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- W4296578834 abstract "The ocean stores the bulk of anthropogenic heat in the Earth system. The ocean heat uptake efficiency (OHUE) -- the flux of heat into the ocean per degree of global warming -- is therefore a key factor in how much warming will occur in the coming decades. In climate models, OHUE is well-characterised, tending to decrease on centennial timescales; in contrast, OHUE is not well-constrained from Earth observations. Here OHUE and its rate of change are diagnosed from global temperature and ocean heat content records. OHUE increased over the past five decades by 0.19$pm$0.04 W/m$^2$K, and was on average 0.58$pm$0.08 W/m$^2$K during this period. This increase is attributed to steepening anthropogenic heat gradients in the ocean, and corresponds to several years' difference in when temperature targets such as 1.5$^circ$C or 2$^circ$C are exceeded." @default.
- W4296578834 created "2022-09-22" @default.
- W4296578834 creator A5015264022 @default.
- W4296578834 date "2022-09-23" @default.
- W4296578834 modified "2023-09-27" @default.
- W4296578834 title "Ocean heat uptake efficiency increase since 1970" @default.
- W4296578834 doi "https://doi.org/10.31223/x52m07" @default.
- W4296578834 hasPublicationYear "2022" @default.
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