Incidental Capture of Juvenile Fish from an Artisanal Fishery in a Coastal Lagoon in the Gulf of California

2009 ◽  
Vol 29 (1) ◽  
pp. 245-255 ◽  
Author(s):  
Felipe Amezcua ◽  
Juan Madrid-Vera ◽  
Hugo Aguirre
1999 ◽  
Vol 38 (9) ◽  
pp. 837-841 ◽  
Author(s):  
J.G Galindo-Reyes ◽  
V.U Fossato ◽  
C Villagrana-Lizarraga ◽  
F Dolci

2018 ◽  
Vol 200 ◽  
pp. 960-970
Author(s):  
Federico Páez-Osuna ◽  
Luis Miguel Flores-Campaña ◽  
Carlos Karam-Quiñones ◽  
Adreissa Lizette Páez-Michel ◽  
Cesar Julio Saucedo-Barrón ◽  
...  

2017 ◽  
Vol 33 (5) ◽  
pp. 1051-1054 ◽  
Author(s):  
N. R. Ehemann ◽  
X. A. Pérez-Palafox ◽  
P. Mora-Zamacona ◽  
M. I. Burgos-Vázquez ◽  
A. F. Navia ◽  
...  

2016 ◽  
Vol 104 (1-2) ◽  
pp. 83-91 ◽  
Author(s):  
J.G. Cardoso-Mohedano ◽  
F. Páez-Osuna ◽  
F. Amezcua-Martínez ◽  
A.C. Ruiz-Fernández ◽  
G. Ramírez-Reséndiz ◽  
...  

2013 ◽  
Vol 83 ◽  
pp. 75-80 ◽  
Author(s):  
Mauricio Carrasquilla-Henao ◽  
Héctor A. González Ocampo ◽  
Antonio Luna González ◽  
Gerardo Rodríguez Quiroz

2003 ◽  
Vol 57 (1-2) ◽  
pp. 99-109 ◽  
Author(s):  
Juan A. Dworak ◽  
José Gómez-Valdés

2020 ◽  
Vol 158 ◽  
pp. 111417
Author(s):  
Alberto Sánchez ◽  
Adriana Gómez-León ◽  
Habacuc Pérez-Tribouillier ◽  
Néstor Rey-Villiers ◽  
Ma. Concepción Ortiz-Hernández ◽  
...  

Atmosphere ◽  
2020 ◽  
Vol 11 (6) ◽  
pp. 626 ◽  
Author(s):  
Lidia Irene Benítez-Valenzuela ◽  
Zulia Mayari Sanchez-Mejia

Despite the critical role latent (LE) and sensible (H) heat play in turbulent processes and heat exchange in the water–air interface, there is a lack of studies of turbulent fluxes over the surface in semiarid regions. We collected continuous measurements of net radiation (Rn), LE, H, and micrometeorological data at a coastal lagoon in the Gulf of California during 2019 with an eddy covariance (EC) system. We analyzed the time series, considering the North American Monsoon System, the pre-monsoon, and post-monsoon season. Results show that Rn (276 ± 118 W m−2) and turbulent fluxes were higher during the monsoon season (July–September) LE (129 ± 18 W m−2), and H (29 ± 9 W m−2). The monthly average of Rn, LE, and H was highest in June (493.9 W m−2), August (142 W m−2), and May (50 W m−2), respectively. Furthermore, during the monsoon season, the (H + LE)/Rn ratio (0.74) suggests that more than half of the Rn reaching the coastal lagoon is used for the turbulent exchange of LE and H. During the pre-monsoon, LE (r2 = 0.36) increases with a higher vapor pressure deficit (VPD), while H (r2 = 0.66) increases with a higher friction velocity (u*) during the monsoon season. Quantitative observations are essential for further research.


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