利用多源数据估算黑河流域总初级生产力

总初级生产力(GPP)决定了进入陆地生态系统的初始物质与能量,但由MODIS GPP产品获取的GPP在地表覆盖复杂的黑河流域却不足以准确的反映生态系统物质与能量的分布。因此,利用MODIS影像数据、ASTER GDEM数据、30 m分辨率土地利用覆被数据和中国区域地面气象要素驱动数据,驱动VPM模型模拟黑河流域2015年5～10月的总初级生产力,并据此揭示黑河流域GPP在生长季的时空格局,时间分辨率为8 d,空间分辨率为500 m。研究结果表明:VPM模型估算结果的精度高于MODIS GPP产品,判定系数增长了45.5%,总均方根误差降低了57.0%;黑河流域生长季累积GPP总体呈现出中游最高、上游其次、下游最低的显著空间分布梯度格局;全境与局部有植被覆盖区域的日GPP均呈先增加后减少倒U型变化规律,且前者在7月下旬达到最高值;植被覆盖率极低的地表区域生长季内的日GPP在基本稳定中上下波动,稳定值处于1 gC·m^-2·d^-1附近。

Estimating gross primary production in the Heihe RiverBasin from multiple data sources

The initial matter and energy entering terrestrialecosystem are determined by the gross primary productivity (GPP).Hovexer,the GPP measurements acquired by the MODIS[WTBX]GPP[WTBZ] products are not sufficient to accurately reflect thedistribution of ecosystem matter and energy in the Heihe River Basin in QinghaiProvince,Gansu Province and Inner Mongolia,China with complex surface coverage.Therefore,basedon MODIS image data,ASTER GDEM data,land cover data with a spatial resolutionof 30 m,and the China Meteorological Forcing Dataset,the VPM model was derivedto simulate the gross primary productivity of the Heihe River Basin from May toOctober 2015 with a spatial resolution of 500 m and a temporal resolution of 8days.Based on simulations using the VPM model,the spatial and temporal patternsof GPP in the Heihe River Basinduring the growing season were determined．The results of the studyindicate that the accuracy of the results estimated using the VPM model washigher than that of the MODIS GPP products.The judgment coefficient increased by 45.5%,while the total root meansquare error reduced by 57.0%.The study results also demonstrate that the GPP accumulation during the growingseason in the Heihe River Basin exhibited a significant spatial distributiongradient pattern,which can be described as the highest in the middlereaches,the next highest in the upper reaches,and the lowest in the lowerreaches.In addition,the daily GPP ofthe whole and partial vegetation-coveredareas in the Heihe River Basin first increased and then decreased in aninverted U-shape.The daily GPP values of all vegetation covered areas reached themaximum in late July.The daily GPP values of those ground areas with very low vegetation coverage fluctuated upand down in their basic stability,while the stable value was approximately 1 gC·m^-1·d^-1.