Call for nominations for the Ostrowski Prize 2017


Call for nominations for the Ostrowski Prize 2017

The aim of the Ostrowski Foundation is to promote the mathematical sciences. Every second year it provides a prize for recent outstanding achievements in pure mathematics and in the foundations of numerical mathematics.

The prize has been awarded every two years since 1989. The most recent winners are Ben Green and Terence Tao in 2005; Oded Schramm in 2007; Sorin Popa in 2009; Ib Madsen, David Preiss, and Kannan Soundararajan in 2011; Yitang Zhang in 2013; and Peter Scholze in 2015.

The jury invites nominations for candidates for the 2017 Ostrowski Prize.  Nominations should include a CV of the candidate, a letter of nomination, and 2-3 letters of reference. Nominations should be sent to the Chair of the jury for 2017, Gil Kalai (Hebrew University of Jerusalem, Israel), by June 30, 2017.

(Because of some technical difficulties in advertising the deadline was extended from the original deadline of May 15, 2017.)

Links: Ostrowski Prize (Webpage) Ostrowski Prize (Wikipedea)

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1 Response to Call for nominations for the Ostrowski Prize 2017

  1. Matthew Cory says:

    One more point: Clay has everyone scrambling to find highly theoretical blowups in INCOMPRESSIBLE flow ( We have successfully complained before ( about the lack of attention paid to the quality problems posed by the mathematics community. Clay would be very hard-pressed to really defend its overly sheltered baby problems in light of unexplored areas that also meet up with practice. Their problems are poorly motivated as are the completely solved modeling problems in physics (common knowledge in the gauge community). For instance, we have major climate modeling issues with Navier-Stokes:

    “Climate model simulations are also sensitive to initial conditions (even in an average sense). Coupling a nonlinear, chaotic atmospheric model to a nonlinear, chaotic ocean model gives rise to something much more complex than the deterministic chaos of the weather model, particularly under conditions of transient forcing (such as the case for increasing concentrations of CO2). Coupled atmosphere/ocean modes of internal variability arise on timescales of weeks, years, decades, centuries and millenia. These coupled modes give rise to bifurcation, instability and chaos. How to characterize such phenomena arising from transient forcing of the coupled atmosphere/ocean system defies classification by current theories of nonlinear dynamical systems, particularly in situations involving transient changes of parameter values. Stainforth et al. (2007) refer to this situation as ‘pandemonium.'”

    It’s embarrassing me.

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