Reply to comment by S. Peacock on “Glacial-interglacial circulation changes inferred from 231Pa/230Th sedimentary record in the North Atlantic region”
Reply to comment by S. Peacock on “Glacial-interglacial circulation changes inferred from 231Pa/230Th sedimentary record in the North Atlantic region”
复制标题
回复S. Peacock关于“根据北大西洋地区231Pa/230Th沉积记录推断的冰期-间冰期环流变化”的评论
DOI：
10.1029/2009pa001867
复制
发表时间：
2010
期刊：
影响因子：
--
通讯作者：
L. Labeyrie
中科院分区：
文献类型：
--
作者：
J. Gherardi;Yiming Luo;R. Francois;J. McManus;S. Allen;L. Labeyrie
[1]Peacock [2010，P10，此后]对我们最近的文章[Gherardi等人，2009年，G 09以下]：（1）我们的现代大西洋纬向翻转环流（AMOC）的描述，（2）现代环流和我们的全新世沉积Pa/Th测深剖面之间的明显不一致，（3）我们使用的核心重建AMOC的位置，不位于深西部边界流（DWBC）。我们欢迎这一评论，因为它使我们有机会澄清我们研究古循环方法的重要方面，并解决我们原始文本措辞所引起的任何潜在误解。
[1] Peacock [2010, P10 hereafter] takes issue with several aspects of our recent article [Gherardi et al., 2009, G09 hereafter]: (1) our description of the modern Atlantic meridional overturning circulation (AMOC), (2) apparent inconsistencies between modern circulation and our Holocene sedimentary Pa/Th bathymetric profile, and (3) our use of cores for reconstructing AMOC from locations that do not lie beneath the Deep Western Boundary Current (DWBC). We welcome the comment as it affords us the opportunity to clarify important aspects of our approach to studying paleocirculation and to address any potential misunderstandings arising from the wording of our original text.