scholarly journals On the peopling of the Americas: molecular evidence for the Paleoamerican and the Solutrean models

2017 ◽  
Author(s):  
Dejian Yuan ◽  
Shi Huang
Keyword(s):  
North Atlantic ◽  
North Atlantic Ocean ◽  
Molecular Evidence ◽  
Bering Strait ◽  
East Asians ◽  
The North ◽  
Pack Ice ◽  
Peopling Of The Americas ◽  
Close Relationship ◽  
The North Atlantic

AbstractMorphological and archaeological studies suggest that the Americas were first occupied by non-Mongoloids with Australo-Melanesian traits (the Paleoamerican model), which was subsequently followed by Southwest Europeans coming in along the pack ice of the North Atlantic Ocean (the Solutrean model) and by East Asians and Siberians arriving by way of the Bering Strait. Past DNA studies, however, have produced different accounts. With a better understanding of genetic diversity, we have now reinterpreted public DNA data. Consistent with our recent finding of a close relationship between South Pacific populations and Denisovans or Neanderthals who were archaic Africans with Eurasian admixtures, the ∼9500 year old Kennewick Man skeleton with Australo-Melanesian affinity from North America was about equally related to Europeans and Africans, least related to East Asians among present-day people, and most related to the ∼42000 year old Neanderthal Mezmaiskaya-2 from Adygea Russia among ancient Eurasian DNAs. The ∼12700 year old Anzick-1 of the Clovis culture was most related to the ∼18720 year old El Miron of the Magdalenian culture in Spain among ancient DNAs. Amerindian mtDNA haplotypes, unlike their Eurasian sister haplotypes, share informative SNPs with Australo-Melanesians, Africans, or Neanderthals. These results suggest a unifying account of informative findings on the settlement of the Americas.

scholarly journals Response of Thermohaline Circulation to Freshwater Forcing under Present-Day and LGM Conditions

2008 ◽  
Vol 21 (10) ◽  
pp. 2239-2258 ◽  
Author(s):  
Aixue Hu ◽  
Bette L. Otto-Bliesner ◽  
Gerald A. Meehl ◽  
Weiqing Han ◽  
Carrie Morrill ◽  
...  
Keyword(s):  
North Atlantic ◽  
Thermohaline Circulation ◽  
North Atlantic Ocean ◽  
The Arctic ◽  
Bering Strait ◽  
Climate System Model ◽  
The North ◽  
Freshwater Forcing ◽  
Bering Strait Throughflow ◽  
The North Atlantic

Abstract Responses of the thermohaline circulation (THC) to freshwater forcing (hosing) in the subpolar North Atlantic Ocean under present-day and the last glacial maximum (LGM) conditions are investigated using the National Center for Atmospheric Research Community Climate System Model versions 2 and 3. Three sets of simulations are analyzed, with each set including a control run and a freshwater hosing run. The first two sets are under present-day conditions with an open and closed Bering Strait. The third one is under LGM conditions, which has a closed Bering Strait. Results show that the THC nearly collapses in all three hosing runs when the freshwater forcing is turned on. The full recovery of the THC, however, is at least a century earlier in the open Bering Strait run than the closed Bering Strait and LGM runs. This is because the excessive freshwater is diverged almost equally toward north and south from the subpolar North Atlantic when the Bering Strait is open. A significant portion of the freshwater flowing northward into the Arctic exits into the North Pacific via a reversed Bering Strait Throughflow, which accelerates the THC recovery. When the Bering Strait is closed, this Arctic to Pacific transport is absent and freshwater can only be removed through the southern end of the North Atlantic. Together with the surface freshwater excess due to precipitation, evaporation, river runoff, and melting ice in the closed Bering Strait experiments after the hosing, the removal of the excessive freshwater takes longer, and this slows the recovery of the THC. Although the background conditions are quite different between the present-day closed Bering Strait run and the LGM run, the THC responds to the freshwater forcing added in the North Atlantic in a very similar manner.

