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Effects of the North Atlantic Oscillation (NAO) on combined temperature and precipitation winter modes in the Mediterranean mountains: Observed relationships and projections for the 21st century

机译:北大西洋涛动(NAO)对地中海山区冬季温度和降水组合模式的影响:观测到的21世纪关系和预测

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Previous research has identified the North Atlantic Oscillation (NAO) as one of the dominant atmospheric patterns on the temporal evolution of precipitation and temperature in the Mediterranean area. The NAO is seen to markedly affect snowpack variability and water resource availability in many mountain areas. This study investigated the influence of the NAO on winter precipitation and temperature variability, and on the occurrence of four winter climate modes defined on the basis of combined precipitation and temperature quantiles: warm and wet (WW), warm and dry (WD), cold and wet (CW) and cold and dry (CD). It is known that the occurrence of different winter modes is closely related to snow accumulation in mountains. The present study focused on 15 mountain areas in Mediterranean Europe, Morocco, Turkey and Lebanon. Global circulation models (GCMs) have been used to simulate the relationships between the NAO and winter modes for the next century under a moderate (A1B) greenhouse gas emissions scenario. The results show that for the majority of the mountain areas in the Mediterranean region, the occurrence of different winter modes was closely related to the NAO state, although the relationships were weaker in the easternmost part of the Mediterranean basin. GCMs have accurately simulated the observed relationships, and indicate that the NAO will continue to influence the occurrence of combined precipitation and temperature modes in coming decades. The GCMs also suggest enhanced winter NAOs in the future, which could lead to an increase in the frequency of dry modes. Moreover, as the simulations indicate a steady increase in temperature, winters classified as "cold" in the 21st century will be noticeably rarer compared with recent decades. The relationships between the NAO and snowpack may also change substantially in the future, especially in low altitude areas.
机译:先前的研究已将北大西洋涛动(NAO)确定为地中海地区降水和温度随时间演变的主要大气模式之一。在许多山区,NAO被认为会显着影响积雪的变化和水资源的可利用性。这项研究调查了NAO对冬季降水和温度变化的影响,以及根据降水和温度分位数组合确定的四种冬季气候模式的发生:暖湿(WW),暖干(WD),冷湿(CW),冷干(CD)。众所周知,不同冬季模式的发生与山区积雪密切相关。本研究的重点是地中海欧洲,摩洛哥,土耳其和黎巴嫩的15个山区。在中等(A1B)温室气体排放情景下,全球循环模型(GCM)已用于模拟下一世纪NAO和冬季模式之间的关系。结果表明,在地中海地区的大多数山区,不同的冬季模式的发生与NAO状态密切相关,尽管在地中海盆地最东部的关系较弱。 GCM已经精确地模拟了观测到的关系,并指出在未来的几十年中,NAO将继续影响降水和温度联合模式的发生。 GCM还建议在将来增强冬季NAO,这可能导致干旱模式的频率增加。此外,由于模拟表明温度持续升高,与最近几十年相比,在21世纪被归类为“寒冷”的冬天将更为罕见。 NAO和积雪之间的关系将来也可能发生很大变化,尤其是在低海拔地区。

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