@InProceedings{Vianna:1995:PrInOs,
author = "Vianna, Marcio Luiz",
title = "Fisheries applications of the Toca monitoring program in the
Atlantic and Indian Oceans: predictability of interannual
oscillations in spiny lobster catches drives by ocean climatic
changes",
year = "1995",
pages = "830--834",
organization = "International Scientific Conference on Tropical Ocean Global
Atmosphere.",
keywords = "OCEANOGRAFIA, ECOSSISTEMAS, PESCA, ECOLOGIA COSTEIRA, BIOLOGIA
MARINHA, MUNDANCAS CLIMATICAS, OCEANOGRAPHY, MARINE ENVIRONMENTS,
ECOSYSTEMS, COASTAL ECOLOGY, MARINE BIOLOGY, CLIMATE CHANGE.",
abstract = "The spiny lobster fisheries in West Australia and Northeast Brazil
are of great socio-economic importance, involving 100 million
dollar annual exports, being the most important export items from
these regions. The ocurrence of high amplitude fluctuations in the
annual production has been arbitrarily attributed to overfishing
and predatory practices, in the case of declining catches, and to
{"}effective{"} management practices, in the case of increases in
catch. In the Brazilian case, this state of affairs has been
causing a dominance of repressive management practices and
increased loss of credibility of fisheries authorities. The recent
finding by Pearce and Phillips (1988)that oscillations in catches
off Western Australia are caused by ocean environmental
fluctuations about four years earlier, and not by variations in
fishing effort, are largely due to the availability of the good
monthly sea-level data sets in Australia. The same kind of
conclusion was reached by Polovina and MitchuM (1992)in relation
to the Hawaiian spiny lobster fishery, and Vianna and Peris
(1995)and in relation to the Northeast Brazilian spiny lobster
fishery.In the Brazilian case, a very striking independence of the
yearly catch on a wide interval of levels of fishing effort defied
explanation, indicating that a possible cause for such a stability
could necessarily be related to the existence of return paths for
the pelagic larvae, which would not be lost through the most
obvious cross-equatorial drift path via the North Brazil Current
(NBC), as some general pictures of the circulation in the South
Atlantic would suggest (Pollock, 1990). We proposed (Vianna and
Peris,1995)that this requires a drift cycle which necessarily uses
the North Brazil upstream retroflection into the South Equatorial
Undercurrent (SEUC)off Fortaleza, and a return path using the
central branch of the South Equatorial Current (SEC)which impinges
the coast of Brazil around 6S. This picture is consistent with the
findings of Molinari (see Molinari, 1982, and references
therein)and the modeling study of Schott and Boning (1991). This
is the only possibility consistent with other biological
indicators, as the presence of the two commercial species
(Panulirus . argus and Panulirus laevicauda)in Femando de Noronha,
and their absence at St.Peter and St.Paul's Rocks
(Vianna,1986)which would indicate the NBC retroflection into the
North Equatorial Countercurrent as the preferred path. The SEC
hypothesis is supported by the existence of a permanent coastal
divergence region just south of Natal, which causes the presence
of tuna and deep water lobsters at anomalously shallow depths, and
the existence of nursery grounds around Natal and Recife.",
conference-location = "Melbourne, AU",
conference-year = "1995",
label = "8978",
targetfile = "INPE 8156.pdf",
urlaccessdate = "21 maio 2024"
}