scholarly journals Trophic structure and food resources of epipelagic and mesopelagic fishes in the North Pacific Subtropical Gyre ecosystem inferred from nitrogen isotopic compositions

2015 ◽  
Vol 60 (4) ◽  
pp. 1156-1171 ◽  
Author(s):  
C. Anela Choy ◽  
Brian N. Popp ◽  
Cecelia C. S. Hannides ◽  
Jeffrey C. Drazen
Keyword(s):  
North Pacific ◽  
Trophic Structure ◽  
Food Resources ◽  
Subtropical Gyre ◽  
North Pacific Subtropical Gyre ◽  
Isotopic Compositions ◽  
The North ◽  
The North Pacific

scholarly journals Euphotic zone metabolism in the North Pacific Subtropical Gyre based on oxygen dynamics

2020 ◽  
Author(s):  
Sara Ferron ◽  
Benedetto Barone ◽  
Matthew J Church ◽  
Angelicque E. White ◽  
David M. Karl
Keyword(s):  
North Pacific ◽  
Euphotic Zone ◽  
Subtropical Gyre ◽  
North Pacific Subtropical Gyre ◽  
The North ◽  
Oxygen Dynamics ◽  
The North Pacific

Weakening and Poleward Shifting of the North Pacific Subtropical Fronts from 1980 to 2018

2021 ◽  
Keyword(s):  
Mixed Layer ◽  
North Pacific ◽  
Subtropical Gyre ◽  
Hadley Cell ◽  
North Pacific Subtropical Gyre ◽  
Mode Water ◽  
Mode Waters ◽  
The North ◽  
The North Pacific ◽  
Subtropical Fronts

Abstract Recent evidence shows that the North Pacific subtropical gyre, the Kuroshio Extension (KE) and Oyashio Extension (OE) fronts have moved poleward in the past few decades. However, changes of the North Pacific Subtropical Fronts (STFs), anchored by the North Pacific subtropical countercurrent in the southern subtropical gyre, remain to be quantified. By synthesizing observations, reanalysis, and eddy-resolving ocean hindcasts, we show that the STFs, especially their eastern part, weakened (20%±5%) and moved poleward (1.6°±0.4°) from 1980 to 2018. Changes of the STFs are modified by mode waters to the north. We find that the central mode water (CMW) (180°-160°W) shows most significant weakening (18%±7%) and poleward shifting (2.4°±0.9°) trends, while the eastern part of the subtropical mode water (STMW) (160°E-180°) has similar but moderate changes (10% ± 8%; 0.9°±0.4°). Trends of the western part of the STMW (140°E-160°E) are not evident. The weakening and poleward shifting of mode waters and STFs are enhanced to the east and are mainly associated with changes of the northern deep mixed layers and outcrop lines—which have a growing northward shift as they elongate to the east. The eastern deep mixed layer shows the largest shallowing trend, where the subduction rate also decreases the most. The mixed layer and outcrop line changes are strongly coupled with the northward migration of the North Pacific subtropical gyre and the KE/OE jets as a result of the poleward expanded Hadley cell, indicating that the KE/OE fronts, mode waters, and STFs change as a whole system.

scholarly journals 2P271 Flow cytometry identification of nanocyanobacteria and their limiting factors in the North Pacific Subtropical Gyre(23. Ecology & Environment,Poster)

2013 ◽  
Vol 53 (supplement1-2) ◽  
pp. S203
Author(s):  
Mathias Girault ◽  
Hisayuki Arakawa ◽  
Gerald Gregori ◽  
Fuminori Hashihama ◽  
Hyonchol Kim ◽  
...  
Keyword(s):  
Flow Cytometry ◽  
North Pacific ◽  
Subtropical Gyre ◽  
Limiting Factors ◽  
North Pacific Subtropical Gyre ◽  
The North ◽  
The North Pacific

scholarly journals Microbiome of Trichodesmium Colonies from the North Pacific Subtropical Gyre

2017 ◽  
Vol 8 ◽  
Author(s):  
Mary R. Gradoville ◽  
Byron C. Crump ◽  
Ricardo M. Letelier ◽  
Matthew J. Church ◽  
Angelicque E. White
Keyword(s):  
North Pacific ◽  
Subtropical Gyre ◽  
North Pacific Subtropical Gyre ◽  
The North ◽  
The North Pacific
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