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31.
Birch (Betula tortuosa) is one of the tree-line forming species within the Siberian Mountains.We analysed the area dynamics of birch stands and the upslope clim... 相似文献
32.
M. S. Zhdanov N. G. Golubev V. V. Spichak Iv. M. Vaientsov 《Geophysical Journal International》1982,68(3):589-607
Summary. This paper deals with the further development of finite-difference methods for electromagnetic field modelling in two-and three-dimensional cases. The main feature of the approach suggested here is the application of generalized asymptotic boundary conditions valid with the accuracy (1/ρN ), where ρ is the distance from the heterogeneities. The finite-difference approximation of problems under solution is made using the balance method, which results in 5-point difference schemes in the 2-D case and 7-point difference schemes in the 3-D case. To solve the linear system of difference equations the successive over-relaxation (SOR) method is used, the relaxation factor being chosen during the iteration procedure. In view of the vectorial character of the problem for the 3-D case, a successive blocked over-relaxation method (SBOR) is applied.
The model's validity is based on the comparison of the fields accounted at the ground surface with those computed by the integral transformation of excessive currents, determined in the heterogeneity region using the finite-difference scheme. 相似文献
The model's validity is based on the comparison of the fields accounted at the ground surface with those computed by the integral transformation of excessive currents, determined in the heterogeneity region using the finite-difference scheme. 相似文献
33.
Sassa Shinji Grilli Stephan T. Tappin David R. Sassa Kyoji Karnawati Dwikorita Gusiakov Viacheslav K. Lvholt Finn 《Landslides》2022,19(2):533-535
Landslides - A World Tsunami Awareness Day Special Event was held in hybrid mode on 5 November 2021, during the Fifth World Landslide Forum, in Kyoto, Japan. In this context, a panel discussion was... 相似文献
34.
Viacheslav G. Makarov Oleg V. Zaytsev Valentina D. Budaeva Felipe Salinas-Gonzalez 《Journal of Oceanography》2008,64(5):675-690
A unified method of approximation, extrapolation, and objective layering is offered for processing vertical oceanographic
profiles. The method is demonstrated using seawater density and consists of adjustable splitting of each individual profile
into N vertical layers based on tentative, piecewise linear homogeneous approximation with specified accuracy and a final fitting
of an N-layered analytical model to data. A set of 3N coefficients of the model includes one density value at the sea surface; N−1 depths of layer interfaces; and N pairs of coefficients that describe a profile shape within the n-th layer—an asymptotic density value (a key parameter for extrapolation) and a vertical scale of maximum density variability
(related to vertical gradient). Several distinctive characteristics of the technique are: (1) It can be used for the analysis
of the vertical structure of individual profiles when N is an unknown parameter, and spatial interpolation when N should be equal for all profiles. (2) A justified downward extrapolation of incomplete data is possible with the model, especially
if historical deepwater profiles are available. (3) Layer interfaces, as well as other coefficients, are derived with only
one fitting to the entire profile. (4) The technique, using its general formulation, can serve as a parent for developing
various types of models. The simpler step-like (with hyperbolic or exponential approximation) and more complicated smooth
(continuous in gradient space) models were designed and tested against a large number of density profiles from the Sea of
Okhotsk and the Gulf of California. Comparison of parametric, z-levels and isopycnal averaging was done for the region off the northeastern coast of Sakhalin. 相似文献
35.
