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91.
In this paper, we have investigated some tilted Bianchi Type I models with heat conduction filled with disordered radiation
of perfect fluid. To get a determinate solution, we have assumed a condition A =(BC)
n between metric potentials. Alternatively we have discussed the case A=(BC)
1/3 for which tilted nature of the model is preserved. The various and geometrical features with singularities in the models
are also discussed.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
92.
G. Handler T. Arentoft R. R. Shobbrook M. A. Wood L. A. Crause P. Crake F. Podmore A. Habanyama T. Oswalt P. V. Birch G. Lowe C. Sterken P. Meintjes J. Brink C. F. Claver R. Medupe J. A. Guzik T. E. Beach P. Martinez E. M. Leibowitz P. A. Ibbetson T. Smith B. N. Ashoka N. E. Raj D. W. Kurtz L. A. Balona D. O'donoghue J. E. S. Costa § M. Breger 《Monthly notices of the Royal Astronomical Society》2000,318(2):511-525
93.
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96.
Nand Lal Sharma Jagdish Chand Kuniyal Mahavir Singh Manum Sharma Raj Pal Guleria 《Acta Geophysica》2011,59(2):334-360
The measurements using a ground based multi wavelength radiometer (MWR) at Mohal (31°54′N, 77°07′E, 1154 m AMSL) in the Kullu
valley of Northwestern Himalayan region show that the spectral aerosol optical depth (AOD) and turbidity coefficient, β, are high in summer, moderate in monsoon season, low in winter and lowest in autumn, while wavelength exponent, α, has an opposite trend. Average annual value of AOD at 500 nm is 0.24±0.01, 0.43±0.02, and 0.28±0.02; that of β is 0.14±0.01, 0.22±0.02, and 0.17±0.03; and that of α is 1.06±0.09, 1.16±0.10, and 0.86±0.13, respectively, for clear, hazy and partially clear sky days. The considerably greater
value of β on hazy days indicates more coarse particles in mountain haze. The fractional asymmetry factor (AF) is more negative in summer
and autumn months. The AOD and β have significantly positive correlation with temperature and wind speed, suggesting high AODs and turbidity on hot and windy
days. 相似文献
97.
Flow records, rising‐stage sediment samplers, and a sand suspension model are used to examine suspended sediment concentrations during major floods caused by tropical cyclones TC Joni and TC Kina in the Rewa River, Fiji. The highest concentrations of total suspended solids were measured during the early stages of TC Kina. The suspension model predicts higher sand concentrations for TC Kina compared with TC Joni because of the larger slope and higher shear stresses during Kina. Extremely high wash load concentrations early in TC Kina are at least partly due to remobilization of fine sediment deposited during the earlier TC Joni flood. Samples from the TC Kina had volumetric concentrations larger than 5%, indicating hyperconcentrated streamflows. Mass‐density shear stresses in the hyperconcentrated flows are up 1·6 times larger than clear‐water shear stresses, but they occur early during low stages of the flood and probably do not result in severe bed erosion. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
98.
We study the static stiff-fluid model for perfect fluid distributions in the presence of incident magnetic field. The magnetic field is surrounded by static stiff fluid of infinite electric conductivity and it is due to the electric current flowing along theZ-axis. The various physical and geometrical properties together with the state of model in absence of magnetic field are also discussed. 相似文献
99.
An LRS Bianchi type I string dust cosmological model with and without bulk viscosity following a method used by Letelier and
Stachel, is investigated. To get a determine solution, it is assumed that σ∝θ whereσ is shear and θ is scalar of expansion
and which leads to A =αBn were n is a constant. The physical and geometrical aspects of the model are also discussed.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
100.