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Simulated Response Of Conterminous United States Ecosystems To Climate Change At Different Levels Of Fire Suppression, Co_2 Emission Rate, And Growth Response To Co_2

机译:在不同程度的灭火,Co_2排放率和对Co_2的生长响应水平下,美国本土生态系统对气候变化的模拟响应

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A modeling experiment was designed to investigate the impact of fire management, CO_2 emission rate, and the growth response to CO_2 on the response of ecosystems in the conterminous United States to climate scenarios produced by three different General Circulation Models (GCMs) as simulated by the MC1 Dynamic General Vegetation Model (DGVM). Distinct regional trends in response to projected climatic change were evident across all combinations of the experimental factors. In the eastern half of the U.S., the average response to relatively large increases in temperature and decreases in precipitation was an 11% loss of total ecosystem carbon. In the West, the response to increases in precipitation and relatively small increases in temperature was a 5% increase in total carbon stocks. Simulated fire suppression reduced average carbon losses in the East to about 6%, and preserved forests which were largely converted to woodland and savanna in the absence of fire suppression. Across the west, unsuppressed fire maintained near constant carbon stocks despite increases in vegetation productivity. With fire suppression, western carbon stocks increased by 10% and most shrublands were converted to woodland or even forest. With a relatively high level of growth in response to CO_2, total ecosystem carbon pools at the end of the century were on average about 9-10% larger in both regions of the U.S. compared to a low CO_2 response. The western U.S. gained enough carbon to counter losses from unsuppressed fire only with the high CO_2 response, especially in conjunction with the higher CO_2 emission rate. In the eastern U.S., fire suppression was sufficient to produce a simulated carbon sink only with both the high CO_2 response and emission rate. Considerable uncertainty exists with respect to the impacts of global warming on the ecosystems of the conterminous U.S., some of which resides in the future trajectory of greenhouse gas emissions, in the direct response of vegetation to increasing CO_2, and in future tradeoffs among different fire management options, as illustrated in this study.
机译:设计了一个模型实验,以研究火灾管理,CO_2排放率以及对CO_2的增长响应对美国本土生态系统对三种不同的通用循环模型(GCM)产生的气候情景的响应的影响, MC1动态通用植被模型(DGVM)。在所有实验因素组合中,明显的区域趋势是对预计的气候变化的响应。在美国东部一半地区,对温度升高和降水减少相对较大的平均反应是生态系统总碳损失11%。在西方,对降水增加和温度相对较小的响应是总碳储量增加了5%。模拟灭火将东部的平均碳损失减少到大约6%,并且保留了在没有灭火的情况下大部分转变为林地和热带稀树草原的森林。在整个西部,尽管植被生产力提高了,但未抑制的火势仍保持着恒定的碳储量。通过灭火,西部的碳储量增加了10%,大多数灌木丛都转变为林地甚至森林。由于对CO_2的响应相对较高的增长水平,与低CO_2响应相比,本世纪末,美国两个地区的生态系统总碳库平均增加了约9-10%。美国西部仅通过高CO_2响应,尤其是与更高的CO_2排放率相结合,就获得了足够的碳以抵消未压抑火势造成的损失。在美国东部,灭火仅足以产生具有高CO_2响应和排放率的模拟碳汇。全球变暖对美国本土生态系统的影响存在相当大的不确定性,其中一些原因在于未来温室气体排放的轨迹,植被对CO_2的直接响应以及未来不同火种管理之间的权衡取舍。如本研究所示。

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