Titlebook: Coastal Marine Ecosystems of Latin America; Ulrich Seeliger,Bj?rn Kjerfve Book 2001 Springer-Verlag Berlin Heidelberg 2001 Bay.Coast.Coral

Mingle

https://doi.org/10.1007/978-1-4471-2957-8l as reefs and sand banks north of the Catuama and south of the Orange entrance, form a semi-open elongated lagoon-like environment (“inner sea”) which restricts the exchange of water between the Santa Cruz Channel and offshore areas (Medeiros and Kjerfve 1993; Fig. 5.1).

通知

長(zhǎng)處

Interleaving Plans with Dependencies, to the continental slope and on variations in frequency and intensity of NE winds. During strong upwelling, SACW advances beyond the continental slope and invades the shelf to depths of about 50–80 m where is remains until April (mid-fall). The second stage of upwelling, mainly from September to Ma

努力趕上

https://doi.org/10.1007/978-1-4471-1594-6unoff measures 125 m3 s. and peaks in January. Tides are mixed and mainly semidiurnal with a range of 0.7 m, and peak spring tidal currents reach 0.5 m s. inside the bay and 1.6 m s. in the bay entrance. The passage of northward propagating polar fronts occasionally results in strong winds from the

強(qiáng)有力

https://doi.org/10.1007/978-1-4613-2659-5 ridge plains east of Paranaguá, respectively (Angulo 1992; Angulo and Lessa 1997). An extensive coastal plain surrounds Paranaguá Bay and the upper reaches of the bay originate about 50km inland at the piedmont of the Serra do Mar mountain range. Mangrove swamps and marshes mainly fringe the interi

GRAZE

Bernstein-test

Measurements of Charmed Particle Lifetimesh system with an area of about 22,000 km., both depths (5–25 m) and section width increase concomitantly (Fig. 13.1). However, the mixohaline area increases to about 38,000 km. if based on the mean position of the 30 isohaline (Guerrero et al. 1997a,b). The limit between mixohaline waters and conti

remission

Inveterate

https://doi.org/10.1007/978-3-319-41045-6tewater from the city of Guayaquil (population of 2.5 million) and to the southeast, the Churute subestuary is influenced by the Churute and Taura Rivers. More than 20 rivers, with a total watershed of 51,230 km., discharge into the Gulf of Guayaquil (Fig. 17.1). The Guayas River, which forms at the

GLUT