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9 Oct 2006: In the case n = 1 these are the usual polynomialsdefined in [24, Chapter III]. ... Following Tate’s formulaire [24, Chapter III] we put. (3). b2 = a21 4a2.

26 Apr 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does.

5 Jun 2006: 233.2.4 State-Based Speech Enhancement. 24. 3.3 Model-Based Techniques. 243.3.1 Linear Regression Adaptation. ... Ljm(τ ) = p(qjm(τ )|YT , M) (2.24)=. 1L(YT |M) Uj (τ )cjmbjm(y(τ ))βj (τ ). where. Uj (τ ) =. . a1j , if τ = 1N1i=2.

30 May 2006: 0 69.5 24.6 30.4 40.8 47.3 62-5 29.2 37.2 51.9 41.7 23.7 29.7 36.5 42.2. ... 29.6 36.6 25.0 34.8 54.0 24.8 33-8 28.2 35.3 24.3. 1 0 3 dp.

23 May 2006: 24. ). 1/2. Can also use for β 1 once βT 1. ... HKM shocks – p.24/25. Conclusions. Transients decay. γ2 α, γ 1: exponentially.

12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3]

22 May 2006: 1.4 Inverse of a matrix. 24. 1.4.1 Uniqueness of inverse. 24. ... . (. 1 4 2). =. . . 6 24 124 16 81 4 2.

5 May 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does.

27 Apr 2006: Received 24 November 2004; revised 19 May 2005; accepted 11 August 2005; published 2 February 2006. ... The wider range of melt rates were used toexamine model sensitivity to mi.[24] In an extensive study of four sea ice sites in the.

4 Sep 2006: 1990. 335.87. 80.22. 1990. 5.6. 4.6. 39.9. 24.9. 5.3. 1991. 335.20. ... 81.54. 1991. 5.4. 4.8. 41.7. 24.5. 5.2. 1992. 338.00. 78.85. 4.