Mingle
发表于 2025-3-25 06:30:26
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
发表于 2025-3-25 09:51:23
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长处
发表于 2025-3-25 13:39:10
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
努力赶上
发表于 2025-3-25 18:34:52
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
强有力
发表于 2025-3-25 23:59:10
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
发表于 2025-3-26 03:34:59
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Bernstein-test
发表于 2025-3-26 07:35:39
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
发表于 2025-3-26 10:04:10
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Inveterate
发表于 2025-3-26 13:15:54
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
发表于 2025-3-26 18:52:19
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