针对甘南草原生态系统水资源压力日益增大及草原退化的形势,本研究采用理论基础坚实、区域应用限制小、反演陆面蒸散发量较为合理准确的SEBS(Surface Energy Balance System)模型。在此基础上,将新一代对地观测数据MODIS应用于反演甘南...针对甘南草原生态系统水资源压力日益增大及草原退化的形势,本研究采用理论基础坚实、区域应用限制小、反演陆面蒸散发量较为合理准确的SEBS(Surface Energy Balance System)模型。在此基础上,将新一代对地观测数据MODIS应用于反演甘南草原区域地表蒸散发(Evapotranspiration,ET),并对甘南草原区域7月份的日均ET进行了反演,分析了2000年和2009年间该区域ET的时空分布格局和发展变化。同时,采用图像剖面线分形的方法描述研究区遥感ET的局部以及微观的结构特征,了解遥感ET分布的空间差异和变化趋势。研究表明:该区域日均ET总体上是减少的,其中一些区域变化幅度较大,减少了50%左右;其中,在地表水含量丰富的吉木都塘草原风景区和桑科草原风景区以及西库乎鹿场附近的黄河支流、尕海自然保护区、科才苦河、白龙江、拱坝河及洮河的水体周围,ET量才有7.00mm左右,主要与该区域水资源的减少有关。展开更多
Lund-Potsdam-Jena Dynamic Global Vegetation Model(LPJ)模型是由Lund University,Pots-dam Climate Research Centre和Max-Planck-Institute for Biogeochemistry,Jena联合开发的植被动态模型,该模型以气候、土壤质地和CO2数据作为...Lund-Potsdam-Jena Dynamic Global Vegetation Model(LPJ)模型是由Lund University,Pots-dam Climate Research Centre和Max-Planck-Institute for Biogeochemistry,Jena联合开发的植被动态模型,该模型以气候、土壤质地和CO2数据作为输入模拟植被与环境的碳水交换过程。为了利用高时间分辨率的输入数据,对模型的代码进行了改写。张掖绿洲盈科站位于干旱区绿洲典型的农田生态系统。应用其观测资料作为LPJ的输入,模拟了张掖绿洲制种玉米的碳水通量,并用涡动观测到的潜热和CO2通量验证蒸散发和NEE的模拟结果。结果表明LPJ模型能够较好地模拟制种玉米与环境之间的碳水交换,蒸散发(ET)的模拟值与观测值的R2为0.8;NEE的模拟值与观测值的R2为0.79。展开更多
论文基于估算NPP的CASA模型和估算ET的三角形模型对水分限制因子算法进行改进的基础上,构建了由NPP子模型和ET子模型组成的WUE遥感估算模型,以2010年相关MODIS影像和气象参量为数据源,实现了渭河流域WUE的估算,并对WUE的时空特征及其与...论文基于估算NPP的CASA模型和估算ET的三角形模型对水分限制因子算法进行改进的基础上,构建了由NPP子模型和ET子模型组成的WUE遥感估算模型,以2010年相关MODIS影像和气象参量为数据源,实现了渭河流域WUE的估算,并对WUE的时空特征及其与年内气温、降雨的关系进行了分析。研究表明:1)WUE模拟结果与通量观测数据以及生态系统模型模拟结果均具有一定的可比性,各模型模拟结果存在差异可能与WUE定义、模拟区域、使用数据源以及使用植被覆盖分类底图等存在差异有关;2)渭河流域WUE年内分布呈现微"双峰"型格局,以8月最高,春、夏、秋、冬四季WUE分别为0.57、1.05、0.66、0.12 g C·m-2·mm-1,呈现夏季>秋季>春季>冬季的特征;3)渭河流域WUE空间分布呈现子午岭、黄龙山、六盘山以及秦岭北坡等林区高,西安市建成区、子流域上游低植被覆盖区以及局部旱作农业区低的分异特征;4)渭河流域尺度上,WUE随年内气温和降雨的变化均呈现5阶段的变化特征,但变化形式存在差异。展开更多
The carbon and water cycle,an important biophysical process of terrestrial ecosystems,is changed by anthropogenic revegetation in arid and semiarid areas.However,there is still a lack of understanding of the mechanism...The carbon and water cycle,an important biophysical process of terrestrial ecosystems,is changed by anthropogenic revegetation in arid and semiarid areas.However,there is still a lack of understanding of the mechanisms of carbon and water coupling in intrinsic ecosystems in the context of human activities.Based on the CO,and H,O flux measurements of the desert steppe with the planted shrub Caragana liouana,this study explored the carbon and water flux coupling of the ecosystem by analyzing the variations in gross primary productivity(GPP),evapotranspiration(ET)and water use efficiency(WUE)and discussing the driving mechanisms of biological factors.The seasonal variation in climate factors induced a periodic variation pattern of biophysical traits and carbon and water fluxes.The GPP and ET fluctuated in seasons,but the WUE was relatively stable in the growing season.The GP,ET and WUE were significantly driven by global radiation(R,),temperature(T,and T),water vapor pressure deficit,leaf area index and plant water stress index(PWSI).However,R,temperature and PWSI were the most important factors regulating WUE.R,and temperature directly affected WUE with a positive effect but indirectly inhibited WUE by rising PWSl.Plant water stress inhibited photosynthesis and transpiration of the planted shrub community in the desert steppe.When the plant water stress exceeded a threshold(PWSI>0.54),the WUE would decrease since the GPP responded more quickly to the plant water stress than ET.Our findings suggest that policies related to large-scale carbon sequestration initiatives under afforestation must first fully consider the status of water consumption and WUE.展开更多
