Palavras-chave
dióxido de carbono. Aquecimento global antropogênico.
Como Citar
Resumo
A periódica mudança climática na Terra pode ser explicada por um número reduzido de fatores terrestres e astronômicos. Nas escalas anual/diária, o clima obedece aos movimentos de translação e de rotação. Ciclos climáticos de períodos médios (décadas/séculos/milênios) relacionam-se a mudanças na radiação solar, provocadas pela influência de grandes planetas do Sistema Solar. As oscilações oceânicas (ordem decadal) são possivelmente causadas por influências planetárias e lunares. Ciclos climáticos longos (dezenas a centenas de milhares de anos) são causados por variações nos parâmetros da órbita da Terra (excentricidade, obliquidade e precessão). Eventos de impacto de grandes corpos no planeta e extinções em massa de espécies advêm de superciclos (dezenas de milhões de anos) provocados pela oscilação vertical do Sistema Solar em relação ao plano galáctico. Tectonismo, vulcanismo e a evolução de supercontinentes exibem superciclos (centenas de milhões de anos) induzidos pelo deslocamento do Sistema Solar ao redor do centro da Via Láctea e pela variação de raios cósmicos. Fatores astronômicos permeiam praticamente todas as ordens dos ciclos climáticos e atuam direta ou indiretamente nos processos bio-geo-oceânico-atmosféricos. Conclui-se que o clima na Terra é caracterizado por ciclos controlados astronomicamente pela Lua, o Sol, os planetas, o Sistema Solar e, até mesmo, a Galáxia.
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