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A Numerical Study of the Relationship between the Carbon Cycle and the Land Surface Processes in the Northern Hemisphere Related to Recent El Ni?o Events

机译:与最近的厄尔尼诺事件相关的北半球碳循环与陆地表面过程关系的数值研究

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This study investigates the natural relationships between the carbon cycle andlandsurface processes in the Northern Hemisphere, relatedto recent El Ni?o events by a general circulation model with a Biosphere?Atmosphere Interaction Model Version 2 (BAIM2). Two cases are simulated; the periods of Case 1 and Case 2 are from 1996 to 2000 and from 2001 to 2005, respectively. Case 1 includedthe El Ni?o event from 1997 to 1998, andCase 2 includedthat from 2002 to 2003 in each simulation period. The physical and biological mechanisms of the relationship between the changes of landsurface processes with climate changes andvariations of CO_2 exchange between the atmosphere andterrestrial ecosystem are systematically examinedusing the results of direct simulation with a terrestrial biosphere-atmosphere fully coupledglobal climate model. In 1998 and2003, high surface temperature andlow soil wetness in the Eurasian Continent andNorth America occurredin the warm season in the Northern Hemisphere. These climate conditions are thought to have induced relatively low gross primary production and net ecosystem production values and contributed to anomalously high atmospheric CO_2 concentrations in these years. The results of this study suggest that there is a common feature in the relationship between the carbon cycle andlandsurface processes in the Northern Hemisphere, relatedto recent El Ni?o events. Specifically, an anomaly of the atmospheric circulation in the warm season in the Northern Hemisphere in the year El Ni?o event ends, which is most likely induced by the global teleconnection associatedwith the tropical sea surface temperature anomaly, causes an anomaly in the landsurface processes; this in turn induces anomalously low carbon absorption by the terrestrial ecosystem, which affects the variation of atmospheric CO_2 concentration growth rate.
机译:这项研究通过使用生物圈-大气相互作用模型第2版(BAIM2)的一般环流模型研究了北半球碳循环与地表过程之间的自然关系,这些过程与最近的厄尔尼诺事件有关。模拟了两种情况;案例1和案例2的期限分别是1996年至2000年和2001年至2005年。案例1包括1997年至1998年的El Ni?o事件,案例2包括每个模拟期间2002年至2003年的事件。利用直接与地球生物圈-大气完全耦合的全球气候模型进行模拟的结果,系统地研究了地表过程变化与气候变化以及大气与陆地生态系统之间CO_2交换变化之间关系的物理和生物学机制。 1998年和2003年,北半球暖季发生在欧亚大陆和北美,地表温度高,土壤湿度低。据认为,这些气候条件引起了相对较低的初级总产值和生态系统净产值,并导致这些年大气CO_2浓度异常升高。这项研究的结果表明,与最近的厄尔尼诺事件有关,北半球的碳循环与地表过程之间有一个共同的特征。具体来说,厄尔尼诺事件结束时北半球暖季的大气环流异常,很可能是由与热带海面温度异常有关的全球遥相关引起的,导致了地表过程异常;这反过来引起陆地生态系统异常低的碳吸收,从而影响了大气中CO_2浓度增长率的变化。

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