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PUBLICATION LIST -- J
www.damtp.cam.ac.uk/user/tsm/jrw_publist1.pdf3 Jun 2024: Martin and M. J. Simons, pp. 235-250. Kluwer, Dordrecht (2002). 200. -
J. Fluid Mech. (2019), vol. 869, pp. 468–499. c© ...
www.damtp.cam.ac.uk/user/drh39/2019_JPlayers.pdf1 Dec 2023: and (e) t =200. ... t/Pe for the same parameters as (b) at t = 200. -
J. Fluid Mech. (2024), vol. 988, A10, doi:10.1017/jfm.2024.223 Flow…
www.damtp.cam.ac.uk/user/hinch/publications/JFM988_A10.pdf10 Jun 2024: J. Fluid Mech. (2024), vol. 988, A10, doi:10.1017/jfm.2024.223. Flow of an Oldroyd-B fluid in a slowly varyingcontraction: theoretical results for arbitraryvalues of Deborah number in the ultra-dilutelimit. Evgeniy Boyko1,†, John Hinch2 and Howard -
Tidal Grounding‐Line Migration Modulated by Subglacial Hydrology
www.damtp.cam.ac.uk/user/drh39/2020_grounding_line.pdf1 Dec 2023: Journal of Glaciology, 56(200), 1104–1114.Jenkins, A., Dutrieux, P., Jacobs, S. S., McPhail, S. -
Opto-fluidically multiplexed assembly and micro-robotics
www.damtp.cam.ac.uk/user/lauga/papers/223.pdf28 Feb 2024: 800. 600. 400. 200. 0. 20. t1 t2. Dis. tanc. eto. -
Flow-driven compaction of a fibrous porous medium
www.damtp.cam.ac.uk/user/drh39/2019_compact.pdf1 Dec 2023: 074306-17. DANIEL T. PATERSON et al. 0 100 200 300 400 500 600 700 800 900 1000Initial volume (mL). ... 0. 100. 200. 300. 400. 500. 600. 700. 800. 900. Fre. -
clas
www.damtp.cam.ac.uk/user/tong/dynamics/one.pdf13 Sep 2023: theory took over 200 years to discover; and it’s not at all clear what the relationship is. -
standardmodel
www.damtp.cam.ac.uk/user/tong/sm/standardmodel5.pdf31 May 2024: 5.73). – 200 –. We see that the three lines don’t meet. -
One-dimensional compression of a saturated elastoviscoplastic medium
www.damtp.cam.ac.uk/user/drh39/2022_elastoviscoplastic_compression.pdf1 Dec 2023: 50. 100. 150. 200. 250. 18 190. 100. 200. 0.6 0.620. -
J. Fluid Mech. (2018), vol. 837, pp. 520–545. c© ...
www.damtp.cam.ac.uk/user/drh39/2018_JPfinger.pdf1 Dec 2023: b,c) Marginal stability curves (σ =0, outlines)and regions of instability (σ > 0, shaded areas), for R = 3 and (b) Pe = 25, 200, 500 and(c) Pe=15, 20, 25.
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