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29 Jan 2019: On the infinite-dimensional QR algorithm. Matthew J. Colbrook† and Anders C. Hansen†. †DAMTP, Centre for Mathematical Sciences, University of Cambridge, Wilberforce Rd,Cambridge CB3 0WA, United Kingdom. Abstract. Spectral computations of

6 Oct 2016: Power and limitations of convex formulationsvia linear and semidefinite programming lifts. by. Hamza Fawzi. Submitted to the Department of Electrical Engineering and ComputerScience. in partial fulfillment of the requirements for the degree of.

19 Oct 2013: compared with typical inverse time scales for the flo". A succession of balance inversion op-. ... The study of Lorenz 0. Krishnamurthy (op. cit.) was not confined to the limited regime where all trajectories approaCl.

22 Aug 2012: STRATOSPHERE-TROPOSPHERE EXCHANGE. James R. Holton • Peter H. Haynes 2 and Michael E. Mcintyre 2 Anne R. Douglass 3 and Richard B. Rood 3 Leonhard Pfister 4. Abstract. In the past, studies of stratosphere-tropo- sphere exchange of mass and

12 Jan 2014: In particular, their Fourier transforms are taken as integrals over [0, 1], as op-posed to R.

14 Jun 2014: to an emptybuffer when the requested destination is a file that does not exist has been fixed, now therequest results in a no-op.

28 Oct 2010: REVIEW OF SCIENTIFIC INSTRUMENTS VOLUME 75, NUMBER 9 SEPTEMBER 2004. REVIEW ARTICLE. Optical trappingKeir C. Neuman and Steven M. Blocka). Department of Biological Sciences, and Department of Applied Physics, Stanford University,Stanford, California

27 Nov 2011: We also conclude that there is asizable increase in temperature as one moves along the op-tical axis away from the surface of the sapphire.

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

4 Oct 2010: Journal of Colloid and Interface Science 309 (2007) 194–224www.elsevier.com/locate/jcis. Feature article. International Union of Pure and Applied Chemistry, Physical and Biophysical Chemistry Division. IUPAC Technical Report. Measurement and

4 Oct 2010: In particular, the ion cloud, of typicalthickness k 2 1, surrounding the polyelectrolyte containsan excess of counterions, which are dragged in the op-posite direction and interact hydrodynamically with theprobe ion

7 Apr 2017: Aus d e m Z o o l o g i s c h e n I n s t i t u t d e r U n i v e r s i t s H a l l e a. S.). Z U R T H E O R I E D E R F L I M M E R B E W E G U N G. ( D Y N A M I K , N U T Z E F F E K T , E N E R G I E B I L A N Z ). V o n. W I L H E L M L U D W