文摘针对甘南草原生态系统水资源压力日益增大及草原退化的形势,本研究采用理论基础坚实、区域应用限制小、反演陆面蒸散发量较为合理准确的SEBS(Surface Energy Balance System)模型。在此基础上,将新一代对地观测数据MODIS应用于反演甘南草原区域地表蒸散发(Evapotranspiration,ET),并对甘南草原区域7月份的日均ET进行了反演,分析了2000年和2009年间该区域ET的时空分布格局和发展变化。同时,采用图像剖面线分形的方法描述研究区遥感ET的局部以及微观的结构特征,了解遥感ET分布的空间差异和变化趋势。研究表明:该区域日均ET总体上是减少的,其中一些区域变化幅度较大,减少了50%左右;其中,在地表水含量丰富的吉木都塘草原风景区和桑科草原风景区以及西库乎鹿场附近的黄河支流、尕海自然保护区、科才苦河、白龙江、拱坝河及洮河的水体周围,ET量才有7.00mm左右,主要与该区域水资源的减少有关。
文摘Lund-Potsdam-Jena Dynamic Global Vegetation Model(LPJ)模型是由Lund University,Pots-dam Climate Research Centre和Max-Planck-Institute for Biogeochemistry,Jena联合开发的植被动态模型,该模型以气候、土壤质地和CO2数据作为输入模拟植被与环境的碳水交换过程。为了利用高时间分辨率的输入数据,对模型的代码进行了改写。张掖绿洲盈科站位于干旱区绿洲典型的农田生态系统。应用其观测资料作为LPJ的输入,模拟了张掖绿洲制种玉米的碳水通量,并用涡动观测到的潜热和CO2通量验证蒸散发和NEE的模拟结果。结果表明LPJ模型能够较好地模拟制种玉米与环境之间的碳水交换,蒸散发(ET)的模拟值与观测值的R2为0.8;NEE的模拟值与观测值的R2为0.79。
文摘论文基于估算NPP的CASA模型和估算ET的三角形模型对水分限制因子算法进行改进的基础上,构建了由NPP子模型和ET子模型组成的WUE遥感估算模型,以2010年相关MODIS影像和气象参量为数据源,实现了渭河流域WUE的估算,并对WUE的时空特征及其与年内气温、降雨的关系进行了分析。研究表明:1)WUE模拟结果与通量观测数据以及生态系统模型模拟结果均具有一定的可比性,各模型模拟结果存在差异可能与WUE定义、模拟区域、使用数据源以及使用植被覆盖分类底图等存在差异有关;2)渭河流域WUE年内分布呈现微"双峰"型格局,以8月最高,春、夏、秋、冬四季WUE分别为0.57、1.05、0.66、0.12 g C·m-2·mm-1,呈现夏季>秋季>春季>冬季的特征;3)渭河流域WUE空间分布呈现子午岭、黄龙山、六盘山以及秦岭北坡等林区高,西安市建成区、子流域上游低植被覆盖区以及局部旱作农业区低的分异特征;4)渭河流域尺度上,WUE随年内气温和降雨的变化均呈现5阶段的变化特征,但变化形式存在差异。
基金the National Natural Science Foundation of China(41967027)the Natural Science Foundation of Ningxia Province(2022AAC02011)+2 种基金the Excellent Talents Support Program of Ningxia Province(RQoo12)the Key Research and Development Program of Ningxia Province(2021BEG02010)the Special Plan for Local Sci-Tech Development Guided by the Central Government of China.
文摘The carbon and water cycle,an important biophysical process of terrestrial ecosystems,is changed by anthropogenic revegetation in arid and semiarid areas.However,there is still a lack of understanding of the mechanisms of carbon and water coupling in intrinsic ecosystems in the context of human activities.Based on the CO,and H,O flux measurements of the desert steppe with the planted shrub Caragana liouana,this study explored the carbon and water flux coupling of the ecosystem by analyzing the variations in gross primary productivity(GPP),evapotranspiration(ET)and water use efficiency(WUE)and discussing the driving mechanisms of biological factors.The seasonal variation in climate factors induced a periodic variation pattern of biophysical traits and carbon and water fluxes.The GPP and ET fluctuated in seasons,but the WUE was relatively stable in the growing season.The GP,ET and WUE were significantly driven by global radiation(R,),temperature(T,and T),water vapor pressure deficit,leaf area index and plant water stress index(PWSI).However,R,temperature and PWSI were the most important factors regulating WUE.R,and temperature directly affected WUE with a positive effect but indirectly inhibited WUE by rising PWSl.Plant water stress inhibited photosynthesis and transpiration of the planted shrub community in the desert steppe.When the plant water stress exceeded a threshold(PWSI>0.54),the WUE would decrease since the GPP responded more quickly to the plant water stress than ET.Our findings suggest that policies related to large-scale carbon sequestration initiatives under afforestation must first fully consider the status of water consumption and WUE.
