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Dunning AM, Michailidou K, Kuchenbaecker KB, Thompson D, French JD, Beesley J, Healey CS, Kar S, Pooley KA, (…), García-Closas M, Vachon C, Chenevix-Trench G, Antoniou AC, Easton DF, Edwards ... Pooley KA, McGuffog L, Barrowdale D, Frost D, Ellis SD,

M Delarue, R Delorme, S Desrivieres, G Devenyi, MA Di Biase, R Dolan, KA Donald, G Donohoe, K Dunlop, AD Edwards, JT Elison, CT Ellis, JA Elman, L Eyler, DA Fair, ... Journal: Sci Rep. E-pub date: 24 Sep 2019. Authors: R Bruffaerts, LK Tyler, M Shafto,

478-424 ka), whilst glaciation during the subsequent Devensian Stage (MIS 2; c. ... 29-18 ka) resulted in blockage of The Wash, causing further river diversions.

Kyiv's Monastery of the Caves (Pechers'ka Lavra) and Saint Sophia.

Journal: Brain. E-pub date: 1 Aug 2023. Authors: M Malpetti, TE Cope, D Street, PS Jones, FH Hezemans, E Mak, KA Tsvetanov, T Rittman, WR Bevan-Jones, K Patterson, L ... Journal: J Nucl Med. E-pub date: 1 Jul 2022. Authors: M Malpetti, SS Kaalund, KA

In the Chew Bahir cores we are focussing on creating a high-resolution age model for the 135 ka – 125 ka interval, around the transition from MIS 6 to MIS 5, ... which will allow a test of the hypothesis that human population increase and range

Poster presentation (presented by Christine Lane). Topic: A 260 ka eruptive history for Kilimanjaro derived from Lake Challa sediments.

Turbulent flow over unsteady monochromatic and Stokes waves has been investigated for various wave steepness ka and wave age cr/U using a Differntial Second-Moment (DSM) closure turbulence model.

The nominal turbulent Reynolds number, Ret=34 and Karlovitz number, Ka=25, places the flame in the thin reaction zones regime of turbulent premixed combustion.

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