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991.
吉林中部呼兰群泥质岩递进变质带特征及其地质意义 总被引:3,自引:0,他引:3
下古生界呼兰群变质岩系位於吉林褶皱带南端,其中泥质岩变质片岩段具有明显的递进变质作用,并可划分为:铁铝石榴石带、十字石带、蓝晶石带、硅线石带四个矿物带,呈中压中温巴洛式变质带特征。本文对该变质带矿物组合、原岩建造、变质作用演化、成因机理及其地质意义进行了探讨。 相似文献
992.
993.
An algorithm for the solution of a nonlinear problem of phase boundary movement and evolution of temperature distribution
due to the perturbation in the basal heat flux has been discussed. The reduction of the problem to a system of nonlinear ordinary
differential equations with the help of a Fourier series method leads to a stiff system. This stiffness is taken care of by
the use of a modified Euler’s method. Various cases of basal heat flow variation have been considered to show the performance
and stability of the technique for such a nonlinear system. The first case of step-wise function is taken to analyse the performance
of the technique, and the study has been extended to other general cases of linear increase, periodic variation, and box and
triangular function type variations in the heat flux. In the step-wise case the phase boundary attains a constant position
rapidly if the supplied heat flux is sufficiently large. The effect of periodicity in the heat flow is clearly depicted in
the phase boundary movement, where the phase boundary oscillates about the mean position at large times. The absence of any
constant level in the case of linear increase in heat flux is due to a very large value of heat flux. In the cases of box
car and triangular heat flux the boundary starts moving downward after the cessation of excess heat flux but does not immediately
return to its original preperturbation state, instead approaches it at large times. This technique may be applied to more
general cases of heat flow variation. 相似文献
994.
G. W. Harris D. Klemp T. Zenker J. P. Burrows B. Mathieu 《Journal of Atmospheric Chemistry》1992,15(3-4):315-326
Measurements of NO2, HCHO, and H2O2 were made by the highly specific method of mid infra-red absorption spectroscopy using tunable diode lasers (TDLAS) during the 1988 Polarstern expedition. The TDLAS data are compared to those obtained during the cruise using less direct methods. Southern Hemisphere NO2 levels suggest nett photochemical destruction of O3 in the boundary layer. Northern Hemisphere HCHO averaged 0.47±0.2 ppbv; the HCHO measurements are used in a simple calculation to estimate OH noontime maxima of 3–6×106 cm-3. 相似文献
995.
996.
伍荣生 《Acta Meteorologica Sinica》1991,(1)
It is convenient to use σ-coordinates to discuss the dynamic effect of orography and the flow inEkman boundary layer.In this paper,the theory of mixing length is generalized to the σ-coordinate system.Then the governing equations,describing the motion in the boundary layer over the mountain regions arederived.The features of flow in the boundary layer,especially the effects of Ekman pumping,are discussed indetails.It is pointed out that there are three factors affecting the vertical motion at the top of the boun-dary layer:(1)vorticity distribution in the boundary layer,which is directly related to the divergence andconvergence of air flow caused by friction,(2)the upslope or downslope motion of flow over the mountainslopes,and(3)the mutual effect of orography and friction induced by the ageostrophic component climbing up-ward or downward in the boundary layer over mountain regions. 相似文献
997.
S. B. S. S. Sarma 《Journal of Earth System Science》1991,100(2):145-154
We discuss high resolution measurements on radio refractive index, in the boundary layer and above the atmosphere in the Indian
sub-continent spread over a period of more than a solar cycle by making use of airborne microwave refractometers, operating
around 9 GHz. Some atmospheric turbulence parameters comparable with earlier results have also been derived. The results demonstrate
sharp gradients of radio refractive index, layer structures and the variability of the boundary layer in time and space.
An erratum to this article is available at . 相似文献
998.
Recent investigations of magnetospheric plasma structure are summarized under the broad categories of empirical models, transport across boundaries, formation, and dynamics of the plasma sheet. This report reviews work in these areas during the period 1991 to 1993. Fully three-dimensional empirical models and simulations have become important contributors to our understanding of the magnetospheric system. Some new structural concepts have appeared in the literature: the entry boundary and geopause, the plasma sheet region 1 vortices, the low-energy layer, the adiabaticity boundary or wall region, and a region in the tail to which we refer as the injection port. Traditional structural concepts have also been the subject of recent study, notably the plasmapause, the magnetopause, and the plasma sheet. Significant progress has been made in understanding the nature of plasma sheet formation and dynamics, but the acceleration of electrons to high energy remains somewhat mysterious. 相似文献
999.
BOUNDARY LAYER GROWTH AND LAPSE RATE CHANGES DETERMINED BY LIDAR AND SURFACE HEAT FLUX IN SOFIA*
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In this study the results from a boundary layer experiment,conducted in autumn 1991 over a flat,build-up urban area in Southeast Sofia,together with some models for mixed layer growth rates are used to investigate the layered structure of the vertical atmospheric stability distribution in the Sofia Valley.Lidar measurements of aerosol layer heights and morning boundary layer development are combined with surface eddy correlation measurements of kinematic heat and moisture fluxes,profiles of temperature and humidity,wind speed and wind direction.A diagnostic method is presented for determining vertical lapse rates using surface meteorological measurements and lidar returns observed during the transition from nighttime stable stratification to daytime convective boundary layer after the sunrise. 相似文献
1000.
Modelling the arctic convective boundary-layer with different turbulence parameterizations 总被引:1,自引:1,他引:0
Different parameterizations of subgrid-scale fluxes are utilized in a nonhydrostatic and anelastic mesoscale model to study their influence on simulated Arctic cold air outbreaks. A local closure, a profile closure and two nonlocal closure schemes are applied, including an improved scheme, which is based on other nonlocal closures. It accounts for continuous subgrid-scale fluxes at the top of the surface layer and a continuous Prandtl number with respect to stratification. In the limit of neutral stratification the improved scheme gives eddy diffusivities similar to other parameterizations, whereas for strong unstable stratifications they become much larger and thus turbulent transports are more efficient. It is shown by comparison of model results with observations that the application of simple nonlocal closure schemes results in a more realistic simulation of a convective boundary layer than that of a local or a profile closure scheme. Improvements are due to the nonlocal formulation of the eddy diffusivities and to the inclusion of heat transport, which is independent of local gradients (countergradient transport). 相似文献