scholarly journals Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011

2016 ◽  
Vol 8 (8) ◽  
pp. 622 ◽  
Author(s):  
Mark Carroll ◽  
Margaret Wooten ◽  
Charlene DiMiceli ◽  
Robert Sohlberg ◽  
Maureen Kelly
Water ◽  
2018 ◽  
Vol 10 (7) ◽  
pp. 824 ◽  
Author(s):  
Yijie Sui ◽  
Dongjie Fu ◽  
Xuefeng Wang ◽  
Fenzhen Su

2022 ◽  
pp. 127449
Author(s):  
Majid Zaremehrjardy ◽  
Justin Victor ◽  
Seonggyu Park ◽  
Brian Smerdon ◽  
Daniel S. Alessi ◽  
...  

2017 ◽  
Vol 9 (5) ◽  
pp. 497 ◽  
Author(s):  
Mark Carroll ◽  
Tatiana Loboda

Nature ◽  
2018 ◽  
Vol 561 (7724) ◽  
pp. 528-532 ◽  
Author(s):  
Sean D. Willett ◽  
Scott W. McCoy ◽  
Helen W. Beeson

2019 ◽  
Vol 224 ◽  
pp. 219-235 ◽  
Author(s):  
Susan C. Steele-Dunne ◽  
Sebastian Hahn ◽  
Wolfgang Wagner ◽  
Mariette Vreugdenhil

Radiocarbon ◽  
1980 ◽  
Vol 22 (3) ◽  
pp. 636-646 ◽  
Author(s):  
Wolfgang Roether ◽  
Karl-Otto Münnich ◽  
Hildegard Schoch

Nuclear-weapon produced 14C (or bomb 14C) in the ocean can be traced by simultaneous tritium observations. Data are presented on the general relationship of bomb 14C and tritium in the North Atlantic. For the period 1965 to 1973, the excess 14C to tritium ratios in the surface water vary, systematically, over a factor of 10: the ratios monotonically increase with time, and decrease with latitude, particularly so for the later observations. The sub-surface water ratios show that the mid- and low-latitude water below about the 15° C isothermal horizon (~500m depth) originates from higher northern latitudes, rather than being renewed by local vertical mixing. It is further shown that in the North Atlantic, bomb 14C did not penetrate beyond the horizon where the presently observed 14C concentration is Δ14C = —75‰. Observed concentrations up to about —40‰ can be corrected for a bomb contribution if the tritium concentration is known because the bomb 14C to tritium concentration ratio is rather uniform in this range. A surface water 14C concentration versus time curve is presented for the period since 1957. This curve is based on a North Atlantic mixing model and is fitted to the 14C observations. Making use of a previously published tritium versus time curve obtained by the same model, a time curve for the average excess 14C to tritium ratio in North Atlantic surface water is given. This curve reproduces the observations well. The presented data and theoretical curves show the usefulness of simultaneous 14C and tritium observations for mixing studies and to provide corrections for bomb 14C in sub-surface 14C data in the North Atlantic.


2019 ◽  
Vol 152 ◽  
pp. 101730
Author(s):  
Marta Martínez-Sánchez ◽  
José-Abel Flores ◽  
Eliana Palumbo ◽  
Montserrat Alonso-Garcia ◽  
Francisco-Javier Sierro ◽  
...  

2006 ◽  
Vol 175 (4S) ◽  
pp. 511-512
Author(s):  
David G. McLeod ◽  
Ira Klimberg ◽  
Donald Gleason ◽  
Gerald Chodak ◽  
Thomas Morris ◽  
...  

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