Viacheslav I. Kharuk Sergei T. Im Maria L. Dvinskaya Kenneth J. Ranson Il’ya A. Petrov 《山地科学学报》2017,14(3):442-452
The phenomenon of tree waves(hedges and ribbons) formation within the alpine ecotone in Altai Mountains and its response to observed air temperature increase was considered. At the upper limit of tree growth Siberian pine(Pinus sibirica) forms hedges on windward slopes and ribbons on the leeward ones. Hedges were formed by prevailing winds and oriented along winds direction. Ribbons were formed by snow blowing and accumulating on the leeward slope and perpendicular to the prevailing winds, as well as to the elevation gradient. Hedges were always linked with microtopography features, whereas ribbons were not. Trees are migrating upward by waves and new ribbons and hedges are forming at or near tree line, whereas at lower elevations ribbons and hedges are being transformed into closed forests. Time series of high-resolution satellite scenes(from 1968 to 2010) indicated an upslope shift in the position ribbons averaged 155±26 m(or 3.7 m yr~(-1)) and crown closure increased(about 35%–90%). The hedges advance was limited by poor regeneration establishment and was negligible. Regeneration within the ribbon zone was approximately 2.5 times(5060 vs 2120 ha~(-1)) higherthen within the hedges zone. During the last four decades, Siberian pine in both hedges and ribbons strongly increased its growth increment, and recent tree growth rate for 50 year-old trees was about twice higher than those recorded for similarly-aged trees at the beginning of the 20~(th) century. Hedges and ribbons are phenomena that are widespread within the southern and northern Siberian Mountains. 相似文献
36.
The neural network estimates of seismic P- and S-wave velocities from electrical resistivity of the rocks and, vice versa, resistivity estimates from seismic velocities are presented. It is shown that, depending on the ratio between the volumes of the known data and the data to be reconstructed, the accuracy of the estimates of the P- and S-wave velocities ranges within 1–4 and 4–6%, respectively. The logarithmic resistivity is estimated from seismic P- and S-velocities as accurately as up to 15–17%. In all cases, the biggest errors are obtained when the estimates are based on correlated data. 相似文献
37.
The applicability of the Bayesian inversion of audiomagnetotelluric data to the electromagnetic mapping of groundwater reservoirs is examined. A model example is used to demonstrate that both the reservoirs and their salinity zones can be mapped using measurements of magnetotelluric fields in the audio frequency range. 相似文献
38.
Alexander Yakirevich Avraham Dody Eilon M. Adar Viacheslav Borisov Mebus Geyh 《Hydrogeology Journal》1998,6(1):50-65
Temporal distributions of the isotopic composition in arid rain storms and in the associated runoff were investigated in
a small arid rocky basin in Israel. Customized rain and runoff samplers provided sequential water samples hermetically sealed
in high-density PVC bags. In several storms where the runoff was isotopically depleted, compared with the rainfall, the difference
could not be explained by fractionation effects occurring during overland flow. A water-balance study relating the runoff
discharge to rainfall over a rocky watershed showed that the entire discharge is produced by a very small segment (1–2 mm)
of the rain storm. The major objective, therefore, was to provide quantitative relations between segments of rainfall (rain
showers and rain spells) and runoff. The time distribution of the composition of stable isotopes (oxygen and hydrogen) was
used to quantify the correlation between the rain spell's amount and the consequent runoff. The aim of this work was to (a)
utilize the dynamic variations in the isotopic composition in rainfall and runoff and model the magnitude of surface-storage
capacity associated with runoff processes of overland flow, and (b) characterize the isotopic composition of the percolating
water with respect to the isotopic distribution in rainfall and runoff events. The conceptual model postulates an isotopic
mixing of overland flow with water within the depression storage. A transport model was then formulated in order to estimate
the physical watershed parameters that control the development of overland flow from a certain rainfall period. Part I (this
paper) presents the results and the assessment of the relative depression storage obtained from oxygen-18 and deuterium analyses
that lead to the physical and mathematical formulation of a double-component model of kinematic-wave flow and transport, which
is presented in Part II (accompanying paper).
Received, February 1997 · Revised, September 1997 · Accepted, September 1997 相似文献
39.
V. V. Spichak 《Izvestiya Physics of the Solid Earth》2006,42(1):60-68
Various hypotheses of the geoelectric structure of the Transcaucasian region reflecting a priori geological and geophysical information and data from profile magnetotelluric (MT) soundings are analyzed. These hypotheses are used to construct simplified 3-D models of electrical conductivity differing in the patterns of the shallow and deep structure of the region. Numerical modeling of MT fields is performed. Comparative analysis of its results indicates that the most probable conductivity model consistent with the available data is a model involving a high-conductivity channel connecting the Black and Caspian seas. 相似文献