Evolution of African Climate

Author(s):  
Daniel A. Livingstone
Keyword(s):  
2012 ◽  
Vol 2012 ◽  
pp. 1-3
Author(s):  
Gregory S. Jenkins ◽  
Alessandra Giannini ◽  
Amadou Gaye ◽  
Andrea Sealy

Science ◽  
2008 ◽  
Vol 322 (5899) ◽  
pp. 252-255 ◽  
Author(s):  
J. E. Tierney ◽  
J. M. Russell ◽  
Y. Huang ◽  
J. S. S. Damste ◽  
E. C. Hopmans ◽  
...  

2016 ◽  
Vol 404 ◽  
pp. 208-209
Author(s):  
M.H. Simon ◽  
M. Ziegler ◽  
I.R. Hall ◽  
S. Barker ◽  
C. Stringer

2021 ◽  
Author(s):  
Stefanie Kaboth-Bahr ◽  
William D. Gosling ◽  
Ralf Vogelsang ◽  
André Bahr ◽  
Eleanor M.L. Scerri ◽  
...  

<p>In this study we synthesize terrestrial and marine proxy records spanning the last 620,000 years, to decipher pan-African climate variability, its drivers and potential linkages to hominin evolution. We find a tight correlation between moisture availability across Africa to Walker and Hadley Circulation variability that were most likely driven by changes in Earth´s eccentricity. Our results demonstrate that low latitude insolation rather than glacial-interglacial cyclicity was the predominant driver of pan-African climate change during the mid to late Pleistocene. We argue that these low-latitude climate processes governed the dispersion and evolution of vegetation, as well as mammals, in eastern and western Africa, ultimately by increasing resource-rich and stable ecotonal settings that have long thought to have been the preferred habitats of hominins.</p>


2018 ◽  
Vol 9 (4) ◽  
pp. 1261-1278 ◽  
Author(s):  
Brahima Koné ◽  
Arona Diedhiou ◽  
N'datchoh Evelyne Touré ◽  
Mouhamadou Bamba Sylla ◽  
Filippo Giorgi ◽  
...  

Abstract. The latest version of RegCM4 with CLM4.5 as a land surface scheme was used to assess the performance and sensitivity of the simulated West African climate system to different convection schemes. The sensitivity studies were performed over the West African domain from November 2002 to December 2004 at a spatial resolution of 50 km × 50 km and involved five convective schemes: (i) Emanuel; (ii) Grell; (iii) Emanuel over land and Grell over ocean (Mix1); (iv) Grell over land and Emanuel over ocean (Mix2); and (v) Tiedtke. All simulations were forced with ERA-Interim data. Validation of surface temperature at 2 m and precipitation were conducted using data from the Climate Research Unit (CRU), Global Precipitation Climatology Project (GPCP) and the Tropical Rainfall Measurement Mission (TRMM) during June to September (rainy season), while the simulated atmospheric dynamic was compared to ERA-Interim data. It is worth noting that the few previous similar sensitivity studies conducted in the region were performed using BATS as a land surface scheme and involved less convective schemes. Compared with the previous version of RegCM, RegCM4-CLM also shows a general cold bias over West Africa whatever the convective scheme used. This cold bias is more reduced when using the Emanuel convective scheme. In terms of precipitation, the dominant feature in model simulations is a dry bias that is better reduced when using the Emanuel convective scheme. Considering the good performance with respect to a quantitative evaluation of the temperature and precipitation simulations over the entire West African domain and its subregions, the Emanuel convective scheme is recommended for the study of the West African climate system.


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