scholarly journals A New Trend in Cryoseismology: A Proxy for Detecting the Polar Surface Environment

2018 ◽  
Author(s):  
Masaki Kanao
Keyword(s):  
Polar Surface ◽  
Surface Environment

scholarly journals Polar-surface-driven growth of ZnS microsprings with novel optoelectronic properties

2015 ◽  
Vol 7 (9) ◽  
pp. e213-e213 ◽  
Author(s):  
Qi Zhang ◽  
Cong Wei ◽  
Xing Li ◽  
Muhammad Hafeez ◽  
Lin Gan ◽  
...  
Keyword(s):  
Optoelectronic Properties ◽  
Polar Surface

Discovery of a Potent Free Fatty Acid 1 Receptor Agonist with Low Lipophilicity, Low Polar Surface Area, and Robust in Vivo Efficacy

2016 ◽  
Vol 59 (6) ◽  
pp. 2841-2846 ◽  
Author(s):  
Steffen V. F. Hansen ◽  
Elisabeth Christiansen ◽  
Christian Urban ◽  
Brian D. Hudson ◽  
Claire J. Stocker ◽  
...  
Keyword(s):  
Fatty Acid ◽  
Free Fatty Acid ◽  
Surface Area ◽  
Receptor Agonist ◽  
Polar Surface Area ◽  
In Vivo Efficacy ◽  
Polar Surface

First-principles study of MgB2 film on the MgO(111) polar surface

2008 ◽  
Vol 372 (10) ◽  
pp. 1671-1675 ◽  
Author(s):  
Z.H. Zhu ◽  
X.H. Yan ◽  
Z.H. Guo ◽  
Y.R. Yang
Keyword(s):  
First Principles ◽  
Polar Surface ◽  
Mgb2 Film ◽  
First Principles Study

High Reactivity of the ZnO(0001) Polar Surface: The Role of Oxygen Adatoms

2017 ◽  
Vol 121 (29) ◽  
pp. 15711-15718 ◽  
Author(s):  
Yang Liu ◽  
Wangping Xu ◽  
Yueyue Shan ◽  
Hu Xu
Keyword(s):  
High Reactivity ◽  
Polar Surface ◽  
Oxygen Adatoms

Paleoceanographic evolution of the SW Svalbard margin (76°N) since 20,000 14C yr BP

2007 ◽  
Vol 67 (1) ◽  
pp. 100-114 ◽  
Author(s):  
Tine L. Rasmussen ◽  
Erik Thomsen ◽  
Marta A. Ślubowska ◽  
Simon Jessen ◽  
Anders Solheim ◽  
...  
Keyword(s):  
Surface Water ◽  
Water Mass ◽  
Atlantic Water ◽  
Subsurface Water ◽  
Planktic Foraminifera ◽  
Surface Conditions ◽  
Polar Surface ◽  
Warm Core ◽  
Heinrich Event ◽  
Benthic Environment

AbstractTwo cores from the southwestern shelf and slope of Storfjorden, Svalbard, taken at 389 m and 1485 m water depth have been analyzed for benthic and planktic foraminifera, oxygen isotopes, and ice-rafted debris. The results show that over the last 20,000 yr, Atlantic water has been continuously present on the southwestern Svalbard shelf. However, from 15,000 to 10,000 14C yr BP, comprising the Heinrich event H1 interval, the Bølling–Allerød interstades and the Younger Dryas stade, it flowed as a subsurface water mass below a layer of polar surface water. In the benthic environment, the shift to interglacial conditions occurred at 10,000 14C yr BP. Due to the presence of a thin upper layer of polar water, surface conditions remained cold until ca. 9000 14C yr BP, when the warm Atlantic water finally appeared at the surface. Neither extensive sea ice cover nor large inputs of meltwater stopped the inflow of Atlantic water. Its warm core was merely submerged below the cold polar surface water.

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