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Mid-21st century climate and weather extremes in Cyprus as projected by six regional climate models

机译:六个区域气候模式预测的塞浦路斯21世纪中叶气候和天气极端事件

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We present climate change projections and apply indices of weather extremes for the Mediterranean island Cyprus using data from regional climate model (RCM) simulations driven by the IPCC A1B scenario within the ENSEMBLES project. Daily time-series of temperature and precipitation were used from six RCMs for a reference period 1976-2000 and for 2026-2050 ('future') for representative locations, applying a performance selection among neighboring model grid-boxes. The annual average temperatures of the model ensemble have a ± 1.5℃ bias from the observations (negative for maximum and positive for minimum temperature), and the models underestimate annual precipitation totals by 4-17%. The climatological annual cycles for the observations fall within the lcr range of the 6-model average, highlighting the strength of using multi-model output. We obtain reasonable agreement between models and observations for the temperature-related indices of extremes for the recent past, while the comparison is less good for the precipitation-related extremes. For the future, the RCM ensemble shows significant wanning of 1℃ in winter to 2℃ in the summer for both maximum and minimum temperatures. Rainfall is projected to decrease by 2-8%, although this is not statistically significant. Our results indicate the shift of the mean climate to a warmer state, with a relatively strong increase in the warm extremes. The precipitation frequency is projected to decrease at the inland Nicosia and at the coastal Limassol, while the mountainous Saittas could experience more frequent 5-15 mm/day rainfall. In future, very hot days are expected to increase by more than 2 weeks/year and tropical nights by 1 month/year. The annual number of consecutive dry days shows a statistically significant increase (of 9 days) in Limassol. These projected changes of the Cyprus climate may adversely affect ecosystems and the economy of the island and emphasize the need for adaptation strategies.
机译:我们使用ENSEMBLES项目中IPCC A1B情景驱动的区域气候模型(RCM)模拟数据,提出了地中海岛屿塞浦路斯的气候变化预测并应用了极端天气指数。在六个参考模型的1976-2000年和2026-2050年(“未来”)的代表性地区,使用了六个RCM的温度和降水的每日时间序列,并在相邻的模型网格箱中进行了性能选择。该模型集合的年平均温度与观测值有±1.5℃的偏差(最高温度为负,最低温度为正),并且这些模型低估了年降水总量4-17%。观测的气候年度周期在6个模型平均值的lcr范围之内,突出了使用多模型输出的优势。我们在模型和观测值之间获得了最近一段时间与温度相关的极端指数的合理共识,而对于与降水相关的极端而言,比较却没有那么好。将来,无论最高温度还是最低温度,RCM集合都将在冬季从1℃显着下降到夏季至2℃。预计降雨量将减少2-8%,尽管这在统计上并不显着。我们的结果表明,平均气候向更温暖的状态转变,极端温暖的情况相对增加。预计内陆尼科西亚和利马索尔沿海地区的降水频率将减少,而山区Saittas可能会遇到更频繁的5-15毫米/天的降雨。将来,预计炎热的日子将以每年超过2周的速度增长,热带夜晚的数字将以每年1个月的速度增长。利马索尔每年连续的干旱天数显示出统计上的显着增加(9天)。塞浦路斯气候的这些预计变化可能会对岛屿的生态系统和经济产生不利影响,并强调需要采取适应战略。

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