The CLME+ Strategic Action Programme: An ecosystems approach for assessing and managing the Caribbean Sea and North Brazil Shelf Large Marine Ecosystems

2017 ◽  
Vol 22 ◽  
pp. 191-205 ◽  
Author(s):  
Patrick Debels ◽  
Lucia Fanning ◽  
Robin Mahon ◽  
Patrick McConney ◽  
Laverne Walker ◽  
...  
2020 ◽  
Vol 12 (2) ◽  
pp. 100-112
Author(s):  
Carolina Mercedes Laurent Singh ◽  
Jamerson Aguiar‐Santos ◽  
Efrem Jorge Gondim Ferreira ◽  
Eucaris del Carmen Evaristo ◽  
Carlos Edwar de Carvalho Freitas

2007 ◽  
Vol 25 (2) ◽  
pp. 331-340 ◽  
Author(s):  
R. C. Cruz Gómez ◽  
S. N. Bulgakov

Abstract. The North Brazil Current Rings (NBCR) penetration into the Caribbean Sea is being investigated by employing a merged altimeter-derived sea height anomaly (TOPEX/Poseidon, Jason-1 and ERS-1, 2), the ocean surface color data (SeaWiFS) and Global Drifter Program information. Four strategies are being applied to process the data: (1) calculations of the Okubo-Weiss parameter for NBCR identification, (2) longitude-time plots (also known as Hovmöller diagrams), (3) two-dimensional Radon transforms and (4) two-dimensional Fourier transforms. A twofold NBCR structure has been detected in the region under investigation. The results have shown that NBC rings mainly propagate into the Caribbean Sea along two principal pathways (near 12° N and 17° N) in the ring translation corridor. Thus, rings following the southern pathway in the fall-winter period can enter through very shallow southern straits as non-coherent structures. A different behavior is observed near the northern pathway (~17° N), where NBC rings are thought to have a coherent structure during their squeezing into the eastern Caribbean, i.e. conserving the principal characteristics of the incident rings. We attribute this difference in the rings' behavior to the vertical scales of the rings and to the bottom topography features in the vicinity of the Lesser Antilles.


Zootaxa ◽  
2007 ◽  
Vol 1557 (1) ◽  
pp. 33-45 ◽  
Author(s):  
IVÁN HERNÁNDEZ-ÁVILA ◽  
ALFREDO GÓMEZ ◽  
CARLOS LIRA ◽  
LEE GALINDO

The crustacean decapod fauna of Cubagua Island in the Caribbean Sea, Venezuela, an island much affected by coastal upweling, was surveyed. A total of 178 species from 41 families were recorded, of which 56 species were new records for the island; eigth genera and six species were new records for Venezuela. Most species had previously been recorded from the the Caribbean province, 19.7% were endemic for the province, 64.1% had affinities to the Brazilian province, 57.3% to the Texan and Carolinian provinces and 45.5% showed continuous distributions across the provinces but showing less endemism and more affinities with Brazilian province than the general trends of distributions of decapods in the Caribbean. It appears that upwelling processes around the island hinders the development of the typical Caribbean marine ecosystems. The proximity with the northern limit of the Brazilian province also affects the biodiversity of the island.


2012 ◽  
Vol 42 (11) ◽  
pp. 2041-2055 ◽  
Author(s):  
Julien Jouanno ◽  
Julio Sheinbaum ◽  
Bernard Barnier ◽  
Jean Marc Molines ◽  
Julio Candela

Abstract Variability of the mesoscale eddy field in the Caribbean Sea is analyzed over the period 1993–2009 using geostrophic anomalies derived from altimeter data and a high-resolution regional model. The Colombia Basin presents the largest values of eddy kinetic energy (EKE) and its semiannual cycle, with a main peak in August–October and a secondary peak in February–March, is the dominant feature in the whole Caribbean EKE cycle. The analysis of energy conversion terms between low-frequency currents and eddies explains these peaks by enhanced baroclinic and barotropic instabilities, in response to seasonally varying currents in the region of the Guajira Peninsula. The semiannual acceleration of the atmospheric Caribbean low-level jet intensifies the southern Caribbean Current (sCC) twice a year in this region, together with its vertical and horizontal velocity shears. The asymmetry of the EKE seasonal cycle in the Colombia Basin is explained by a summer peak in the annual cycle of the whole sCC. Numerical results suggest that the arrival of more energetic North Brazil Current rings during part of the year have almost no impact on the seasonal cycle of EKE in the Colombia Basin. Instead, they are shown to contribute, together with the annual cycle of the Caribbean inflow through the southern passages of the Lesser Antilles, to an annual peak of EKE in the Venezuela Basin between May and August. At the interannual scale the mechanism is similar: interannual variability of the alongshore wind stress controls the speed of the southern Caribbean Current and the energy of the eddies in the Colombia Basin through instability.


2009 ◽  
Vol 56 (7) ◽  
pp. 1057-1076 ◽  
Author(s):  
Christian Mertens ◽  
Monika Rhein ◽  
Maren Walter ◽  
Kerstin Kirchner

2017 ◽  
Vol 22 ◽  
pp. 1-8 ◽  
Author(s):  
Kenneth Sherman ◽  
Norma Patricia Muñoz Sevilla ◽  
Porfirio Álvarez Torres ◽  
Betsy Peterson

2014 ◽  
Vol 29 (6) ◽  
pp. 508-517 ◽  
Author(s):  
Alberto M. Mestas‐Nuñez ◽  
Peter Molnar
Keyword(s):  
Ice Age ◽  

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