2017
Rainfall regimes of the Green Sahara
Abstract: We estimate rainfall during the “Green Sahara” period.
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Cited by 406 publications
(403 citation statements)
References 101 publications
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“…The 87 Sr/ 86 Sr analyses largely agree with δ 18 O-based salinity estimations, and provide additional indications for significant precipitation across the NW African hinterland after the suggested abrupt aridification event around 5.5 ka BP. Our data are consistent with the precipitation reconstructions of Tierney et al (2017), which also indicate the persistence of considerable rainfall until ∼3-4 ka BP. Moreover, our record is coherent with the local occupation history in the Ras el Sass area that was abandoned at ∼3 ka BP, most likely as a consequence of decreasing surface freshwater availability (Vernet and Tous, 2004).…”
Section: Resultssupporting
confidence: 89%
“…The 87 Sr/ 86 Sr analyses largely agree with δ 18 O-based salinity estimations, and provide additional indications for significant precipitation across the NW African hinterland after the suggested abrupt aridification event around 5.5 ka BP. Our data are consistent with the precipitation reconstructions of Tierney et al (2017), which also indicate the persistence of considerable rainfall until ∼3-4 ka BP. Moreover, our record is coherent with the local occupation history in the Ras el Sass area that was abandoned at ∼3 ka BP, most likely as a consequence of decreasing surface freshwater availability (Vernet and Tous, 2004).…”
Section: Resultssupporting
confidence: 89%
“…Thus, it seems possible that post-highstand Bosumtwi δ D wax may be partly biased by input of pre-aged leaf waxes, which could explain the difference to the GeoB4905-4 δ D wax record. Offshore NW Africa, δ D wax records have shown wet conditions during the AHP; in particular core GC37 displays aridification at about 5.5 ka 9 , similar to our record. This was interpreted as a rapid response at the AHP termination, although bioturbation was thought to be significant in these lower-resolution records, making direct comparisons difficult.…”
Section: Resultssupporting
confidence: 87%
“…Using the results from EC-Earth, we found that the orbit-induced Saharan vegetation collapse could affect this climate transition from humid to more arid conditions over the ME at the end of mid-Holocene. Some previous studies suggested that the ME precipitation can be affected by the Afro-Asian monsoon during the mid-Holocene (i.e., Wanner et al 2008), but we found that neither the change in North African summer monsoon (Tierney et al 2017) nor the Asian summer monsoon (Sun et al 2019) can reach the ME. Our modeling work provides a new perception for Accepted for publication in Journal of Climate.…”
Section: Discussioncontrasting
confidence: 92%
