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IMPACTS OF CLOUDS ON GPP AND ECOSYSTEM RESPIRATION OF CONTRASTING TERRESTRIAL ECOSYSTEMS

机译:云对GPP的影响以及对立陆地生态系统的生态系统呼吸

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摘要

The presence or absence of clouds in a region is a consequence of complex interactions among many atmospheric, oceanic and terrestrial processes. It is a physical expression of changes in a number of environmental factors, such as radiation, heat, temperature, moisture, precipitation, etc. All these factors are vital for the functioning of terrestrial ecosystems, and influence the exchange of energy and mass of terrestrial ecosystems with the overlying atmosphere. In particular, it has been observed that for many forest ecosystems, the maximal net uptake of carbon dioxide (CO_2) often occurs on cloudy rather than on sunny day. In a previous study, we showed that a boreal deciduous forest and a temperate deciduous forest had maximal carbon uptake under sky conditions with a solar radiation level equivalent to about 70-80% of the corresponding clear-sky solar irradiance. We also demonstrated that the two forests could tolerate a cloud-induced sunlight reduction of as much as 50% without lowering the capacity to sequester carbon as compared with sunny days (Gu et al. 1999). However, uncertainties remain in regard to the mechanism of this phenomenon. Since variations in net carbon uptake can be achieved through changes in photosynthesis, or respiration or both, an interesting question is: does moderate cloudiness increase net carbon uptake by enhancing canopy photosynthesis or by reducing ecosystem respiration or both? Canopy photosynthesis can be enhanced by increased diffuse radiation (Gu et al. 2002) or reduced water stress (Freedman et al. 2001). Ecosystem respiration can be reduced by decreased temperature under cloudy conditions. In this study, we have investigated the responses of contrasting terrestrial ecosystems to cloudiness by analyzing tower flux measurements. We have found that moderate cloudiness tends to enhance canopy photosynthesis. For the influences of clouds on ecosystem respiration, the responses are more complex. Some ecosystems show reduction in ecosystem respiration in the presence of clouds, but for others the response is weak. Possible explanations for this difference include temperature - moisture interactions on soil respiration.
机译:一个区域中是否存在云是许多大气,海洋和陆地过程之间复杂的相互作用的结果。它是多种环境因素(例如辐射,热量,温度,湿度,降水等)变化的物理表达。所有这些因素对于陆地生态系统的功能至关重要,并且会影响陆地能量和质量的交换上层大气的生态系统。尤其是,已经观察到,对于许多森林生态系统而言,二氧化碳(CO_2)的最大净吸收通常发生在阴天而不是晴天。在先前的研究中,我们显示了北方落叶性森林和温带落叶性森林在天空条件下具有最大的碳吸收量,太阳辐射水平相当于相应晴朗天空太阳辐照度的约70-80%。我们还证明,与晴天相比,这两个森林可以忍受由云引起的日照减少多达50%,而不会降低固存碳的能力(Gu等,1999)。但是,关于这种现象的机理仍存在不确定性。由于净碳吸收量的变化可以通过光合作用或呼吸作用或两者的变化来实现,因此一个有趣的问题是:适度的混浊是否通过增强冠层的光合作用或通过减少生态系统呼吸作用或两者来增加净碳吸收量?冠层的光合作用可以通过增加散射辐射(Gu等,2002)或减少水分胁迫(Freedman等,2001)来增强。多云条件下温度降低可以减少生态系统的呼吸。在这项研究中,我们通过分析塔通量测量研究了对比的陆地生态系统对多云的响应。我们发现适度的混浊倾向于增强冠层的光合作用。由于云对生态系统呼吸的影响,响应更加复杂。一些生态系统在有云的情况下显示出生态系统呼吸的减少,但对其他生态系统的响应却很弱。这种差异的可能解释包括温度-水分对土壤呼吸的相互作用。

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