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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >A 250-year annual precipitation reconstruction and drought assessment for Cyprus from Pinus brutia Ten. tree-rings
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A 250-year annual precipitation reconstruction and drought assessment for Cyprus from Pinus brutia Ten. tree-rings

机译:松树十国对塞浦路斯的250年年度降水重建和干旱评估。年轮

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摘要

Precipitation around Cyprus, a relatively small island, is generally consistent in year-to-year variation in all dimensions except amplitude, with the higher elevations in the west generally receiving more precipitation. An annual record of precipitation was found in tree-rings of the predominant pine species, Pinus brutia Ten., which grows from the lower foothills up to 1400m in altitude across the island. Tree-ring chronologies from four sites in west-central Cyprus are used here to reconstruct the annual September to August precipitation and a drought record for AD 1830–2006, with the drought reconstruction extending back to 1756. A minimum of 40% of the variance in annual precipitation and drought occurrence is explained by the variance in the tree-ring widths in all cases. Our drought assessment indicates that, on average, annual droughts occur once every 5 years and sustained droughts, 2–6 years in length, have occurred in small clusters of time, from 1806–1824, 1915–1934 and 1986–2000, when the winter North Atlantic Oscillation was in a predominantly positive phase. These results suggest that a sustained drought period has a mean return time probability of one in 70–100 years. This study provides the first long-term annual precipitation reconstruction and drought assessment at low to mid-elevations for Cyprus and will aid in future plans for drought mitigation.
机译:塞浦路斯(一个相对较小的岛屿)周围的降水量除振幅外,其他所有维度的年均变化基本一致,西部海拔较高的地区通常降水量更大。在主要的松树树种Pinus brutia Ten。的树轮上发现了年度降水记录,该树种从低山丘生长到​​整个岛屿的海拔1400m。这里使用塞浦路斯中西部四个地点的树年轮年代表,以重建9月至8月的年度降水量以及公元1830-2006年的干旱记录,干旱重建可追溯到1756年。至少有40%的方差在所有情况下,树木年轮宽度的变化都可以解释年降水量和干旱发生的原因。我们的干旱评估表明,从1806年至1824年,1915年至1934年和1986年至2000年,每年平均每5年发生一次干旱,持续时间为2至6年的持续干旱发生在一小段时间。冬季北大西洋涛动主要处于积极阶段。这些结果表明,持续干旱期的平均返还时间概率为70-100年。这项研究为塞浦路斯提供了中低海拔地区的首次长期年度降水重建和干旱评估,并将有助于未来缓解干旱的计划。

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