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DOI | 10.1038/s41558-021-01152-0 |
Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change | |
Liu M.; Vecchi G.; Soden B.; Yang W.; Zhang B. | |
发表日期 | 2021 |
ISSN | 1758-678X |
起始页码 | 848 |
结束页码 | 853 |
卷号 | 11期号:10 |
英文摘要 | The large-scale moistening of the atmosphere in response to increasing greenhouse gases amplifies the existing patterns of precipitation minus evaporation (P − E), which, in turn, amplifies the spatial contrast in sea surface salinity. Here, by performing a series of transient CO2 doubling experiments, we demonstrate that surface salinification driven by the amplified dry conditions (P − E < 0), primarily in the subtropical ocean, accelerates ocean heat uptake. The salinification also drives the sequestration of upper-level heat into the deeper ocean, reducing the thermal stratification and increasing the heat uptake through positive feedback. The change in Atlantic Meridional Overturning Circulation due to salinification has a secondary role in heat uptake. Consistent with the heat uptake changes, the transient climate response would increase by approximately 0.4 K without this process. Observed multidecadal changes in subsurface temperature and salinity resemble those simulated, indicating that anthropogenically forced changes in salinity are probably enhancing ocean heat uptake. © 2021, The Author(s), under exclusive licence to Springer Nature Limited. |
来源期刊 | Nature Climate Change
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/237220 |
作者单位 | Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, United States; Department of Geosciences, Princeton University, Princeton, NJ, United States; Princeton Environmental Institute, Princeton University, Princeton, NJ, United States |
推荐引用方式 GB/T 7714 | Liu M.,Vecchi G.,Soden B.,et al. Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change[J],2021,11(10). |
APA | Liu M.,Vecchi G.,Soden B.,Yang W.,&Zhang B..(2021).Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change.Nature Climate Change,11(10). |
MLA | Liu M.,et al."Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change".Nature Climate Change 11.10(2021). |
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