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LAND COVER ANALYSIS ALONG SEMI-ARID TRANSECTS IN ASIA

机译:亚洲半干旱地区的土地覆盖分析

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The use of higher spatial scale land cover data for development of regional estimates of land cover types are improving our ability to estimate land use and ecosystem interactions with global climate change. The spatial pattern and area estimates developed using land cover maps estimated from the TM-1 km products will provide a more detailed description of land use and cover for extrapolation of ecosystem dynamics for regional analyses. Since AVHRR data are of low spatial resolution, the land cover types which are classified by AVHRR data need to be of large spatial scale to be picked up by this sensor. The 50~*50 km~2 land cover maps used by mesoscale climate analyses and some ecosystem analyses would have a better representation of the land cover pattern and area estimates for biogeochemical and water flux estimates using the TM-1 km derived products. The difficulty in differentiating small grains of the croplands and the grassland regions contributes to the bias, but the consistent fashion in which the cropland dominants are weighted by the IGBP Discover analysis is conspicuous in this region of Asia. This over-estimate of croplands can contribute to higher estimates of carbon emissions, gaseous N losses, and erosion estimates for this region of the world. The greater spatial heterogeneity of the land cover distribution displayed by the TM-1 km data for this region would result in different interactions with mesoscale climate patterns than those indicated by the IGBP Discover data set (Pielke et al. 1997, Fu and Wei 1993).
机译:使用更高空间尺度的土地覆盖数据来开发区域性土地覆盖类型的估计值,正在提高我们估计土地使用量和生态系统与全球气候变化相互作用的能力。使用从TM-1 km产品估算的土地覆盖图开发的空间格局和面积估算,将提供土地利用和覆盖的更详细描述,以便为区域分析外推生态系统动态。由于AVHRR数据的空间分辨率较低,因此按AVHRR数据分类的土地覆盖类型必须具有较大的空间比例,才能由该传感器采集。中尺度气候分析和某些生态系统分析使用的50〜* 50 km〜2土地覆盖图将更好地表示土地覆盖模式以及使用TM-1 km衍生产品估算的生物地球化学和水通量的面积估计。区分耕地和草地小颗粒的困难是造成这种偏见的原因,但是在该地区,以IGBP Discover分析加权耕地优势者的一贯方式是显而易见的。对耕地的这种高估可能会导致对世界上该地区的碳排放,气态氮损失和侵蚀估算进行更高的估算。与IGBP Discover数据集相比,TM-1 km数据显示的该地区更大的土地覆被分布空间异质性将导致与中尺度气候模式的相互作用(Pielke等,1997; Fu和Wei,1993)。 。

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