Role of colloidal material in the removal of 234Th in the Canada basin of the Arctic Ocean

2003 ◽  
Vol 50 (10-11) ◽  
pp. 1353-1373 ◽  
Author(s):  
M. Baskaran ◽  
P.W. Swarzenski ◽  
D. Porcelli
Author(s):  
Mary C. O’Brien ◽  
Humfrey Melling ◽  
Thomas F. Pedersen ◽  
Robie W. Macdonald

2012 ◽  
Vol 47 (2) ◽  
pp. 923-931 ◽  
Author(s):  
James M. Armitage ◽  
Sung-Deuk Choi ◽  
Torsten Meyer ◽  
Trevor N. Brown ◽  
Frank Wania

2019 ◽  
Vol 177 ◽  
pp. 201-212 ◽  
Author(s):  
Igor Niezgodzki ◽  
Jarosław Tyszka ◽  
Gregor Knorr ◽  
Gerrit Lohmann

2019 ◽  
Vol 53 (22) ◽  
pp. 13136-13145 ◽  
Author(s):  
Luis M. Laglera ◽  
Camila Sukekava ◽  
Hans A. Slagter ◽  
Javier Downes ◽  
Alberto Aparicio-Gonzalez ◽  
...  

2013 ◽  
Vol 67 ◽  
pp. 8-13 ◽  
Author(s):  
Xin He ◽  
Liguang Sun ◽  
Zhouqing Xie ◽  
Wen Huang ◽  
Nanye Long ◽  
...  

2007 ◽  
Vol 37 (4) ◽  
pp. 1066-1076 ◽  
Author(s):  
M-L. Timmermans ◽  
H. Melling ◽  
L. Rainville

Abstract A 50-day time series of high-resolution temperature in the deepest layers of the Canada Basin in the Arctic Ocean indicates that the deep Canada Basin is a dynamically active environment, not the quiet, stable basin often assumed. Vertical motions at the near-inertial (tidal) frequency have amplitudes of 10– 20 m. These vertical displacements are surprisingly large considering the downward near-inertial internal wave energy flux typically observed in the Canada Basin. In addition to motion in the internal-wave frequency band, the measurements indicate distinctive subinertial temperature fluctuations, possibly due to intrusions of new water masses.


Polar Record ◽  
2015 ◽  
Vol 52 (1) ◽  
pp. 114-117 ◽  
Author(s):  
Ling Lin ◽  
Jianfeng He ◽  
Fang Zhang ◽  
Shunan Cao ◽  
Can Zhang

ABSTRACTMelt ponds are common on the surface of ice floes in the Arctic Ocean during spring and summer. Few studies on melt pond algae communities have been accomplished. These studies have shown that these melt ponds were ultra-oligotrophic, and contribute little to overall productivity. However, during the 6th Chinese Arctic Cruise in the Arctic Ocean in summer 2014, a closed coloured melt pond with a chlorophyll a concentration of 15.32 μg/L was observed on Arctic pack ice in the Canada Basin. The bloom was caused by the chlorophyte Carteria lunzensis at an abundance of 15.49×106 cells/L and biomass of 5.07 mg C/L. Primary production within surface melt ponds may need more attention along with Arctic warming.


2010 ◽  
Vol 44 (22) ◽  
pp. 8422-8428 ◽  
Author(s):  
Xiaoguo Wu ◽  
James C. W. Lam ◽  
Chonghuan Xia ◽  
Hui Kang ◽  
Liguang Sun ◽  
...  

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