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作 者:赵德华[1] 李建龙[1] 齐家国[2] 范亚民[1]
机构地区:[1]南京大学生物系,南京210093 [2]美国密歇根州立大学地理系和全球变化-对地观测中心,密歇根州东兰辛市48823
出 处:《生态学报》2006年第8期2655-2662,共8页Acta Ecologica Sinica
基 金:南京大学人才引进启动资助项目(0208005122);江苏省自然科学基金重点预研项目联合资助项目(No.BK2005212)~~
摘 要:陆地生态系统碳平衡是全球变化科学中的核心问题之一,目前也是生态科学中的前沿与热点问题,而陆地生态系统的复杂性与不确定性决定了对陆地生态系统碳平衡估测的复杂性和不确定性。为研究这一复杂性问题,已发展了许多研究方法,可分为“自下而上”与“自上而下”两种,各种方法都有其自身的优势和劣势。相关方向也已经有了大量的研究报道,但是,不同的研究由于在方法、时间与空间尺度等存在的差异,使得许多研究结果和预测很难被有效的整合或适用于大范围甚至全球水平。综述了陆地碳平衡的主要研究方法,分析和比较了各方法的特点,指出在研究中对不同方法的结果进行分析和比较,以及采用综合方法的必要性。The continued increase in atmospheric carbon dioxide (CO2) due to anthropogenic emissions (mostly by fossil burning and land use and land cover change) is believed to have caused significant changes in global climate and biology. Because terrestrial ecosystems play an important but ambiguous role in the global carbon budget, a prime focus of much research in the global change studies is on the carbon accounting of the terrestrial ecosystems. Despite carbon sequestration by terrestrial ecosystems has been thought to occur predominantly in the Northern Hemisphere, the magnitude, longitudinal distribution and dynamics of carbon sinks remain uncertain. To fully balance carbon budget, uncertainties in estimating carbon sinks / sources must be quantified that include soll respiration variations with temperature, terrestrial responses to climate change, major disturbances in forest ecosystems, and total amount of sequestrations by the global oceans and terrestrial ecosystems. Most of these uncertainties mainly result from the complexity of terrestrial ecosystems. To reduce uncertainties in carbon budget estimation, many methods have been developed in the past several decades. However, these methods may not necessarily result in uncertainties reduction, instead, they often constrain the generality of carbon estimates. The purpose of this study is to provide comprehensive review of current methods, specifically focusing on terrestrial ecosystems. Eight methods commonly used in estimating terrestrial ecosystem carbon budget were reviewed with respects to their merits and limitations that include 1) the whole-plant or soil chamber method, 2) forest inventory, 3) the eddy covariance techniques, 4) plant-soil C isotopes techniques, 5) land use and land cover change, 6) process-based modeling, 7) atmospheric tracer-transport modeling, and 8) remote sensing techniques. These methods were divided into two groups, bottom-up (or land-based) and top-down (or atmosphere-based). Generally, the botto
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