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1 Sep 2011: For g! = R M! this provides100) g! 2 Wk1[0;1]200) g! = (

3 Dec 2011: Generalized Sampling: Extension to Frames and Inverse andIll-Posed Problems. Ben Adcock Anders C. Hansen † Evelyn Herrholz ‡ Gerd Teschke‡. Abstract. Generalized sampling is new framework for sampling and reconstruction in

22 Nov 2011: 20 trials) (middle)and f fN1,N2,m2,t (avg. 20 trials) (bottom), where N = N2 = 1001,m = 370, N1 = 170, m2 = 200.

2 Nov 2011: Generalized sampling and infinite-dimensionalcompressed sensing. Ben AdcockDepartment of Mathematics. Simon Fraser UniversityBurnaby, BC V5A 1S6. Canada. Anders C. HansenDAMTP, Centre for Mathematical Sciences. University of CambridgeWilberforce Rd,

13 Apr 2011: 9. been sent by e-mail to about 200 people. The objective function is specified bya subroutine, provided by the user, that calculates F(x) for any x in Rn thatsatisfies ... 103.92 32.86 / 32.21160 34.62499 / 26.13208 436.25 / 352.69 200.73 / 173.07.

5 Aug 2011: 2140 E. W. Wolff. –440. –410. –380. 0 200 400 600 800age (EDC3 kyr BP). ... 200 ppbv) than in interglacials (up to 280 ppbv) [53], although therecord is patchy because artefacts do occur that make the records in some sectionsof ice unreliable.

14 Jul 2011: Fundamentals of Atmosphere–OceanDynamics. M. E. McIntyre. LATEX version edited by. Björn Haßler. and. Christophe Koudella. with the kind assistance of. Teresa Cronin. and. Sarah Shea–Simonds. Version of 2007–8. ii Part , 0.0. Author’s

1 Sep 2011: Woo J. Fluid Mech. vol. 86, 1978, pp. 179-200. We regret overlooking the fact that the first use of the result (2.12) for the numbers of surface saddle and

19 Aug 2011: 1 10-6. 1.5 10-6. 2 10-6. 0 200 400 600 800 1000 1200. ... 1.5 10-6. 2 10-6. 0 200 400 600 800 1000 1200.

10 Apr 2011: Scales are 200 m. (d) Alinear Volvox cluster viewed from above (scale is 1 mm).