2022
DOI: 10.1016/j.quascirev.2022.107416
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The dynamics of warming during the last deglaciation in high-elevation regions of Eastern Equatorial Africa

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Cited by 14 publications
(21 citation statements)
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“…The reconstructed overall temperature ranges are, however, consistent with the elevations of the lake archives. The amplitude of temperature change over the last 13 kyr at Garba Guracha is ∼ 6 • C. Similar amplitudes of change have been reconstructed at other high-altitude sites (Lake Mahoma and Lake Rutundu) (Loomis et al, 2017;Garelick et al, 2022), whereas equatorial records at lower elevations yield lower temperature amplitudes (Lake Victoria and Lake Tanganyika) (Tierney et al, 2008;Berke et al, 2012b), and higher temperature amplitudes are also recorded in the northeast African Lake Tana (Loomis et al, 2015). In fact, Garba Guracha has some of the highest-amplitude temperature changes of all of the sites during the Holocene, perhaps because it combines high elevation with a slightly higher latitude than other terrestrial African temperature records.…”
Section: Palaeotemperature Reconstructions For the Garbasupporting
confidence: 72%
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“…The reconstructed overall temperature ranges are, however, consistent with the elevations of the lake archives. The amplitude of temperature change over the last 13 kyr at Garba Guracha is ∼ 6 • C. Similar amplitudes of change have been reconstructed at other high-altitude sites (Lake Mahoma and Lake Rutundu) (Loomis et al, 2017;Garelick et al, 2022), whereas equatorial records at lower elevations yield lower temperature amplitudes (Lake Victoria and Lake Tanganyika) (Tierney et al, 2008;Berke et al, 2012b), and higher temperature amplitudes are also recorded in the northeast African Lake Tana (Loomis et al, 2015). In fact, Garba Guracha has some of the highest-amplitude temperature changes of all of the sites during the Holocene, perhaps because it combines high elevation with a slightly higher latitude than other terrestrial African temperature records.…”
Section: Palaeotemperature Reconstructions For the Garbasupporting
confidence: 72%
“…The remaining ice in the basin might have (i) reduced the temperature of the lake water by inflow of cold meltwater and (ii) buffered the air temperature warming caused by increasing insolation. Indeed, rising temperatures were recorded in other eastern African records as early as 21 ka cal BP (Lake Mahoma) (Garelick et al, 2022) and in Ethiopia as early as 14 ka cal BP (Lake Tana) (Loomis et al, 2015;Tierney et al, 2016).…”
Section: Deglacial Warmingmentioning
confidence: 93%
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