利用CASA模型模拟了西北植被净初级生产力(NPP)值,并结合地统计学理论,利用趋势分析及相关性分析研究了西北地区2000—2013年植被NPP时空变化特征,并结合气象数据探究了其对气候变化的响应。结果表明:(1)西北地区植被NPP在研究年限内呈...利用CASA模型模拟了西北植被净初级生产力(NPP)值,并结合地统计学理论,利用趋势分析及相关性分析研究了西北地区2000—2013年植被NPP时空变化特征,并结合气象数据探究了其对气候变化的响应。结果表明:(1)西北地区植被NPP在研究年限内呈现波动增加趋势,线性增加趋势达到极显著水平(p<0.01)。(2)植被NPP分布具有明显的空间异质性,整体呈现由东向西递减的趋势,除新疆外,其余省份也总体上表现为南高北低的分布格局。植被NPP呈现增加趋势的面积占总面积的85.97%,主要集中在陕西北部、宁夏南部、甘肃东部、青海的东部及南部和新疆西部部分地区,呈现减少趋势主要集中在新疆西部;不同植被类型NPP的均值呈现明显的差异,具体表现为:草地[262.16 g C/(m^2·a)]>灌丛[66.51 g C/(m^2·a)]>农田[45.90 g C/(m^2·a)]>森林[14.36 g C/(m^2·a)]。2000—2013年草地、农田及灌丛的NPP均呈现极显著增加趋势(p<0.01),而森林NPP的增加趋势不显著(p>0.05)。(3)总体上,西北地区植被NPP与气温、降水呈正相关,其对降水响应较为敏感,降水是限制西北地区植被NPP增加的主要因素。展开更多
Understanding the net primary productivity(NPP) of grassland is crucial to evaluate the terrestrial carbon cycle. In this study, we investigated the spatial distribution and the area of global grassland across the glo...Understanding the net primary productivity(NPP) of grassland is crucial to evaluate the terrestrial carbon cycle. In this study, we investigated the spatial distribution and the area of global grassland across the globe. Then, we used the Carnegie-Ames-Stanford Approach(CASA) model to estimate global grassland NPP and explore the spatio-temporal variations of grassland NPP in response to climate change from 1982 to 2008. Results showed that the largest area of grassland distribution during the study period was in Asia(1737.23 × 104 km^2), while the grassland area in Europe was relatively small(202.83 × 10~4 km^2). Temporally, the total NPP increased with fluctuations from 1982 to 2008, with an annual increase rate of 0.03 Pg C/yr. The total NPP experienced a significant increasing trend from 1982 to 1995, while a decreasing trend was observed from 1996 to 2008. Spatially, the grassland NPP in South America and Africa were higher than the other regions, largely as a result of these regions are under warm and wet climatic conditions. The highest mean NPP was recorded for savannas(560.10 g C/(m^2·yr)), whereas the lowest was observed in open shrublands with an average NPP of 162.53 g C/(m^2·yr). The relationship between grassland NPP and annual mean temperature and annual precipitation(AMT, AP, respectively) varies with changes in AP, which indicates that, grassland NPP is more sensitive to precipitation than temperature.展开更多
文摘利用CASA模型模拟了西北植被净初级生产力(NPP)值,并结合地统计学理论,利用趋势分析及相关性分析研究了西北地区2000—2013年植被NPP时空变化特征,并结合气象数据探究了其对气候变化的响应。结果表明:(1)西北地区植被NPP在研究年限内呈现波动增加趋势,线性增加趋势达到极显著水平(p<0.01)。(2)植被NPP分布具有明显的空间异质性,整体呈现由东向西递减的趋势,除新疆外,其余省份也总体上表现为南高北低的分布格局。植被NPP呈现增加趋势的面积占总面积的85.97%,主要集中在陕西北部、宁夏南部、甘肃东部、青海的东部及南部和新疆西部部分地区,呈现减少趋势主要集中在新疆西部;不同植被类型NPP的均值呈现明显的差异,具体表现为:草地[262.16 g C/(m^2·a)]>灌丛[66.51 g C/(m^2·a)]>农田[45.90 g C/(m^2·a)]>森林[14.36 g C/(m^2·a)]。2000—2013年草地、农田及灌丛的NPP均呈现极显著增加趋势(p<0.01),而森林NPP的增加趋势不显著(p>0.05)。(3)总体上,西北地区植被NPP与气温、降水呈正相关,其对降水响应较为敏感,降水是限制西北地区植被NPP增加的主要因素。
基金Under the auspices of Asia Pacific Network for Global Change Research(APN)Global Change Fund Project(No.ARCP2015-03CMY-Li)+2 种基金National Natural Science Foundation of China(No.41271361,41501575)National Key Research and Development Project(No.2018YFD0800201)Key Project of Chinese National Programs for Fundamental Research and Development(No.2010CB950702)
文摘Understanding the net primary productivity(NPP) of grassland is crucial to evaluate the terrestrial carbon cycle. In this study, we investigated the spatial distribution and the area of global grassland across the globe. Then, we used the Carnegie-Ames-Stanford Approach(CASA) model to estimate global grassland NPP and explore the spatio-temporal variations of grassland NPP in response to climate change from 1982 to 2008. Results showed that the largest area of grassland distribution during the study period was in Asia(1737.23 × 104 km^2), while the grassland area in Europe was relatively small(202.83 × 10~4 km^2). Temporally, the total NPP increased with fluctuations from 1982 to 2008, with an annual increase rate of 0.03 Pg C/yr. The total NPP experienced a significant increasing trend from 1982 to 1995, while a decreasing trend was observed from 1996 to 2008. Spatially, the grassland NPP in South America and Africa were higher than the other regions, largely as a result of these regions are under warm and wet climatic conditions. The highest mean NPP was recorded for savannas(560.10 g C/(m^2·yr)), whereas the lowest was observed in open shrublands with an average NPP of 162.53 g C/(m^2·yr). The relationship between grassland NPP and annual mean temperature and annual precipitation(AMT, AP, respectively) varies with changes in AP, which indicates that, grassland NPP is more sensitive to precipitation than temperature.
