首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Variability in the mean latitude of the Atlantic Intertropical Convergence Zone as recorded by riverine input of sediments to the Cariaco Basin (Venezuela)
【24h】

Variability in the mean latitude of the Atlantic Intertropical Convergence Zone as recorded by riverine input of sediments to the Cariaco Basin (Venezuela)

机译:河流向Cariaco盆地(委内瑞拉)的沉积物输入所记录的大西洋热带辐合带平均纬度的变化

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

Changes in the strength and position of the Intertropical Convergence Zone (ITCZ) are an important component of climate variability in the tropical Atlantic. The Cariaco Basin, located on the northern margin of Venezuela, is sensitive to tropical Atlantic climate change and its sediments provide a record of past ITCZ behavior. Today, the Cariaco Basin experiences two distinct seasons that reflect the annual migration of the Atlantic ITCZ. Between January and March, when the ITCZ lies south of the equator, northeasterly trade winds sit directly over Cariaco Basin and strong coastal upwelling and dry conditions dominate. Beginning in June-July, as the ITCZ moves north, local rainfall reaches a maximum and the upwelling diminishes or disappears. Here we summarize new and previously published data on the river-derived terrigenous fraction of Cariaco Basin sediments, as well as comparisons to other paleoclimate records, which together suggest a coherent climatologic response in the tropical Atlantic triggered by a pattern of ITCZ migration that mimics the seasonal cycle. During periods of cooler North Atlantic SSTs, on time-scales ranging from the Little Ice Age to the Younger Dryas to the cold stadials of the last glacial, decreased detrital delivery to Cariaco Basin from local rivers suggests a southward shift in the mean latitudinal position of the ITCZ. During warm interstadials and periods of Holocene and deglacial warmth, northward shifts in ITCZ position and its belt of convective rainfall are inferred from increased dettrital delivery to the basin. Whether the rapid shifts in ITCZ position and precipitation recorded by Cariaco Basin sediments and other regional records reflect a response to forcing originating in the high latitude Atlantic or to forcing potentially sourced in the tropics is a key question yet to be fully answered. (c) 2005 Elsevier B.V. All rights reserved.
机译:热带辐合带(ITCZ)的强度和位置的变化是热带大西洋气候变异的重要组成部分。位于委内瑞拉北部边缘的Cariaco盆地对热带大西洋气候变化敏感,其沉积物提供了过去ITCZ行为的记录。今天,卡里亚科盆地经历了两个不同的季节,分别反映了大西洋ITCZ的年度迁移。在1月至3月之间,当ITCZ位于赤道以南时,东北风正好位于Cariaco盆地上空,强劲的沿海上升流和干旱条件占主导地位。从6月至7月开始,随着ITCZ向北移动,当地降雨量达到最大值,上升流减少或消失。在这里,我们总结了有关Cariaco盆地沉积物的河源陆源部分的新数据和先前发布的数据,以及与其他古气候记录的比较,这些数据共同表明,由模拟ITCZ迁移的ITCZ迁移模式引发的热带大西洋气候特征是连贯的。季节周期。在北大西洋海温较低的时期,从小冰期到较年轻的树状干果,再到最后一次冰川的寒冷季节,从当地河流到卡里亚科盆地的碎屑输送量减少,表明该地区的平均纬向向南偏移。 ITCZ。在温暖的星际间以及全新世和冰期暖期,ITCZ位置的北移及其对流降雨带是由向盆地的碎屑输送增加所推断的。 Cariaco盆地沉积物和其他区域记录所记录的ITCZ位置和降水的快速变化是否反映了对源自高纬度大西洋的强迫或对来自热带的潜在强迫的响应,这是一个尚待充分回答的关键问题。 (c)2005 Elsevier B.V.保留所有权利。

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