commons Attribution 4.0 International</dc:rights>
    <dc:rights>http://creativecommons.org/licenses/by/4.0</dc:rights>
    <dc:relation>https://data.mendeley.com/datasets/x8pdwgrykj</dc:relation>
    <dc:date>2019-10-18T06:46:04Z</dc:date>
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