首页> 外文期刊>Hydrological Processes >Interpretation of El Niño-Southern Oscillation‐related precipitation anomalies in north‐western Borneo using isotopic tracers
【24h】

Interpretation of El Niño-Southern Oscillation‐related precipitation anomalies in north‐western Borneo using isotopic tracers

机译:利用同位素示踪解释婆罗洲西北部厄尔尼诺-南方涛动相关的降水异常

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

We examined rainfall anomalies associated with the El Nino-Southern Oscillation (ENSO) in northern Sarawak, Malaysia, using the oxygen isotopic composition of rainfall. Two precipitation-sampling campaigns were conducted for isotope analysis: (a) at the Lambir Hill National Park (4.2 degrees N, 114.0 degrees E) from July 2004 to October 2006 and (b) at the Gunung Mulu National Park (3.9 degrees N, 114.8 degrees E) from January 2006 to July 2008. The records from these campaigns were merged with a previously published rainfall isotope dataset from Gunung Mulu site to create a 7-year-long record of the oxygen isotopic composition of Sarawak rainfall. The record exhibits clear intraseasonal variations (ISVs) with periods ranging from 10 to 70days. The ISVs of 10- to 90-day band-pass filtered oxygen isotopic composition are linked to the synoptic-scale precipitation anomalies over the southern South China Sea (SCS). The lead-lag correlation map of precipitation with the filtered oxygen isotope anomalies shows that an anomalous wet condition responsible for the decrease in oxygen isotopic composition appears over the SCS in association with the passage of north-eastward propagation of the boreal summer intraseasonal oscillation (BSISO) in the summer monsoon season. The anomalous wet condition in spring is connected with eastward-propagating Madden-Julian oscillation (MJO), whereas the sustained wet condition in winter is responsible for the occurrence of the Borneo vortex (BV) over the SCS. ENSO modulates the frequency of these synoptic conditions on a seasonal and longer time scale, showing a strong correlation between the seasonal isotopic anomalies and the Southern Oscillation index. We therefore discern, from the significant correlation between the isotope anomalies and area-averaged Sarawak rainfall anomalies (R=-0.65, p0.01), that ENSO-related precipitation anomalies are linked to the seasonal modulation of the BSISO and MJO activity and BV genesis.
机译:我们使用降雨的氧同位素组成研究了马来西亚北部砂拉越与厄尔尼诺-南方涛动(ENSO)相关的降雨异常。进行了两次降水采样活动以进行同位素分析:(a)2004年7月至2006年10月在兰比尔山国家公园(北纬4.2度,东经114.0度),以及(b)在Gunung Mulu国家公园(北纬3.9度,从2006年1月至2008年7月,海拔114.8度。将这些活动的记录与先前从Gunung Mulu站点发布的降雨同位素数据集合并,以创建长达7年的砂拉越降雨的氧同位素组成记录。该记录显示明显的季节内变化(ISV),周期从10到70天不等。 10到90天带通滤过的氧同位素组成的ISV与南海南部(SCS)的天气尺度降水异常有关。与过滤的氧同位素异常有关的降水超前-滞后相关图表明,与夏季北半球季节内振荡(BSISO)的东北向传播有关,SCS上出现了导致氧同位素组成降低的异常湿润条件。 )在夏季风季节。春季的异常潮湿状况与向东传播的马登-朱利安振荡(MJO)有关,而冬季持续的潮湿状况是造成南海婆罗洲涡(BV)发生的原因。 ENSO在季节和较长的时间尺度上调节这些天气条件的频率,显示季节同位素异常与南方涛动指数之间有很强的相关性。因此,我们从同位素异常与砂拉越降水平均面积异常之间的显着相关性(R = -0.65,p <0.01)可以看出,ENSO相关的降水异常与BSISO和MJO活性以及BV的季节性调节有关。成因。

著录项

  • 来源
    《Hydrological Processes》 |2018年第14期|2176-2186|共11页
  • 作者单位

    Nagoya Univ, Inst Space Earth Environm Res ISEE, Nagoya, Aichi, Japan;

    Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi, Japan;

    Nagoya Univ, Inst Space Earth Environm Res ISEE, Nagoya, Aichi, Japan;

    Nagoya Univ, Inst Space Earth Environm Res ISEE, Nagoya, Aichi, Japan;

    Nagoya Univ, Inst Space Earth Environm Res ISEE, Nagoya, Aichi, Japan;

    Natl Taiwan Univ, Sch Forestry & Resource Conservat, Taipei, Taiwan;

    Res Inst Humanity & Nat, Kyoto, Japan;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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