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Thermal-based modeling of coupled carbon, water, and energy fluxes using nominal light use efficiencies constrained by leaf chlorophyll observations

机译:基于名义光利用效率的碳,水和能量通量耦合的热模型建模,受叶绿素观测值的限制

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Recent studies have shown that estimates of leaf chlorophyll content (Chl),defined as the combined mass of chlorophyll a and chlorophyll b per unit leafarea, can be useful for constraining estimates of canopy light use efficiency(LUE). Canopy LUE describes the amount of carbon assimilated by a vegetativecanopy for a given amount of absorbed photosynthetically active radiation(APAR) and is a key parameter for modeling land-surface carbon fluxes. Acarbon-enabled version of the remote-sensing-based two-source energy balance(TSEB) model simulates coupled canopy transpiration and carbon assimilationusing an analytical sub-model of canopy resistance constrained by inputs ofnominal LUE (βn), which is modulated within the model in response tovarying conditions in light, humidity, ambient CO2 concentration, andtemperature. Soil moisture constraints on water and carbon exchange areconveyed to the TSEB-LUE indirectly through thermal infrared measurements ofland-surface temperature. We investigate the capability of using Chlestimates for capturing seasonal trends in the canopy βn from in situmeasurements of Chl acquired in irrigated and rain-fed fields of soybean andmaize near Mead, Nebraska. The results show that field-measured Chl isnonlinearly related to βn, with variability primarily related tophenological changes during early growth and senescence. Utilizing seasonallyvarying βn inputs based on an empirical relationship with in situmeasured Chl resulted in improvements in carbon flux estimates from the TSEBmodel, while adjusting the partitioning of total water loss between planttranspiration and soil evaporation. The observed Chl–βn relationshipprovides a functional mechanism for integrating remotely sensed Chl into theTSEB model, with the potential for improved mapping of coupled carbon, water,and energy fluxes across vegetated landscapes.
机译:最近的研究表明,对叶绿素含量(Chl)的估计(定义为每单位叶面积的叶绿素 a 和叶绿素 b 的总质量)可用于限制对天篷光的利用效率(LUE)。冠层LUE描述了给定数量的光合作用活性辐射(APAR)所吸收的植物冠层吸收的碳量,并且是模拟陆面碳通量的关键参数。基于遥感的两源能量平衡(TSEB)模型的启用碳的版本使用受名义LUE输入约束的冠层阻力分析子模型(β n < / i> ),它会根据光线,湿度,环境CO 2 浓度和温度的变化条件在模型中进行调制。土壤水分对水和碳交换的限制通过热红外测量地表温度间接传递给TSEB-LUE。我们研究了使用Chletimate捕获从内布拉斯加州米德(Mead)附近的大豆和玉米灌溉和雨养田中获得的Chl的原位测量捕获冠层β n 季节趋势的能力。结果表明,实测的Chl与β n 非线性相关,其变异性主要与早期生长和衰老过程中的物候变化有关。基于与实测Chl的经验关系使用季节性变化的β n 输入,可以改善TSEB模型的碳通量估算值,同时可以调节植物蒸腾作用和水分损失之间的总水分分配土壤蒸发。观测到的Chl–β n 关系为将遥感Chl整合到TSEB模型中提供了一种功能机制,具有改善植被间碳,水和能量通量的映射的潜力风景。

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