885 research outputs found
Computing Hilbert Class Polynomials
We present and analyze two algorithms for computing the Hilbert class
polynomial . The first is a p-adic lifting algorithm for inert primes p
in the order of discriminant D < 0. The second is an improved Chinese remainder
algorithm which uses the class group action on CM-curves over finite fields.
Our run time analysis gives tighter bounds for the complexity of all known
algorithms for computing , and we show that all methods have comparable
run times
Oscillatory subglacial drainage in the absence of surface melt
The presence of strong diurnal cycling in basal water pressure records
obtained during the melt season is well established for many glaciers. The
behaviour of the drainage system outside the melt season is less well
understood. Here we present borehole observations from a surge-type valley
glacier in the St Elias Mountains, Yukon Territory, Canada. Our data indicate
the onset of strongly correlated multi-day oscillations in water pressure in
multiple boreholes straddling a main drainage axis, starting several weeks
after the disappearance of a dominant diurnal mode in August 2011 and
persisting until at least January 2012, when multiple data loggers suffered
power failure. Jökulhlaups provide a template for understanding spontaneous
water pressure oscillations not driven by external supply variability. Using
a subglacial drainage model, we show that water pressure oscillations can
also be driven on a much smaller scale by the interaction between conduit
growth and distributed water storage in smaller water pockets, basal
crevasses and moulins, and that oscillations can be triggered when water
supply drops below a critical value. We suggest this in combination with a
steady background supply of water from ground water or englacial drainage as a
possible explanation for the observed wintertime pressure oscillations
Some genus 3 curves with many points
Using an explicit family of plane quartic curves, we prove the existence of a
genus 3 curve over any finite field of characteristic 3 whose number of
rational points stays within a fixed distance from the Hasse-Weil-Serre upper
bound. We also provide an intrinsic characterization of so-called Legendre
elliptic curves
Reducing the linewidth of a diode laser below 30 Hz by stabilization to a reference cavity with finesse above 10^5
An extended cavity diode laser operating in the Littrow configuration
emitting near 657 nm is stabilized via its injection current to a reference
cavity with a finesse of more than 10^5 and a corresponding resonance linewidth
of 14 kHz. The laser linewidth is reduced from a few MHz to a value below 30
Hz. The compact and robust setup appears ideal for a portable optical frequency
standard using the Calcium intercombination line.Comment: 8 pages, 4 figures on 3 additional pages, corrected version,
submitted to Optics Letter
Development of daily precipitation projections for the United States based on probabilistic downscaling
West Antarctic ice sheet and CO2 greenhouse effect: a threat of disaster
DIB's contribution to this work is from the DOMINOS project, a component of the International Thwaites Glacier Collaboration (ITGC). Support for DIB was provided by the Natural Environment Research Council (NERC: Grant NE/S006605/1). ITGC Contribution No. ITGC:025.Over 40 years ago, the glaciologist John Mercer warned that parts of the West Antarctic Ice Sheet were at risk of collapse due to the CO2 greenhouse effect. Mercer recognised the unique vulnerability of ice sheets resting on beds far below sea level (marine-based ice sheets), where an initial warming signal can initiate irreversible retreat. In this paper, we review recent work on evidence for ice sheet collapse in warmer periods of the recent geological past, the current behaviour of the ice sheet, and computer models used to predict future ice-sheet response to global warming. Much of this work points in the same direction: warming climates can indeed trigger collapse of marine-based portions of the West Antarctic Ice Sheet, and retreat in response to recent warming has brought parts of the ice sheet to the threshold of instability. Further retreat appears to be inevitable, but the rate of collapse depends critically on future emissions.Publisher PDFPeer reviewe
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