Abstract
The climate response to a massive release of methane from gas hydrates is simulated in two 2500-year-long numerical experiments performed with a three-dimensional, global coupled atmosphere-sea ice-ocean model of intermediate complexity. Two different equilibrium states were used as reference climates; the first state with preindustrial forcing conditions and the second state with a four times higher atmospheric CO
Original language | English |
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Journal | Paleoceanography |
Volume | 19 |
DOIs | |
Publication status | Published - 2004 |