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211.
The specific features of formulation and implementation of balance-hydrodynamic simulation during different-scale studies of natural resources of groundwater. Are an example of detailed estimate of the resources and balance of groundwater in the Vologda River basin is given. It is noted that the use of balance-hydrodynamic models, in addition to an increase in the general reliability of estimates, allows the calculation of normal annual characteristics of groundwater resources with different occurrence (exceedance probability), which is impracticable when hydrodynamic methods in other formulations are used. 相似文献
212.
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214.
Characterization of potential zones of dust generation at eleven stations in the southern Sahara 总被引:2,自引:0,他引:2
Summary Synoptic wind data for multi-decadal periods at eleven stations located in the southern Sahara region (Agadez, Atar, Bilma, Dori, Gao, Kayes, Nema, Niamey, Nouadhibou, Ouagadougou and Tessalit) are used to study the monthly dust deflation power over the region. We found that, regardless of the conditions of the soil, the deflation power (or wind efficiency) is not sufficient to generate significant amounts of aerosols south of 15°N. North of this latitude, the deflation power is much larger, with potential zones of either very strong deflation (Nouadhibou and Bilma) or severe deflation (Gao, Tessalit, Nema, Atar, Agadez). Stations in the Sahel region such as Gao, Agadez and Tessalit are characterized by a gradual reinforcement of the deflation power between 1970 and 1984 in correspondence of increasing desertification over the region. During this same period, Bilma, a well know region of dust source, experienced a major reduction in deflation power due to shifts in large scale wind patterns. 相似文献
215.
216.
Recently new calculations for the probability field distribution in plasma generating a new expression for the Debye screening fields was carried out by Martin and Perez (1996). This field is a very accurate solution of the Poisson equation for a point test charge in a plasma described by a uniform charge density at Boltzmann thermal equilibrium. The method that we here present is based mainly on the introduction of this adequate field considering the dependence of the potential with the magnitude of the test charge in the calculus of the distribution. First we find the spectral function F(k) carrying out the Fourier transform of the field which is numerically calculated for each representative value of the variable in k space and then fitting these data in order to get F(k). Thus, after the usual numerical integration on the wave number space d3k, the field strength distribution is achieved. This approximation recovers the Holtsmark distribution in the limit of high temperature, and/or, small densities as also these where 0. As in previous works (Ecker, 1972; Spatschek, 1990) the most probable value of the field decreases as the temperature is reduced, and/or, the density increased. 相似文献
217.
Non-linear - dynamo waves existing in an incompressible medium with the turbulence dissipative coefficients depending on temperature are studied in this paper. We investigate of - solar non-linear dynamo waves when only the first harmonics of magnetic induction components are included. If we ignore the second harmonics in the non-linear equation, the turbulent magnetic diffusion coefficient increases together with the temperature, the coefficient of turbulent viscosity decreases, and for an interval of time the value of dynamo number is greater than 1. In these conditions a stationary solution of the non-linear equation for the dynamo waves amplitude exists; meaning that the magnetic field is sufficiently excited. The amplitude of the dynamo waves oscillates and becomes stationary. Using these results we can explain the existence of Maunders minimum. 相似文献
218.
Radial abundance gradients of the element ratios O/H, Ne/H, S/H, and Ar/H are determined for a sample of disk planetary nebulae,
emphasizing the behaviour of the gradients at large galactocentric distances.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
219.
J. Egger 《Climate Dynamics》1999,15(7):561-568
Principal oscillation pattern (POP) analysis fits a first order multivariate autoregressive model to a reduced subset of
the variables of a complex system. It has been shown in the past that important modes of complex systems can be detected through
the POP technique. In this note two problems with this method will be addressed. Firstly, the POP analysis may face difficulties
if the reduced system is of higher order in time than first. An example from linear equatorial wave dynamics is given to illustrate
this point. Autoregressive models of higher order (MOP-models) are shown to provide a partial solution in such situations
but are not fully satisfactory either. Nonlinearity may cause problems as well. A nonlinear low-order model is used to discuss
this point. Both the POP and the MOP scheme are applied without data reduction. The MOP approach is superior to the POP technique
in that it detects oscillating patterns which elude the POP analysis. The results suggest that the MOP analysis may be a valuable
extension of the POP approach.
Received: 29 July 1998 / Accepted: 10 February 1999 相似文献
220.