Organochlorine contaminants in seven species of Arctic seabirds from northern Baffin Bay

2004 ◽  
Vol 128 (3) ◽  
pp. 327-338 ◽  
Author(s):  
Andrea H. Buckman ◽  
Ross J. Norstrom ◽  
Keith A. Hobson ◽  
Nina J. Karnovsky ◽  
Jason Duffe ◽  
...  
2011 ◽  
Vol 43 ◽  
pp. 65-79 ◽  
Author(s):  
O A Jorgensen ◽  
C Hvingel ◽  
M A Treble

2003 ◽  
Vol 22 (1) ◽  
pp. 11-18 ◽  
Author(s):  
Harry L. Stern ◽  
Mads Peter Heide-Jørgensen
Keyword(s):  
Sea Ice ◽  

1986 ◽  
Vol 21 (2) ◽  
pp. 251-256 ◽  
Author(s):  
Robert C. McCrea ◽  
Greg M. Wickware

Abstract Peatland waters of the Moose River basin, as well as surficial sediments and vascular plants of the estuary were sampled in 1982. Elevated levels of PCBs were found at all five peatland sites; concentrations ranged from 28 to 65 ng/L. Of the seventeen organochlorine pesticides investigated, the hexachlorocyclohexane isomers (a-and y-BHC) were the most prominent with total BHC concentrations ranging from 1.5 to 13.7 ng/L. The presence of these contaminants in ombrotrophic bogs indicated that there was atmospheric deposition of organochlorine contaminants in the basin. Analyses of surficial sediments, collected from tidal flats and coastal marshes, showed that PCBs and organochlorine pesticides were not present. Samples of Triglochin maritima L. seed heads and Typha latifolia L. roots were also free of PCBs.


2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Rebecca Jackson ◽  
Anna Bang Kvorning ◽  
Audrey Limoges ◽  
Eleanor Georgiadis ◽  
Steffen M. Olsen ◽  
...  

AbstractBaffin Bay hosts the largest and most productive of the Arctic polynyas: the North Water (NOW). Despite its significance and active role in water mass formation, the history of the NOW beyond the observational era remains poorly known. We reconcile the previously unassessed relationship between long-term NOW dynamics and ocean conditions by applying a multiproxy approach to two marine sediment cores from the region that, together, span the Holocene. Declining influence of Atlantic Water in the NOW is coeval with regional records that indicate the inception of a strong and recurrent polynya from ~ 4400 yrs BP, in line with Neoglacial cooling. During warmer Holocene intervals such as the Roman Warm Period, a weaker NOW is evident, and its reduced capacity to influence bottom ocean conditions facilitated northward penetration of Atlantic Water. Future warming in the Arctic may have negative consequences for this vital biological oasis, with the potential knock-on effect of warm water penetration further north and intensified melt of the marine-terminating glaciers that flank the coast of northwest Greenland.


1985 ◽  
Vol 8 (1) ◽  
pp. 42 ◽  
Author(s):  
Harry M. Ohlendorf ◽  
Fred C. Schaffner ◽  
Thomas W. Custer ◽  
Charles J. Stafford

2005 ◽  
Vol 134 (3) ◽  
pp. 397-409 ◽  
Author(s):  
Katrine Borgå ◽  
Hans Wolkers ◽  
Janneche U. Skaare ◽  
Haakon Hop ◽  
Derek C.G. Muir ◽  
...  

2017 ◽  
Vol 116 (1-2) ◽  
pp. 517-520 ◽  
Author(s):  
Florence E. Poon ◽  
Jennifer F. Provencher ◽  
Mark L. Mallory ◽  
Birgit M. Braune ◽  
Paul A. Smith

1980 ◽  
Vol 25 (93) ◽  
pp. 425-438
Author(s):  
B. Dey

AbstractThe study reported here illustrates the unique value of NOAA thermal infrared (TIR) images for monitoring the North Water area in Smith Sound and northern Baffin Bay during the periods of polar darkness. Wintertime satellite images reveal that, during the months of December through February, open water and thin ice occur in a few leads and polynyas. However, in March, the areas of open water and thin ice decrease to a minimum with a consequent higher concentration of ice. Two ice dams, in northern Kennedy Channel and in northern Smith Sound, regulate the flow of ice into northern Baffin Bay and also determine the areal variations of open water and thin ice in Smith Sound.


Author(s):  
Cecilia E. Heuvel ◽  
Kenneth G. Drouillard ◽  
G. Douglas Haffner ◽  
Yingming Zhao ◽  
Aaron T. Fisk

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