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Constraining sources and sinks of carbon at the regional scale with aircraft observations.

机译:通过飞机观测来限制区域范围的碳源和碳汇。

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Anthropogenic perturbations to the carbon cycle have led to increasing atmospheric concentrations of the radiatively active species CO2. Quantitative knowledge of terrestrial carbon sources and sinks at the regional scale (102∼103 km)—the scale of political borders and ecosystems—remains highly uncertain. CO2 measurements have generally been collected in the remote marine boundary-layer, where signals of terrestrial fluxes have already been attenuated. CO2 concentrations over the continent contain strong terrestrial signals but exhibit large spatio-temporal variability that challenges current-generation analysis frameworks.; This dissertation seeks to address the current uncertainties in regional scale carbon sources and sinks. A quantitative characterization of the spatial variability of CO2 was carried out based on an extensive dataset compiled from aircraft observations over the Pacific and North America. The variability was used to determine the deviation between point observations and gridcell-averaged value used by models (“representation error”). The higher variability of continental CO2 led to significantly larger representation errors than over the ocean. The Stochastic Time-Inverted Lagrangian Transport (STILT) model was developed to resolve the variability in tracers like CO2 and minimize the representation error. STILT simulates atmospheric transport backward in time using particle ensembles starting from the locations of point observations that link the observations to upstream sources/sinks. Empirical assessments of time-reversibility revealed that mass violation in the wind fields led to time-irreversibility; backward-time results were identical to those from forward-time simulations when mass conserving winds were used.; The constraint on regional sources/sinks provided by continental CO 2 observations was explored in the CO2 Budget and Rectification Airborne (COBRA) pilot study. A receptor-oriented analysis framework which merges the regional scale atmospheric constraint with detailed information from ground-based measurements is presented. The STILT model was further applied as a flight planning tool during COBRA to predict locations of upstream air parcels and implement Lagrangian experiments, which minimized uncertainties in upstream tracer values and imposed direct constraints on regional scale fluxes.; The remaining limitations to the presented work and the necessary steps forward are discussed within the context of a general information transfer problem.
机译:人为干扰碳循环导致大气中放射性活性物质CO 2 的浓度增加。政治边界和生态系统的规模(10 2 〜10 3 km)在区域范围内陆地碳源和汇的定量知识仍然高度不确定。通常在偏远的海洋边界层收集了CO 2 测量值,在该边界层中,地面通量的信号已经被衰减。大陆上的CO 2 浓度包含强大的地面信号,但表现出较大的时空变化,这对当前的分析框架构成了挑战。本文旨在解决当前区域规模碳源和汇的不确定性。基于从太平洋和北美洲的飞机观测数据汇编而来的大量数据集,对CO 2 的空间变异性进行了定量表征。变异性用于确定点观测值与模型使用的网格单元平均值之间的偏差(“表示误差”)。大陆CO 2 的较高变异性导致比海洋上的代表误差大得多。建立了随机时间倒置拉格朗日运输模型(STILT),以解决CO 2 等示踪剂的变异性,并将表示误差降至最低。 STILT使用粒子集合从点观测的位置开始,将粒子观测连接到上游源/汇,从而模拟了大气向后传播的时间。对时间可逆性的经验评估表明,风场中的质量违规会导致时间不可逆。当使用质量守恒风时,后向结果与向前模拟的结果相同。在CO 2 机载预算和纠正整顿(COBRA)试点研究中,探索了大陆CO 2 观测对区域源/汇的限制。提出了一个面向受体的分析框架,该框架将区域尺度的大气限制与地面测量的详细信息融合在一起。 STILT模型在COBRA期间被进一步用作飞行计划工具,以预测上游空气包的位置并实施拉格朗日实验,从而最大程度地减少了上游示踪剂值的不确定性并直接限制了区域尺度通量。在一般的信息传输问题的背景下讨论了对提出的工作的其余限制和必要的前进步骤。

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