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1 Sep 2011: TO KA-SAETSQ PORQDKA POLIGARMONINOSTI (g) = @(f)=@xj, TO, POSKOLXKU OPERACIQ DIFFERENCIRO-WANIQ SOHRANQET TOT PORQDOK, IMEEMr2(g) = 0; = m1 1 2m1 = m:pREDLOVENIE 1a0, A S NIM I SLUAJ 1a)

29 Nov 2011: Master of Arts. Elson, Harriet Lucy Grace. Leung, Ka On Charlotte.

29 Nov 2011: Hayton, David Michael. Hui, Eugenie Ka. Tang, Tjun Yip. in absence.

31 Oct 2011: 10-100 ka climatic shifts throughout the Earth's history would have caused the. ... Their. formation ranges between 120 and 18 Ka. They consequently span between OIS 5c-d.

29 Nov 2011: Chung, Ka Kin Kenny. Cica, Natasha. Savell, Kristin Louise. Tang, Kit Shing.

29 Nov 2011: Bachelor of Arts. Ng, Ka-Lun. in absence. Master of Arts. Adam, Alastair David Gordon.

5 Aug 2011: Although the strong correlationsuggests an almost constant and linear relationship, it actually appears as ifthe earliest part of the record (before about 650 ka) had lower mixing ratios(both absolutely and ... a) The last interglacial and methane. The

31 Oct 2011: INQUA SEQS. International Union for Quaternary Research (INQUA)Section on European Quaternary Stratigraphy (SEQS). Southern Scientific Centre, Russian Academy of SciencesGeological Institute, Russian Academy of Sciences. Quaternary stratigraphy and

1 Sep 2011: On Lp-boundedness of the L2-projectoronto nite element spacesA. Yu. Shadrin1. IntroductionIn [Sh] we proved that, for p suciently close to 2, the Lp-norm of the L2-projector P onto the space S of polynomial splines of order k on a knot-sequence is

16 Dec 2011: Old Testament Studies: Graham Ivor Davies, F. Oncology, Li Ka Shing: Bruce Anthony John Ponder, JE.