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• W1606956086 abstract "[1] The ‘Mystery Interval’ (17.5–14.5 ka BP) is characterized by a large decline in atmospheric Δ14C synchronous with an increase in atmospheric CO2. The most widely accepted hypothesis to explain these observed shifts involves the existence of an isolated ‘old’ ocean carbon reservoir that was subsequently ventilated. Here we use the UVic Earth System Climate Model to locate a potential carbon rich and Δ14C depleted water mass under 17.5 ka BP boundary conditions. We then investigate two mechanisms for the potential ventilation of such a reservoir, namely the weakening of the North Atlantic Meridional Overturning due to iceberg calving and latitudinal shifts in Southern Hemisphere Westerlies (SHW) due to southern hemispheric warming. We find that simulations derived from an equilibrium state forced with present-day SHW and moderate North Atlantic Deep Water (NADW) formation are in better agreement with atmospheric and ocean Δ14C reconstructions than simulations derived from an equilibrium state forced with a northward shifted SHW belt resulting in a shut-down of the Atlantic Meridional Overturning and formation of North Pacific Deep Water. For simulations with present-day SHW, the oldest water masses are found in the North Pacific, although the Southern Ocean cannot be ruled out as a potential ‘Mystery Reservoir’. According to our simulations, the strength of Atlantic overturning is the dominant mechanism in increasing the ocean-atmosphere carbon flux, while shifting SHW results in a rearrangement of deep ocean carbon largely between the Atlantic and Pacific basins. In our ‘best case’ scenario, the model can account for 58% of the atmospheric CO2 increase and 48% of the atmospheric Δ14C decline. While the rate of ventilation and the age of ventilated water masses are comparable with observations, the ventilation in the model could not be sustained long enough to account for the full excursion seen in paleodata." @default.
• W1606956086 created "2016-06-24" @default.
• W1606956086 creator A5009719935 @default.
• W1606956086 creator A5012473459 @default.
• W1606956086 date "2012-11-14" @default.
• W1606956086 modified "2023-10-01" @default.
• W1606956086 title "Oceanic carbon and water masses during the Mystery Interval: A model-data comparison study" @default.
• W1606956086 cites W1501961051 @default.
• W1606956086 cites W1508130212 @default.
• W1606956086 cites W1531433086 @default.
• W1606956086 cites W1566807995 @default.
• W1606956086 cites W1593116295 @default.
• W1606956086 cites W1666444433 @default.
• W1606956086 cites W1668155428 @default.
• W1606956086 cites W1676501496 @default.
• W1606956086 cites W1711109436 @default.
• W1606956086 cites W1964950613 @default.
• W1606956086 cites W1965509371 @default.
• W1606956086 cites W1969195701 @default.
• W1606956086 cites W1974540405 @default.
• W1606956086 cites W1977293647 @default.
• W1606956086 cites W1977355907 @default.
• W1606956086 cites W1978064540 @default.
• W1606956086 cites W1980203794 @default.
• W1606956086 cites W1981309347 @default.
• W1606956086 cites W1981976147 @default.
• W1606956086 cites W1983349253 @default.
• W1606956086 cites W1985246090 @default.
• W1606956086 cites W1986496434 @default.
• W1606956086 cites W1991170456 @default.
• W1606956086 cites W1995845231 @default.
• W1606956086 cites W2000444336 @default.
• W1606956086 cites W2000766006 @default.
• W1606956086 cites W2001072306 @default.
• W1606956086 cites W2002717773 @default.
• W1606956086 cites W2004587064 @default.
• W1606956086 cites W2008401121 @default.
• W1606956086 cites W2011374672 @default.
• W1606956086 cites W2012434986 @default.
• W1606956086 cites W2014727327 @default.
• W1606956086 cites W2017344048 @default.
• W1606956086 cites W2018156694 @default.
• W1606956086 cites W2022498420 @default.
• W1606956086 cites W2022977692 @default.
• W1606956086 cites W2023542692 @default.
• W1606956086 cites W2025833891 @default.
• W1606956086 cites W2029446893 @default.
• W1606956086 cites W2034543862 @default.
• W1606956086 cites W2035587516 @default.
• W1606956086 cites W2035800339 @default.
• W1606956086 cites W2042476750 @default.
• W1606956086 cites W2046492186 @default.
• W1606956086 cites W2051126029 @default.
• W1606956086 cites W2060812013 @default.
• W1606956086 cites W2060839089 @default.
• W1606956086 cites W2062983418 @default.
• W1606956086 cites W2063409788 @default.
• W1606956086 cites W2073259396 @default.
• W1606956086 cites W2074440988 @default.
• W1606956086 cites W2074482550 @default.
• W1606956086 cites W2076254583 @default.
• W1606956086 cites W2077457915 @default.
• W1606956086 cites W2079487889 @default.
• W1606956086 cites W2082763329 @default.
• W1606956086 cites W2083986366 @default.
• W1606956086 cites W2083987367 @default.
• W1606956086 cites W2084428435 @default.
• W1606956086 cites W2086797840 @default.
• W1606956086 cites W2087991745 @default.
• W1606956086 cites W2094173026 @default.
• W1606956086 cites W2094759330 @default.
• W1606956086 cites W2102622779 @default.
• W1606956086 cites W2111833217 @default.
• W1606956086 cites W2112236890 @default.
• W1606956086 cites W2112350769 @default.
• W1606956086 cites W2117920489 @default.
• W1606956086 cites W2118885545 @default.
• W1606956086 cites W2122363754 @default.
• W1606956086 cites W2126730472 @default.
• W1606956086 cites W2131537194 @default.
• W1606956086 cites W2135546271 @default.
• W1606956086 cites W2143666789 @default.
• W1606956086 cites W2151857876 @default.
• W1606956086 cites W2156924943 @default.
• W1606956086 cites W2161926766 @default.
• W1606956086 cites W2163092193 @default.
• W1606956086 cites W2163961280 @default.
• W1606956086 cites W2165943358 @default.
• W1606956086 cites W2171106889 @default.
• W1606956086 cites W2173251738 @default.
• W1606956086 cites W2175318910 @default.
• W1606956086 cites W2175906253 @default.
• W1606956086 cites W2176978061 @default.
• W1606956086 cites W2491678165 @default.
• W1606956086 cites W4211135859 @default.
• W1606956086 doi "https://doi.org/10.1029/2012pa002368" @default.
• W1606956086 hasPublicationYear "2012" @default.
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