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首页> 外文期刊>International Journal of Biometeorology: Journal of the International Society of Biometeorology >Predicting the patterns of change in spring onset and false springs in China during the twenty-first century
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Predicting the patterns of change in spring onset and false springs in China during the twenty-first century

机译:预测二十一世纪中国春季发作和假弹簧的变化模式

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Spring onset has generally shifted earlier in China over the past several decades in response to the warming climate. However, future changes in spring onset and false springs, which will have profound effects on ecosystems, are still not well understood. Here, we used the extended form of the Spring Indices model (SI-x) to project changes in the first leaf and first bloom dates, and predicted false springs for the historical (1950-2005) and future (2006-2100) periods based on the downscaled daily maximum/minimum temperatures under two emission scenarios from 21 General Circulation Models (GCMs) of the Coupled Model Intercomparison Project Phase 5 (CMIP5). On average, first leaf and first bloom in China were projected to occur 21 and 23days earlier, respectively, by the end of the twenty-first century in the Representative Concentration Pathway (RCP) 8.5 scenario. Areas with greater earlier shifts in spring onset were in the warm temperate zone, as well as the north and middle subtropical zones of China. Early false spring risk increased rapidly in the warm temperate and north subtropical zones, while that declined in the cold temperate zone. Relative to early false spring risk, late false spring risk showed a common increase with smaller magnitude in the RCP 8.5 scenario but might cause greater damage to ecosystems because plants tend to become more vulnerable to the later occurrence of a freeze event. We conclude that future climate warming will continue to cause earlier occurrence of spring onset in general, but might counterintuitively increase plant damage risk in natural and agricultural systems of the warm temperate and subtropical China.
机译:春季发作一般在过去的几十年里在中国早期转移,以应对温暖的气候。然而,春季发病和假泉的未来变化将对生态系统产生深远的影响,仍然无法清楚地理解。在这里,我们使用春季指数模型(SI-X)的扩展形式来到第一叶和第一个盛开日期的项目变化,并为历史(1950-2005)和未来(2006-2100)期间预测了假弹簧在耦合型号耦合型号相互比较项目阶段5(CMIP5)的总循环模型(GCMS)下的两个发射场景下的次要日最大/最小温度。平均而言,在中国的二十一世纪结束时,中国的第一叶和第一次盛开将分别于21至23天在代表性浓度途径(RCP)8.5场景中。春季发病较早换档的地区在温暖的温带区域,以及中国的北极和中部亚热带区域。早期假春季风险在温带温带和北亚热带地区迅速增加,而冷水区中有所下降。相对于早期假春天风险,迟到的假弹簧风险显示,RCP 8.5场景中的较小幅度呈较小的幅度较小,但可能对生态系统造成更大的损害,因为工厂往往变得更容易受到冻结事件的后期发生的影响。我们得出结论,未来的气候变暖将继续引起春季发病的早期发生,但可能会违反温带和亚热带地区天然和农业系统的植物损伤风险。

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