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- W4295346229 abstract "Arctic sea ice retreat is linked to extrapolar thermal energy import, while the potential impact of pan-Arctic river heat discharge on sea-ice loss has been unresolved. We reconstructed the Holocene history of Arctic sea ice and Russian pan-Arctic river heat discharge, combining ice-rafted debris records and sedimentation rates from the East Siberian Arctic Shelf with a compilation of published paleoclimate and observational data. In the mid-Holocene, the early summer (June-July) solar insolation was higher than that during the late Holocene, which led to a larger heat discharge of the Russian pan-Arctic rivers and contributed to more Arctic sea ice retreat. This intensified decline of early-summer sea ice accelerated the melting of sea ice throughout the summertime by lowering regional albedos. Our findings highlight the important impact of the larger heat discharge of pan-Arctic rivers, which can reinforce Arctic sea-ice loss in the summer in the context of global warming." @default.
- W4295346229 created "2022-09-13" @default.
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- W4295346229 date "2022-09-13" @default.
- W4295346229 modified "2023-10-15" @default.
- W4295346229 title "Enhanced Arctic sea ice melting controlled by larger heat discharge of mid-Holocene rivers" @default.
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- W4295346229 doi "https://doi.org/10.1038/s41467-022-33106-1" @default.
- W4295346229 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/36100586" @default.
- W4295346229 hasPublicationYear "2022" @default.
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