首页> 外文期刊>Global change biology >Characterizing differences in precipitation regimes of extreme wet and dry years: implications for climate change experiments
【24h】

Characterizing differences in precipitation regimes of extreme wet and dry years: implications for climate change experiments

机译:表征极端干旱和干旱年份降水状况的差异:对气候变化实验的影响

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Climate change is intensifying the hydrologic cycle and is expected to increase the frequency of extreme wet and dry years. Beyond precipitation amount, extreme wet and dry years may differ in other ways, such as the number of precipitation events, event size, and the time between events. We assessed 1614 long-term (100year) precipitation records from around the world to identify key attributes of precipitation regimes, besides amount, that distinguish statistically extreme wet from extreme dry years. In general, in regions where mean annual precipitation (MAP) exceeded 1000mm, precipitation amounts in extreme wet and dry years differed from average years by similar to 40% and 30%, respectively. The magnitude of these deviations increased to >60% for dry years and to >150% for wet years in arid regions (MAP500mm). Extreme wet years were primarily distinguished from average and extreme dry years by the presence of multiple extreme (large) daily precipitation events (events >99th percentile of all events); these occurred twice as often in extreme wet years compared to average years. In contrast, these large precipitation events were rare in extreme dry years. Less important for distinguishing extreme wet from dry years were mean event size and frequency, or the number of dry days between events. However, extreme dry years were distinguished from average years by an increase in the number of dry days between events. These precipitation regime attributes consistently differed between extreme wet and dry years across 12 major terrestrial ecoregions from around the world, from deserts to the tropics. Thus, we recommend that climate change experiments and model simulations incorporate these differences in key precipitation regime attributes, as well as amount into treatments. This will allow experiments to more realistically simulate extreme precipitation years and more accurately assess the ecological consequences.
机译:气候变化正在加剧水文循环,并有望增加极端干旱和干旱年份的频率。除了降水量之外,极端的湿润和干旱年份可能还会以其他方式有所不同,例如降水事件的数量,事件的大小以及两次事件之间的时间。我们评估了1614个来自世界各地的长期(100年)降水记录,以找出降水量的主要属性(除数量外),这些属性将统计学上的极端湿润与极端干旱年份区分开来。通常,在年平均降水量(MAP)超过1000mm的地区,极端湿润和干燥年份的降水量与平均年份的差异分别约为40%和30%。在干旱地区(MAP <500mm),这些偏差的幅度在干旱年份增加到> 60%,在潮湿年份增加到> 150%。极端湿年与平均干年和极端干年的主要区别在于存在多个极端(大型)日降水事件(所有事件> 99%)与极端年份相比,这些年份在极端潮湿的年份发生的频率是两倍。相反,这些大降水事件在极端干旱年份很少见。对于区分极端干旱和干旱年份而言,次要事件大小和频率或两次事件之间的干旱天数不太重要。但是,极端干旱年份与平均年份的区别在于事件之间的干旱天数增加。在从沙漠到热带地区的全球12个主要陆地生态区中,极端干旱和干旱年份的降水方式属性始终不同。因此,我们建议气候变化实验和模型模拟应将这些差异纳入关键的降水状态属性,并将其纳入处理中。这将使实验能够更真实地模拟极端降水年份并更准确地评估生态后果。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

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