Search Results - (Author, Cooperation:T. Strohmayer)
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1J. M. Miller ; J. S. Kaastra ; M. C. Miller ; M. T. Reynolds ; G. Brown ; S. B. Cenko ; J. J. Drake ; S. Gezari ; J. Guillochon ; K. Gultekin ; J. Irwin ; A. Levan ; D. Maitra ; W. P. Maksym ; R. Mushotzky ; P. O'Brien ; F. Paerels ; J. de Plaa ; E. Ramirez-Ruiz ; T. Strohmayer ; N. Tanvir
Nature Publishing Group (NPG)
Published 2015Staff ViewPublication Date: 2015-10-23Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsPublished by: -
2Dieters, S. ; Strohmayer, T. ; van Paradijs, J. ; Fishman, G. J. ; Meegan, C. A. ; Hurley, K. ; Kommers, J. ; Smith, I. ; Frail, D. ; Murakami, T. ; Kouveliotou, C.
[s.l.] : Macmillan Magazines Ltd.
Published 1998Staff ViewISSN: 1476-4687Source: Nature Archives 1869 - 2009Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsNotes: [Auszug] Soft γ-ray repeaters (SGRs) emit multiple, brief (∼0.1-s), intense outbursts of low-energy γ-rays. They are extremely rare—three are known in our Galaxy and one in the Large Magellanic Cloud. Two SGRs are associated with young supernova remnants (SNRs), and therefore most ...Type of Medium: Electronic ResourceURL: -
3Fenimore, E. E. ; Epstein, R. I. ; Ho, C. ; Klebesadel, R. W. ; Lacey, C. ; Laros, J. G. ; Meier, M. ; Strohmayer, T. ; Pendleton, G. ; Fishman, G. ; Kouveliotou, C. ; Meegan, C.
[s.l.] : Nature Publishing Group
Published 1993Staff ViewISSN: 1476-4687Source: Nature Archives 1869 - 2009Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsNotes: [Auszug] If y-ray bursters (GRBs) are at cosmological distances, the dearth of weak events results from the expansion of the universe, either because the signal is redshifted out of the bandpass of the instrument, and/or through evolution of the sources. The relative number of bursts at different ...Type of Medium: Electronic ResourceURL: -
4Staff View
ISSN: 1432-1181Source: Springer Online Journal Archives 1860-2000Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision MechanicsPhysicsDescription / Table of Contents: Zusammenfassung Überlagerte freie und aufgezwungene Konvektionsströmung in einem gekühlten vertikalen Kanal mit Eisschichtbildung an den Wänden ist numerisch untersucht worden. Grundlage der Eisschichtberechnung ist das einfache numerische Modell der Grenzschichtgleichungen. Für den Fall der dem Gravitationsvektor gleichgerichteten, gemischten Konvektion wird eine Verstärkung des Wärmeübergangs beobachtet, da die Strömungsgeschwindigkeit in der Nähe der Phasengrenze zunimmt. Aufgrund der Massenerhaltung kann es bei einer ausgeprägten Geschwindigkeitszunahme in der Nähe der Phasengrenze zu Rückströmungen in der Kanalmitte kommen. Die numerischen Ergebnisse zeigen gute Übereinstimmung mit Messungen von Campbell und Incropera [10]. Für den Fall der dem Gravitationsvektor entgegengerichteten Strömung kann es zur Strömungsablösung nahe der Phasengrenze kommen, die eine wellenartige Eisschicht bewirkt.Notes: Abstract The effect of mixed convection flow on the shape of the frozen crust in a cooled vertical channel was investigated numerically. For the prediction of the ice-layer thickness a simple numerical model which is based on the boundary layer equations was used. It can be seen that in case of assisting mixed convection flow the heat transfer at the solid crust increases because of inreasing velocity near the solid-liquid interface. On the other hand this increase of the velocity near the solid-liquid interface can lead to flow separation in the core region of the channel because of continuity of mass. By comparing the numerically obtained results for aiding mixed flow with measurements of Campbell and Incropera [10] good agreement can be observed. In case of opposing mixed flow it can be shown that flow separation might occur near the solid-liquid interface. This can result in a wave-like structure of the ice-layer.Type of Medium: Electronic ResourceURL: