首页> 外文期刊>Rangeland Ecology & Management >Climate-driven interannual variability in net ecosystem exchange in the Northern Great Plains grasslands. (Special Issue: Global grazinglands and greenhouse gas fluxes.)
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Climate-driven interannual variability in net ecosystem exchange in the Northern Great Plains grasslands. (Special Issue: Global grazinglands and greenhouse gas fluxes.)

机译:大平原北部草原地区气候驱动的净生态系统交换的年际变化。 (特刊:全球牧场和温室气体通量。)

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摘要

The Northern Great Plains grasslands respond differently under various climatic conditions; however, there have been no detailed studies investigating the interannual variability in carbon exchange across the entire Northern Great Plains grassland ecosystem. We developed a piecewise regression model to integrate flux tower data with remotely sensed data and mapped the 8-d and 500-m net ecosystem exchange (NEE) for the years from 2000 to 2006. We studied the interannual variability of NEE, characterized the interannual NEE difference in climatically different years, and identified the drought impact on NEE. The results showed that NEE was highly variable in space and time across the 7 yr. Specifically, NEE was consistently low (-35 to 32 g C.m-2 . yr-1) with an average annual NEE of -2+or-24 g C.m-2 . yr-1 and a cumulative flux of -15 g C.m-2. The Northern Great Plains grassland was a weak source for carbon during 2000-2006 because of frequent droughts, which strongly affected the carbon balance, especially in the Western High Plains and Northwestern Great Plains. Comparison of the NEE map with a drought monitor map confirmed a substantial correlation between drought and carbon dynamics. If drought severity or frequency increases in the future, the Northern Great Plains grasslands may become an even greater carbon source.
机译:大平原北部的草原在各种气候条件下的反应不同。然而,目前还没有详细的研究来研究整个大平原地区北部草地生态系统中碳交换的年际变化。我们开发了一个分段回归模型,以将通量塔数据与遥感数据相集成,并绘制了2000年至2006年的8-d和500-m净生态系统交换(NEE)。我们研究了NEE的年际变化,表征了年际变化。 NEE在气候不同的年份有所不同,并确定了干旱对NEE的影响。结果表明,在7年中,NEE的时空变化很大。具体来说,NEE一直很低(-35至32 g Cm -2 。yr -1 ),年平均NEE为-2+或-24 g Cm -2 。 yr -1 ,累积通量为-15 g C.m -2 。在2000-2006年期间,北部大平原草原是碳的薄弱来源,原因是干旱频发,严重影响了碳平衡,特别是在西部高平原和西北大平原。 NEE图与干旱监测图的比较证实了干旱与碳动力学之间的显着相关性。如果将来干旱的严重性或频率增加,大平原北部的草原可能会成为更大的碳源。

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