首页> 外文期刊>Tellus, Series B. Chemical and Physical Meteorology >Estimating regional terrestrial carbon fluxes for the Australian continent using a multiple-constraint approach I. Using remotely sensed data and ecological observations of net primary production
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Estimating regional terrestrial carbon fluxes for the Australian continent using a multiple-constraint approach I. Using remotely sensed data and ecological observations of net primary production

机译:使用多重约束方法估算澳大利亚大陆的区域陆地碳通量I.使用遥感数据和净初级生产的生态观测

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We have developed a modelling framework that synthesizes various types of field measurements at different spatial and temporal scales. We used this modelling framework to estimate monthly means and their standard deviations of gross photosynthesis, total ecosystem production, net primary production (NPP) and net ecosystem production (NEP) for eight regions of the Australian continent between 1990 and 1998. Annual mean NPP of the Australian continent varied between 800 and 1100 Mt C yr~(-1) between 1990 and 1998, with a coefficient of variation that is defined as the ratio of standard deviation and mean between 0.24 and 0.34. The seasonal variation of NPP for the whole continent varied between 50 and 110 Mt C month ~(-1) with two maxima, one in the autumn and another in the spring. NEP was most negative in the winter (a carbon sink) and was most positive (a carbon source) in the summer. However, the coefficient of variation of monthly mean NEP was very large (> 4), and consequently confidence in the predicted net carbon fluxes for any month in the period 1990-1998 for the whole continent was very low. A companion paper will apply atmospheric inverse technique to measurements of CO_2 concentration to further constrain the continental carbon cycle and reduce uncertainty in estimated mean monthly carbon fluxes.
机译:我们已经开发了一种建模框架,可以在不同的空间和时间尺度上综合各种类型的野外测量。我们使用此建模框架来估算1990年至1998年之间澳大利亚大陆八个地区的月均值及其总光合作用,总生态系统产量,净初级生产(NPP)和净生态系统产量(NEP)的标准偏差。澳大利亚大陆在1990年至1998年之间的变化范围为800至1100 Mt Cyr〜(-1),变化系数定义为标准偏差与平均值之比在0.24至0.34之间。整个大陆的NPP的季节变化在50至110 Mt C月〜(-1)之间变化,有两个最大值,一个在秋天,另一个在春天。 NEP在冬季最负(碳汇),而在夏季最正(碳源)。但是,月平均NEP的变化系数非常大(> 4),因此,整个大陆对1990-1998年期间任何月份的预测净碳通量的信心非常低。另一篇论文将应用大气逆技术来测量CO_2浓度,以进一步限制大陆碳循环并减少估计的平均每月碳通量的不确定性。

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