scholarly journals Finescale Planktonic Vertical Structure: Horizontal Extent and the Controlling Physical Processes Layered Organization in the Coastal Ocean (LOCO) DRI

2007 ◽  
Author(s):  
Timothy J. Cowles
2015 ◽  
Vol 120 (10) ◽  
pp. 4718-4748 ◽  
Author(s):  
Xianan Jiang ◽  
Duane E. Waliser ◽  
Prince K. Xavier ◽  
Jon Petch ◽  
Nicholas P. Klingaman ◽  
...  

2015 ◽  
Vol 120 (10) ◽  
pp. 4749-4763 ◽  
Author(s):  
Prince K. Xavier ◽  
Jon C. Petch ◽  
Nicholas P. Klingaman ◽  
Steve J. Woolnough ◽  
Xianan Jiang ◽  
...  

2015 ◽  
Vol 120 (10) ◽  
pp. 4671-4689 ◽  
Author(s):  
Nicholas P. Klingaman ◽  
Xianan Jiang ◽  
Prince K. Xavier ◽  
Jon Petch ◽  
Duane Waliser ◽  
...  

2015 ◽  
Vol 120 (10) ◽  
pp. 4690-4717 ◽  
Author(s):  
Nicholas P. Klingaman ◽  
Steven J. Woolnough ◽  
Xianan Jiang ◽  
Duane Waliser ◽  
Prince K. Xavier ◽  
...  

2021 ◽  
Author(s):  
Alizee Roobaert ◽  
Goulven Laruelle ◽  
Laure Resplandy ◽  
Peter Landschützer ◽  
Nicolas Gruber ◽  
...  

<p>The spatio-temporal variability and the underlying drivers of the carbon dioxide (CO<sub>2</sub>) exchange at the air-water interface (FCO<sub>2</sub>) of the global coastal ocean are still poorly understood and their quantification remains highly uncertain. Here, we present an analysis of the spatial and seasonal variability of FCO<sub>2</sub> using a high-resolution (0.25 degree) monthly climatology (1998-2015 period) for coastal sea surface partial pressure in CO<sub>2</sub> (pCO<sub>2</sub>), globally.</p><p>Overall, a clear latitudinal pattern emerges from our analysis regarding sources/sinks distribution of atmospheric CO<sub>2</sub> and we find that in most regions, annual mean CO<sub>2</sub> flux densities are comparable in sign and magnitude to those of the adjacent open ocean except for river dominated systems. Globally, coastal regions act as a CO<sub>2</sub> sink with a more intense uptake occurring in summer because of the disproportionate influence of high latitude coastal seas in the Northern Hemisphere. The majority of the coastal seasonal FCO<sub>2</sub> variations stems from the air-sea pCO<sub>2</sub> gradient, although changes in wind speed and sea-ice cover can also be significant regionally. To investigate further the drivers of the spatio-seasonal variability, our observation-based pCO<sub>2</sub> climatology is used in conjunction with global ocean biogeochemistry model MOM6-COBALT. The model outputs allow us to quantify the respective contributions of thermal effects, biology, and non-thermal physical processes (circulation and freshwater inputs) to seasonal variations in coastal pCO<sub>2</sub>. Generally, biological activity is the dominant driver of the pCO<sub>2</sub> seasonal variability in temperate and high latitudes while thermal and non-thermal physical processes dominate in low latitudes.</p>


2014 ◽  
Vol 119 (1) ◽  
pp. 445-460 ◽  
Author(s):  
Vincent Rossi ◽  
Amandine Schaeffer ◽  
Julie Wood ◽  
Guillaume Galibert ◽  
Brad Morris ◽  
...  

2005 ◽  
Vol 301 ◽  
pp. 199-215 ◽  
Author(s):  
MA McManus ◽  
OM Cheriton ◽  
PT Drake ◽  
DV Holliday ◽  
CD Storlazzi ◽  
...  

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