首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Hydrologic profiling for greenhouse gas effluxes from natural grasslands in the prairie pothole region of Canada
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Hydrologic profiling for greenhouse gas effluxes from natural grasslands in the prairie pothole region of Canada

机译:加拿大大草原坑洼地区天然草地温室气体排放的水文特征分析

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The prairie pothole physiographic region of North America is likely to be affected by climate change, and it is important to establish its baseline global warming potential as a basis for assessing global change effects. This study estimated the hydrologic effects on soil greenhouse gas efflux during the growing season along hydrologic profiles within natural prairie potholes ranging from the southern to northern limits of the prairie pothole region within central Canada. Soil moisture was found to be an important driver of differences in soil efflux along the hydrologic profiles and along the south-to-north gradient. The position of peak cumulative soil efflux varied along the hydrologic profile, with the N_2O peak occurring at the backslope, the CO_2 peaks at footslope and toeslope, and the CH_4 peaks at toeslope and surface waters. When cumulative soil efflux was converted to global warming potential (Mg CO_2 eq), the largest values were restricted to the narrow land-water interface in the south but expanded to a broader area of the hillslope in the north. CO_2 was the major (> 95%) contributor to global warming potential. Omitting hydrologic controls on greenhouse gas fluxes from estimates of global warming potential led to substantial underestimates of the contributions of N_2O and CH _4. Arid regions in the south had smaller global warming potential than wetter regions in the north. If future climate projections for a warmer, drier climate in this region are realized, global warming potential from soil greenhouse gas fluxes will be smaller in this landscape, because the changing hydrologic conditions should result in a reduction of global warming potential from land surfaces, even as global warming potential from surface waters increases. Key Points topographically regulated hydrologic profiles exist in prairie potholeshydrologic profiles influence greenhouse gas flux emissionmodels that capture hydrologic profiles are more accurate
机译:北美的草原坑洼地域可能会受到气候变化的影响,因此必须确定其基准全球变暖潜力,以此作为评估全球变化影响的基础。这项研究估计了在生长季节,沿着加拿大中部大草原坑洼地区的南部到北部界限的自然大草原坑洼中的水文剖面对土壤温室气体外流的水文影响。发现土壤水分是沿着水文剖面和从南北向梯度变化的土壤外流的重要驱动力。累积土壤外排的峰值位置随水文剖面而变化,N_2O峰值出现在后坡,CO_2峰值出现在山坡和趾坡,CH_4峰值出现在坡面和地表水。当累积的土壤外排转化为全球变暖潜能(Mg CO_2当量)时,最大值局限于南部的狭窄水土界面,而扩展到北部的山坡区域。 CO_2是导致全球变暖潜力的主要因素(> 95%)。根据对全球变暖潜能的估计,省略了对温室气体通量的水文控制,从而大大低估了N_2O和CH _4的贡献。南部的干旱地区比北部的湿润地区具有较小的全球变暖潜力。如果实现该地区未来更温暖,更干燥气候的未来气候预测,那么在此景观中,土壤温室气体通量产生的全球变暖潜力将较小,因为不断变化的水文条件将导致陆地表面的全球变暖潜力减少,甚至随着地表水导致全球变暖的可能性增加。草原坑洼地水文剖面中存在地形调控水文剖面的关键因素影响温室气体通量排放模型

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