scholarly journals SEA-SURFACE TEMPERATURE SUMMARY FOR THE NORTHWESTERN GULF OF MEXICO, 1912–33

1935 ◽  
Vol 63 (4) ◽  
pp. 147-148
Author(s):  
GILES SLOCUM
2020 ◽  
Vol 48 (3) ◽  
pp. 406-420
Author(s):  
Javier E. Viana-Morayta ◽  
Yassir E. Torres-Rojas ◽  
Jaime Camalich-Carpizo

The current study examined the stomach contents of the Atlantic sharpnose shark (Rhizoprionodon terraenovae) in the southern Gulf of Mexico during 2015 to understand the relationship between diet and changes in sea surface temperature (SST). Prey-specific index of relative importance (%PSIRI), diet breadth (Bi), trophic level (TrL), and trophic overlap (PERMANOVA) were calculated between sexes, body size, and climatic seasons (dry, rainy and winter storm). The lowest temperature recorded in the area was during February (23.9°C), and the highest was during August (29.1°C). A total of 124 stomachs were analyzed, with 54.84% containing food. The trophic spectrum was composed of 32 identified prey, with demersal fish (Haemulon plumierii; %PSIRI = 22.82) and pelagic fish (Sardinella aurita; %PSIRI = 12.83) being the most important. According to the diet breadth (Bi = 0.002), Costello's graph, and trophic level (TrL = 4.2), R. terraenovae is a specialist tertiary consumer. PERMANOVA indicated significant trophic differences between sexes (F = 32.22; P < 0.05), body size (F = 13.68; P < 0.05), and among climatic seasons (F = 23.86; P < 0.05). Spearman's correlation indicated a negative relationship between the diversity of prey consumed by R. terraenovae and sea surface temperature (r = -0.75; P < 0.05). Therefore, diet for R. terraenovae is associated with SST, allowing for the development of possible scenarios related to climatic phenomena like climate change.


2019 ◽  
Vol 32 (14) ◽  
pp. 4263-4280 ◽  
Author(s):  
Geidy Rodriguez-Vera ◽  
Rosario Romero-Centeno ◽  
Christopher L. Castro ◽  
Víctor Mendoza Castro

Abstract This work describes dominant patterns of coupled interannual variability of the 10-m wind and sea surface temperature in the Caribbean Sea and the Gulf of Mexico (CS&GM) during the period 1982–2016. Using a canonical correlation analysis (CCA) between the monthly mean anomalies of these fields, four coupled variability modes are identified: the dipole (March–April), transition (May–June), interocean (July–October), and meridional-wind (November–February) modes. Results show that El Niño–Southern Oscillation (ENSO) influences almost all the CS&GM coupled modes, except the transition mode, and that the North Atlantic Oscillation (NAO) in February has a strong negative correlation with the dipole and transition modes. The antisymmetric relationships found between the dipole mode and the NAO and ENSO indices confirm previous evidence about the competing remote forcings of both teleconnection patterns on the tropical North Atlantic variability. Precipitation in the CS and adjacent oceanic and land areas is sensitive to the wind–SST coupled variability modes from June to October. These modes seem to be strongly related to the interannual variability of the midsummer drought and the meridional migration of the intertropical convergence zone in the eastern Pacific. These findings may eventually lead to improving seasonal predictability in the CS&GM and surrounding land areas.


2012 ◽  
Vol 64 (5) ◽  
pp. 956-965 ◽  
Author(s):  
Iliana Chollett ◽  
Frank E. Müller-Karger ◽  
Scott F. Heron ◽  
William Skirving ◽  
Peter J. Mumby

2020 ◽  
Author(s):  
Geidy Rodríguez-Vera ◽  
Rosario Romero-Centeno ◽  
Christopher L. Castro ◽  
Víctor Mendoza Castro

&lt;p&gt;This work describes dominant patterns of coupled interannual variability of the 10-m wind and sea surface temperature in the Caribbean Sea and the Gulf of Mexico (CS&amp;GM) during the period 1982&amp;#8211;2016. Using a canonical correlation analysis (CCA) between the monthly mean anomalies of these fields, four coupled variability modes are identified: the dipole (March&amp;#8211;April), transition (May&amp;#8211;June), interocean (July&amp;#8211;October), and meridional-wind (November&amp;#8211;February) modes. Results show that El Ni&amp;#241;o&amp;#8211;Southern Oscillation (ENSO) influences almost all the CS&amp;GM coupled modes, except the transition mode, and that the North Atlantic Oscillation (NAO) in February has a strong negative correlation with the dipole and transition modes. The antisymmetric relationships found between the dipole mode and the NAO and ENSO indices confirm previous evidence about the competing remote forcings of both teleconnection patterns on the tropical North Atlantic variability. Precipitation in the CS and adjacent oceanic and land areas is sensitive to the wind&amp;#8211;SST coupled variability modes from June to October. These modes seem to be strongly related to the interannual variability of the midsummer drought and the meridional migration of the intertropical convergence zone in the eastern Pacific. These findings may eventually lead to improving seasonal predictability in the CS&amp;GM and surrounding land areas.&lt;/p&gt;


2021 ◽  
Author(s):  
Mingqiu Hou ◽  
Guangsheng Zhuang ◽  
et al.

Table S1: Leaf wax isotopic records in the Gulf of Mexico; Table S2: Reconstructions of mean annual precipitation based on leaf wax carbon isotopic records; Table S3: Sea surface temperature reconstructions; Table S4: Leaf wax isotopic records of modern trees.


Sign in / Sign up

Export Citation Format

Share Document