Abstract
It is an open question to what extent wetlands contributed to the interglacial‐glacial
decrease in atmospheric methane concentration. Here we estimate methane emissions
from glacial wetlands, using newly available PMIP2 simulations of the Last Glacial
Maximum (LGM) climate from coupled atmosphere‐ocean and atmosphere‐oceanvegetation
models. These simulations apply improved boundary conditions resulting in
better agreement with
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