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The lapse-rate feedback is the dominant driver of stronger warming in the Arctic than the Antarctic in simulations with increased CO2. While Antarctic surface elevation has been implicated in promoting a weaker Antarctic lapse-rate feedback, the mech
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0546afcb8bde83b47c46ac2b9c8fc3e
https://doi.org/10.31223/osf.io/6fbjk
https://doi.org/10.31223/osf.io/6fbjk
