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Impacts of droughts on carbon sequestration by China's terrestrial ecosystems from 2000 to 2011

机译:2000年至2011年干旱对中国陆地生态系统固碳的影响

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In recent years, China's terrestrial ecosystems have experienced frequentdroughts. How these droughts have affected carbon sequestration by theterrestrial ecosystems is still unclear. In this study, the process-basedBoreal Ecosystem Productivity Simulator (BEPS) model, driven by remotelysensed vegetation parameters, was employed to assess the effects of droughtson net ecosystem productivity (NEP) of terrestrial ecosystems in China from2000 to 2011. Droughts of differing severity, as indicated by a standardprecipitation index (SPI), hit terrestrial ecosystems in China extensively in2001, 2006, 2009, and 2011. The national total annual NEP exhibited theslight decline of ?11.3 Tg C yr?2 during the aforementioned years ofextensive droughts. The NEP reduction ranged from 61.1 Tg C yr?1 to168.8 Tg C yr?1. National and regional total NEP anomalies werecorrelated with the annual mean SPI, especially in Northwest China, NorthChina, Central China, and Southwest China. The reductions in annual NEP in2001 and 2011 might have been caused by a larger decrease in annual grossprimary productivity (GPP) than in annual ecosystem respiration (ER). Thereductions experienced in 2009 might be due to a decrease in annual GPP andan increase in annual ER, while reductions in 2006 could stem from a largerincrease in ER than in GPP. The effects of droughts on NEP lagged up to 3–6months, due to different responses of GPP and ER. In eastern China, where ishumid and warm, droughts have predominant and short-term lagged influences onNEP. In western regions, cold and arid, the drought effects on NEP wererelatively weaker but prone to lasting longer.
机译:近年来,中国陆地生态系统遭受了频繁的干旱。这些干旱如何影响陆地生态系统的固碳尚不清楚。在这项研究中,基于遥感的植被参数驱动的基于过程的北方生态系统生产力模拟器(BEPS)模型被用于评估2000年至2011年中国陆地生态系统的旱灾净生态系统生产力(NEP)的影响。根据标准降水指数(SPI)的数据,2001、2006、2009和2011年,中国的陆地生态系统受到了广泛的破坏。前几年的广泛干旱。 NEP降低范围为61.1 Tg C yr ?1 到168.8 Tg C yr ?1 。国家和地区的总NEP异常与年平均SPI相关,特别是在西北,华北,中部和西南地区。 2001年和2011年NEP的减少可能是由于年度总初级生产力(GPP)的下降幅度大于年度生态系统呼吸(ER)的幅度。 2009年出现的减少可能是由于年度GPP减少和年度ER的增加,而2006年的减少可能是由于ER的增长比GPP更大。由于GPP和ER的不同响应,干旱对NEP的影响滞后了3-6个月。在潮湿,温暖的华东地区,干旱对NEP产生了主要和短期的滞后影响。在寒冷和干旱的西部地区,干旱对NEP的影响相对较弱,但持续时间更长。

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