Water masses and larval fish habitats in the Pacific tropical-subtropical convergence off Mexico

2021 ◽  
pp. 104575
Author(s):  
Fernando Contreras-Catala ◽  
Emilio J. Beier ◽  
Laura Sánchez-Velasco ◽  
Victor M. Godínez ◽  
Elvia D. Sánchez-Pérez ◽  
...  
2019 ◽  
Vol 124 (12) ◽  
pp. 9690-9705 ◽  
Author(s):  
Laura Sánchez‐Velasco ◽  
Víctor M. Godínez ◽  
Erick D. Ruvalcaba‐Aroche ◽  
Amaru Márquez‐Artavia ◽  
Emilio Beier ◽  
...  

2012 ◽  
Vol 33 ◽  
pp. 89-99 ◽  
Author(s):  
L. Sánchez-Velasco ◽  
M.F. Lavín ◽  
S.P.A. Jiménez-Rosenberg ◽  
J.M. Montes ◽  
P.J. Turk-Boyer

2017 ◽  
Vol 26 (6) ◽  
pp. 655-667 ◽  
Author(s):  
Maik Tiedemann ◽  
Heino O. Fock ◽  
Patrice Brehmer ◽  
Julian Döring ◽  
Christian Möllmann

2014 ◽  
Vol 94 (7) ◽  
pp. 1517-1530 ◽  
Author(s):  
Emilio A. Inda-Díaz ◽  
Laura Sánchez-Velasco ◽  
Miguel F. Lavín

We examined the effect of a tidal-mixing front on the three-dimensional distribution of larval fish habitats (LFHs) in the Midriff Archipelago Region in the Gulf of California during winter. Zooplankton and environmental variables were sampled from 0 to 200 m in 50 m strata. Four LFHs were defined in association with the front, two on the northern side and two on the southern side. The northern LFHs were: (1) the Mainland Shelf Habitat, located from the surface to 100 m depth on the north-east mainland shelf, characterized mainly by the presence of Citharichtys fragilis; and (2) the Wide Distribution Habitat, extending from north-west to south across the front from the surface to 200 m depth, dominated by the ubiquitous Engraulis mordax. The southern LFHs were: (3) the Eddy Zone Habitat, defined nearly on an anticyclonic eddy, with the highest larval abundance and richness from the surface to 100 m depth, dominated by Leuroglossus stilbius; and (4) the Southern Gulf Habitat, associated with low temperature waters from the southern Gulf of California, dominated by southern-gulf species (e.g. Scomber japonicus and Sardinops sagax). Despite the weak stratification and low thermal contrast (~1.5°C) across the south front compared to summer (~3°C), our results demonstrate that the frontal zone may influence the formation of planktonic habitats even during generally homogeneous periods, which may also be relevant in other regions of the world.


Water ◽  
2020 ◽  
Vol 12 (5) ◽  
pp. 1434 ◽  
Author(s):  
Yayu Yang ◽  
Xuezhi Bai

Hydrographic data from the World Ocean Database 2013 and the Chinese National Arctic Research Expedition were used to investigate the summertime changes in the eastern Chukchi Sea from 1974 to 2017. Owing to the Pacific inflow and timing of the sea ice retreat, water masses and vertical thermohaline structures in the eastern Chukchi Sea have changed but with regional differences. The entire eastern Chukchi Sea warmed up with significant temperature increase in the central shelf; however, the surface and bottom salinity in the southern, central, and northern shelves exhibited different trends. The northward extension of the Pacific Summer Water after 1997 influenced the summer hydrography significantly. Moreover, the data reveal changes in the characteristics of various water masses. Both Bering Summer Water (BSW) and Pacific Winter Water in the deeper layer became saltier, whereas the Alaskan Coastal Water in the upper layer became fresher after 1997. The previous definition of the BSW should be modified to include the warming water mass in the southern Chukchi Sea in the more recent years. Furthermore, the vertical thermohaline structure over the Chukchi shelves experienced considerable changes in its characteristics due to the combined effects of the Pacific inflow and surface forcing.


1996 ◽  
Vol 43 (4) ◽  
pp. 501-544 ◽  
Author(s):  
Susan E. Wijffels ◽  
John M. Toole ◽  
Harry L. Bryden ◽  
Rana A. Fine ◽  
William J. Jenkins ◽  
...  
Keyword(s):  

1960 ◽  
Vol 17 (1) ◽  
pp. 91-112 ◽  
Author(s):  
J. P. Tully ◽  
F. G. Barber

It is shown that the features of an estuarine system occur northward of a sub-Arctic boundary in the Pacific Ocean.The limit of downward mixing from the surface is the limit (L) of the halocline. This is defined by a discontinuity in the logarithmic plot of salinity structure, where the salinity is nearly constant (33.8 ± 0.1‰). On this surface the transfer is uni-directional upward. Here the water masses being entrained into the halocline and upper zone may be identified by their temperature alone.


Sign in / Sign up

Export Citation Format

Share Document