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首页> 外文期刊>Global change biology >Carbon dioxide exchange over multiple temporal scales in an arid shrub ecosystem near La Paz, Baja California Sur, Mexico.
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Carbon dioxide exchange over multiple temporal scales in an arid shrub ecosystem near La Paz, Baja California Sur, Mexico.

机译:在墨西哥下加利福尼亚州拉巴斯附近的干旱灌木生态系统中,二氧化碳在多个时间尺度上交换。

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摘要

Arid environments represent 30% of the global terrestrial surface, but are largely under-represented in studies of ecosystem carbon flux. Less than 2% of all FLUXNET eddy covariance sites exist in a hot desert climate. Long-term datasets of these regions are vital for capturing the seasonal and interannual variability that occur due to episodic precipitation events and climate change, which drive fluctuations in soil moisture and temperature patterns. The objectives of this study were to determine the meteorological variables that drive carbon flux on diel, seasonal, and annual scales and to determine how precipitation events control annual net ecosystem exchange (NEE). Patterns of NEE from 2002 to 2008 were investigated, providing a record with multiple replicates of seasons and conditions. Precipitation was extremely variable (55-339 mm) during the study period, and reduced precipitation in later years (2004-2008) appears to have resulted in annual moderate to large carbon sources (62-258 g C m-2 yr-1) in contrast to the previously reported sink (2002-2003). Variations in photosynthetically active radiation were found to principally drive variations in carbon uptake during the wet growing season while increased soil temperatures at a 5 cm depth stimulated carbon loss during the dry dormant season. Monthly NEE was primarily driven by soil moisture at a 5 cm depth, and years with a higher magnitude of precipitation events showed a longer growing season with annual net carbon uptake, whereas years with lower magnitude had drier soils and displayed short growing seasons with annual net carbon loss. Increased precipitation frequency was associated with increased annual NEE, which may be a function of increased microbial respiration to more small precipitation events. Annual precipitation frequency and magnitude were found to have effects on the interannual variability of NEE for up to 2 years.
机译:干旱环境占全球陆地面积的30%,但在生态系统碳通量研究中的代表性不足。在炎热的沙漠气候中,只有不到2%的FLUXNET涡流协方差站点存在。这些区域的长期数据集对于捕获由于突发性降水事件和气候变化而导致的季节性和年际变化至关重要,这些变化驱动了土壤水分和温度模式的波动。这项研究的目的是确定在diel,季节和年度尺度上驱动碳通量的气象变量,并确定降水事件如何控制年度净生态系统交换(NEE)。研究了2002年至2008年的NEE模式,该记录提供了多个季节和条件的重复记录。在研究期间,降水变化很大(55-339毫米),并且后期(2004-2008年)降水减少似乎导致了每年中等至较大的碳源(62-258 g C m -2 < / sup> yr -1 )与先前报告的接收器(2002-2003)相反。研究发现,光合作用辐射的变化主要驱动湿生季碳吸收的变化,而5 cm深度的土壤温度升高刺激了干旱休眠期的碳损失。每月的NEE主要是由5 cm深度的土壤水分驱动的,而降水事件幅度较大的年份表明其生长季节较长,且每年净吸收碳,而强度较低的年份则土壤较干燥,且生长季节较短,且每年的净碳含量较高。碳损失。降水频率的增加与年度NEE的增加有关,这可能是微生物对较小的降水事件的呼吸增加所致。发现年降水频率和强度对NEE的年际变化影响长达2年。

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