首页> 外文OA文献 >On the spatial and temporal variability of ENSO precipitation and drought teleconnection in mainland Southeast Asia
【2h】

On the spatial and temporal variability of ENSO precipitation and drought teleconnection in mainland Southeast Asia

机译:东南亚大陆ENSO降水与干旱遥相关的时空变化

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

The variability of the hydroclimate over mainland Southeast Asia is strongly influenced by the El Niño-Southern Oscillation (ENSO), which has been linked to severe droughts and floods that profoundly influence human societies and ecosystems alike. Although the significance of ENSO is well understood, there are still limitations in the understanding of its effects on hydroclimate, particularly with regard to understanding the spatiooral characteristics and the long-term variation of its effects. Therefore we analysed the seasonal evolution and spatial variations in the effect of ENSO on precipitation over the period of 1980-2013 and the long-term variation in the ENSO teleconnection using tree-ring-derived Palmer drought severity indices (PDSIs) for the March-May season that span over the time period 1650-2004. The analyses provided an improved understanding of the seasonal evolution of the precipitation anomalies during ENSO events. The effects of ENSO were found to be most consistent and expressed over the largest areal extents during March-May of the year when the ENSO events decay. On a longer timescale, we found that ENSO has affected the region's March-May hydroclimate over the majority (95%) of the 355-year study period and that during half (52%) of the time ENSO caused a significant increase in hydroclimatic variability. The majority of the extremely wet and dry March-May seasons also occurred during ENSO events. However, considerable variability in ENSO's influence was revealed: the spatial pattern of precipitation anomalies varied between individual ENSO events, and the strength of ENSO's influence was found to vary through time. Given the high variability in ENSO teleconnection that we described and the limitations of the current understanding of the effects of ENSO, we suggest that the adaptation to ENSO-related extremes in hydroclimate over mainland Southeast Asia needs to recognise uncertainty as an inherent part of adaptation, must go beyond "predict and control", and should seek adaptation opportunities widely within society.
机译:厄尔尼诺-南方涛动(ENSO)强烈影响了东南亚大陆上水文气候的变化,该现象与严重影响人类社会和生态系统的严重干旱和洪水有关。尽管ENSO的重要性已广为人知,但在了解其对水文气候的影响方面仍存在局限性,尤其是在了解其时空特征及其影响的长期变化方面。因此,我们使用树木年轮得出的帕尔默干旱严重性指数(PDSI)分析了1980-2013年期间ENSO对降水的影响的季节性演变和空间变化,以及ENSO遥相关的长期变化。在1650-2004年期间的五月季节。通过分析,可以更好地了解ENSO事件期间降水异常的季节演变。在ENSO事件衰减的一年中的3月至5月期间,发现ENSO的影响最为一致,并在最大的面积范围内表达。在更长的时间范围内,我们发现ENSO在355年研究期间的大部分(95%)中影响了该地区3月至5月的水文气候,并且在一半(52%)的时间中ENSO导致了水文气候变异性的显着增加。在3月至5月的极端潮湿和干燥季节中,大多数也发生在ENSO事件期间。但是,揭示了ENSO影响的显着变化:降水异常的空间模式在各个ENSO事件之间有所不同,并且发现ENSO影响的强度随时间变化。鉴于我们描述的ENSO远程连接的高度可变性以及当前对ENSO的影响的局限性,我们建议对东南亚大陆水文气候的ENSO相关极端情况进行适应需要将不确定性视为适应的固有部分,必须超越“预测和控制”,并应在社会中广泛寻求适应机会。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号