The first transit of the Northwest Passage by Russian icebreaker

Polar Record ◽  
1993 ◽  
Vol 29 (169) ◽  
pp. 148-148 ◽  
Author(s):  
John Splettstoesser ◽  
Beezie Drake Splettstoesser
Keyword(s):  
Atlantic Ocean ◽  
South Korea ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Coast Guard ◽  
Bering Strait ◽  
Northwest Passage ◽  
The North ◽  
The North Atlantic

In a voyage beginning 24 July in Ulsan, South Korea, and ending i n St Petersburg, Russia, on 21 September 1992, the icebreaker Kapitan Khlebnikov successfully completed an unassisted transit of the Northwest Passage, from Bering Strait to the North Atlantic Ocean. The ship was chartered jointly by Polar Schiffahrts-Consulting, Hamburg, Germany; Blyth and Company Travel, Toronto, Ontario, Canada; and D.G. Wells Marine Ltd, Ottawa, Ontario, Canada. It was marketed for tourists, some of whom traveled the entire distance of 14,120 nautical miles [26,150 km]. Khlebnikov was the fifty-third vessel to complete the Northwest Passage since Roald Amundsen first accomplished it in 1906 (Pullen and Swithinbank 1991, and confirmed by the office of Coast Guard Northern, Ottawa, Canada).

Spatiotemporal evolution of the chlorophyll a trend in the North Atlantic Ocean

2018 ◽  
Vol 612 ◽  
pp. 1141-1148 ◽  
Author(s):  
Min Zhang ◽  
Yuanling Zhang ◽  
Qi Shu ◽  
Chang Zhao ◽  
Gang Wang ◽  
...  
Keyword(s):  
Atlantic Ocean ◽  
Chlorophyll A ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Spatiotemporal Evolution ◽  
The North ◽  
The North Atlantic

On the uncertainty of future projections of Marine Heatwave events in the North Atlantic Ocean

2021 ◽  
Vol 56 (7-8) ◽  
pp. 2027-2056
Author(s):  
Sandra M. Plecha ◽  
Pedro M. M. Soares ◽  
Susana M. Silva-Fernandes ◽  
William Cabos
Keyword(s):  
Atlantic Ocean ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Future Projections ◽  
The North ◽  
The North Atlantic

Monthly satellite-derived phytoplankton pigment distribution for the North Atlantic Ocean basin

Eos ◽  
1986 ◽  
Vol 67 (44) ◽  
pp. 835 ◽  
Author(s):  
W. E. Esaias ◽  
G. C. Feldman ◽  
C. R. McClain ◽  
J. A. Elrod
Keyword(s):  
Atlantic Ocean ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Ocean Basin ◽  
Phytoplankton Pigment ◽  
The North ◽  
Pigment Distribution ◽  
The North Atlantic

scholarly journals A New Method for Tracking Meddies by Satellite Altimetry

2014 ◽  
Vol 31 (6) ◽  
pp. 1434-1445 ◽  
Author(s):  
Federico Ienna ◽  
Young-Heon Jo ◽  
Xiao-Hai Yan
Keyword(s):  
Remote Sensing ◽  
Atlantic Ocean ◽  
North Atlantic ◽  
North Atlantic Ocean ◽  
Saline Water ◽  
Ensemble Empirical Mode Decomposition ◽  
Altimeter Data ◽  
In Situ Techniques ◽  
The North ◽  
The North Atlantic

Abstract Subsurface coherent vortices in the North Atlantic, whose saline water originates from the Mediterranean Sea and which are known as Mediterranean eddies (meddies), have been of particular interest to physical oceanographers since their discovery, especially for their salt and heat transport properties into the North Atlantic Ocean. Many studies in the past have been successful in observing and studying the typical properties of meddies by probing them with in situ techniques. The use of remote sensing techniques would offer a much cheaper and easier alternative for studying these phenomena, but only a few past studies have been able to study meddies by remote sensing, and a reliable method for observing them remotely remains elusive. This research presents a new way of locating and tracking meddies in the North Atlantic Ocean using satellite altimeter data. The method presented in this research makes use of ensemble empirical mode decomposition (EEMD) as a means to isolate the surface expressions of meddies on the ocean surface and separates them from any other surface constituents, allowing robust meddies to be consistently tracked by satellite. One such meddy is successfully tracked over a 6-month time period (2 November 2005 to 17 May 2006). Results of the satellite tracking method are verified using expendable bathythermographs (XBT).

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