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Spatial and temporal variations of N_2O emissions from global forest and grassland ecosystems

机译:全球森林和草原生态系统的N_2O排放的空间和时间变化

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A process-based dynamic ecosystem model of TRIPLEX-GHG was used to estimate the spatial and temporal patterns of N_2O fluxes from global forest and grassland ecosystems under the effects of global warming and elevated CO_2 concentrations. From 1992 to2015, the estimated average N_20 emissions from forests and grasslands were 3.62 ± 0.16 Tg N yr~(-1), and 1.40 ± 0.03 Tg N yr~(-1), respectively. Tropical regions made large contributions (83.9% for forests and 74% for grasslands) to the total N_2O budgets, which were due to the larger N_20 flux values and large natural forest and grassland areas. The regional variations in N_2O emissions mainly resulted from the differences in the spatial distributions of climate characteristics, especially the precipitation patterns. In addition, anomalous years when N_2O emissions were relatively low/high were mainly due to the changes in climate patterns, which may have been induced by El Nino/La Nina events with different strengths and frequencies. Soil N_2O emissions from forests showed a positive effect on the atmospheric N_2O concentrations during June to November (R~2: 0.14-0.28), while those from grasslands showed a positive effect during the growing seasons (R~2: 0.17-0.28). Although natural N_2O sources(forests and grasslands in this study) showed slightly increasing trends, with 9.9 Gg N increment per year for forests and 2.1 Gg N increment per year for grasslands, they were not the main contributors to the elevated N_2O concentrations.
机译:基于过程的动态生态系统模型的Triplep-GHG用于估计全球森林和草原生态系统的N_2O助熔剂的空间和时间模式,在全球变暖和升高的CO_2浓度的影响下。从1992年到2015年,森林和草原的估计平均N_20排放量分别为3.62±0.16 Tg n Yr〜(-1),分别为1.40±0.03 tg n〜(-1)。热带地区为总N_2O预算制作了大量贡献(森林的83.9%,草原为74%),这是由于N_20助焊剂值和大型天然林和草原地区较大。 N_2O排放的区域变化主要是由于气候特征的空间分布的差异,尤其是降水模式。此外,当N_2O排放相对较低/高的异常年主要是由于气候模式的变化,这可能是由EL Nino / La Nina事件引起不同强度和频率的影响。森林的土壤N_2O排放对6月至11月的大气N_2O浓度显示出积极影响(R〜2:0.1.0.28),而来自草原的人在生长季节(R〜2:0.17-0.28)显示出积极效果。虽然天然N_2O来源(本研究中的森林和草原)表现出略微增加的趋势,但每年森林每年9.9 Gg增加,每年为2.1 Gg为草地增量,它们不是升高的N_2O浓度的主要贡献者。

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