001482743 000__ 06072cam\\22005177i\4500 001482743 001__ 1482743 001482743 003__ OCoLC 001482743 005__ 20231128003349.0 001482743 006__ m\\\\\o\\d\\\\\\\\ 001482743 007__ cr\cn\nnnunnun 001482743 008__ 231031s2023\\\\si\a\\\\o\\\\\000\0\eng\d 001482743 019__ $$a1406831522 001482743 020__ $$a9789819965755$$q(electronic bk.) 001482743 020__ $$a9819965756$$q(electronic bk.) 001482743 020__ $$z9789819965748 001482743 020__ $$z9819965748 001482743 0247_ $$a10.1007/978-981-99-6575-5$$2doi 001482743 035__ $$aSP(OCoLC)1406982823 001482743 040__ $$aGW5XE$$beng$$erda$$epn$$cGW5XE$$dYDX$$dEBLCP 001482743 049__ $$aISEA 001482743 050_4 $$aQE501$$b.P76 2023 001482743 08204 $$a551.1$$223/eng/20231031 001482743 24500 $$aProcesses in GeoMedia.$$nVolume VII /$$cTatiana Chaplina, editor. 001482743 264_1 $$aSingapore :$$bSpringer,$$c2023. 001482743 300__ $$a1 online resource (vii, 309 pages) :$$billustrations (some color). 001482743 336__ $$atext$$btxt$$2rdacontent 001482743 337__ $$acomputer$$bc$$2rdamedia 001482743 338__ $$aonline resource$$bcr$$2rdacarrier 001482743 4901_ $$aSpringer geology,$$x2197-9553 001482743 5050_ $$aAcoustic wave reflection coefficient from large-scale irregularities weakly non-Gaussian sea surface -- Numerical modeling of wind currents in the Sivash Gulf (Sea of Azov) -- Metamorphic Conditions Carbonaceous Rocks Framing of the Larino Granite-Gneiss Dome (South Ural, Russia) -- Chemical and microbiological features of the coastal waters of the Black and Azov Seas in summer season -- On the issue of "true polar wander" phenomenon and its alternative physical interpretation based on galactic model -- The Black Sea deep-water circulation under climatic and anomalous atmospheric forcing -- Determination of the initial Cs140 concentration field in the Black Sea after the Chernobyl accident -- Analytical solution of the evolutionary model of wind currents -- Assessment of the wave asymmetry contribution to the dynamics of sediment fractions in the coastal zone of the Kalamitsky Gulf -- Changes in the repeatability of dangerous winds in the arctic zone of Siberia for the summer months in the period 1961-2020 -- Repeatability of dangerous winds over the sea of Azov and Black sea and their coasts -- Investigation of the spatio-temporal heterogeneity of the snow thickness at the site of the Lomonosov MSU in winter of 2022/2023 -- Experimental estimates of the rate of deepening of individual thermals -- Interaction of nonlinear waves taking into account planetary scale blems -- Hydrodynamic interaction between two systems of intense intra-mantle vortices as a possible cause of the connection between distant earthquakes -- Wave motions of a liquid in a rotating annular layer -- The problem of propagation of plane long waves in a nonhomogeneous liquid over a deformable bottom -- Technogenic gold-bearing mineralization of eastern orenburg region -- Morpholitosystem of Piltun lagoon (Sakhalin region) -- Propagation of tsunami waves in the Forked Bays -- Assessment of the state of the hydrosphere in the zone of development of oil fields of the Western Orenburg region -- Biogenic morpholitogenesis on sea coasts Sakhalin island -- Organogenic morpholitosystem of the Nabil lagoon -- Concept of a structural system of a large-panel residential building with a free layout considering the requirements for earthquake resistance during construction in a sharply continental climate -- Geophysical investigation of the ski slope snow thickness at "Vorob'yovy Gory" hills in winter period 2022/23 -- Statement of individual problems of the dynamics of stratified media with allowance for compressibility -- Formation of modern technogenic processes in historical urban areas -- Carbon sequestration in managed salt wetlands (Carbon polygon) -- Methodology for determining the content of BTEX and oils in water with various external parameters -- Abrasion-denudation cycle levels as the basis of paleoreconstructions on rising coasts -- Exact Analytical Expression for Maximum Heat Flux from Impulsive Sources of Charged Particles in Magnetic Field. 001482743 506__ $$aAccess limited to authorized users. 001482743 520__ $$aThis book includes new results of theoretical and experimental studies of various scales of the processes occurring on the earth including the lithosphere, atmosphere, and hydrosphere. Intensive development of research in these areas is due to several factors: 1) the widespread introduction of computer technology, allowing the calculation of complex phenomena; 2) the invention and improvement of a new generation of geophysical instruments such as remote observation systems based on ships, aircraft, and satellites, providing a large amount of data to objectively reflect a broad picture of the processes; and 3) the development of measurement techniques, creating opportunities for controllable and reproducible laboratory data acquisition for generation of new ideas and concepts. Their recent developments have facilitated our research and understanding of these academic fields. The book enriches the understanding of the geophysical processes taking place in various environments (lithosphere, hydrosphere, and atmosphere), including the anthropogenic one, and it further contributes to their development. This book is a valuable resource for specialists working in the oil, gas, and engineering industry to improve their understandings of the field. 001482743 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed October 31, 2023). 001482743 650_0 $$aGeodynamics.$$0(DLC)sh 85053976 001482743 655_0 $$aElectronic books. 001482743 7001_ $$aChaplina, Tatiana,$$eeditor. 001482743 77608 $$iPrint version: $$z9819965748$$z9789819965748$$w(OCoLC)1394894959 001482743 830_0 $$aSpringer geology,$$x2197-9553 001482743 852__ $$bebk 001482743 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-981-99-6575-5$$zOnline Access$$91397441.1 001482743 909CO $$ooai:library.usi.edu:1482743$$pGLOBAL_SET 001482743 980__ $$aBIB 001482743 980__ $$aEBOOK 001482743 982__ $$aEbook 001482743 983__ $$aOnline 001482743 994__ $$a92$$bISE