之前的大气/海洋环流不同巴拿马地峡的形成?- 江南体育网页版- - - - -地球科学堆江南电子竞技平台栈交换 最近30从www.hoelymoley.com 2023 - 07 - 10 - t01:35:54z //www.hoelymoley.com/feeds/question/899 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/899 7 之前的大气/海洋环流不同巴拿马地峡的形成? InquilineKea //www.hoelymoley.com/users/10 2014 - 05 - 12 - t00:23:25z 2014 - 12 - 21 - t21:52:54z < p >是厄尔尼诺现象扩展到非洲的西海岸吗?当时的经向翻转环流存在吗?有另一个推翻循环存在? < / p > //www.hoelymoley.com/questions/899/-/902 # 902 7 答案由plannapus的大气/海洋循环的不同形成前巴拿马地峡吗? plannapus //www.hoelymoley.com/users/87 2014 - 05 - 12 - t06:57:02z 2014 - 05 - 12 - t15:01:50z < p >关于温盐环流:定义的一部分,我认为是底水在极地地区的形成。< / p > < p >南极底层水的形成(AABW)在南大洋与南极绕极流的存在密切相关(ACC)。ACC的可能只有在塔斯马尼亚的网关和德雷克海峡(之间的南极洲,南美)都发生在始新世末/最早的渐新世。ACC被认为是深、强电流今天渐新世末以来的最新(<强>莱尔et al . 2008 < /强>),所以AABW也被认为存在自渐新世。< / p > < p >然而至于北大西洋深层水(NADW)形成而言:它确实与部分墨西哥湾流和北半球冰期。而后者只发生3.6 ma (e . g。<强> Muddelsee,作者2005 < /强>),关闭的墨西哥湾流是一个直接后果的巴拿马地峡:浅的(因此关闭当前)巴拿马航道被认为以前扔在ca。4.6 ma(<强> Haug,蒂1998 < /强>)完全关闭2.6 ma(< >强水汽et al . 2008 < /强>)。< / p > < p >这相当有把握地说,温盐环流我们今天知道了大概3.6 ma(因此中新世)。< / p > < p >在始新世马33(55),底水的形成被认为发生在中低纬度(e . g。<强> Kennett, Stott 1990) leading to a very completely different kind of global circulation.

The impact on the ENSO (if it existed at the time) is, as far as I know, unknown but since South America was still here to limit it eastward I don't think it ever reached Africa.

References:
Haug, G. H. & R. Tiedemann. 1998. Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation. Nature, 393: 673-676.
Kennett, J. P. & L. D. Stott. 1990. Proteus and Proto-oceanus: ancestral Paleogene oceans as revealed from Antarctic stable isotopic results; ODP Leg 113. In P. F. Barker et al. (Eds), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113: 865-880.
Lunt, D. J., P. J. Valdes, A. Haywood & I. C. Rutt. 2008. Closure of the Panama Seaway during the Pliocene: implications for climate and Northern Hemisphere glaciation. Climate Dynamics, 30: 1-18.
Lyle, M., Gibbs, S., Moore T. C., Rea, D. K., 2007. Late Oligocene initiation of the Antarctic Circumpolar Current: evidence from the South Pacific. Geology, 35(8): 691-694.
Mudelsee, M. & M. E. Raymo. 2005. Slow dynamics of the Northern Hemisphere glaciation. Paleoceanography, 20: PA4022.

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