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000807147 019__ $$a987911207$$a988280765$$a992539160$$a1011954797
000807147 020__ $$a9783319566399$$q(electronic book)
000807147 020__ $$a3319566393$$q(electronic book)
000807147 020__ $$z9783319566382
000807147 020__ $$z3319566385
000807147 0247_ $$a10.1007/978-3-319-56639-9$$2doi
000807147 035__ $$aSP(OCoLC)ocn988169587
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000807147 049__ $$aISEA
000807147 050_4 $$aQB335.A52
000807147 08204 $$a526/.709989$$223
000807147 1001_ $$aKlokočník, J.$$q(Jaroslav),$$eauthor.
000807147 24510 $$aGravitational atlas of Antarctica /$$cJaroslav Klokočník, Jan Kostelecký, Aleš Bezděk.
000807147 264_1 $$aCham :$$bSpringer,$$c2017.
000807147 300__ $$a1 online resource :$$bcolor illustrations
000807147 336__ $$atext$$btxt$$2rdacontent
000807147 337__ $$acomputer$$bc$$2rdamedia
000807147 338__ $$aonline resource$$bcr$$2rdacarrier
000807147 347__ $$atext file$$bPDF$$2rda
000807147 4901_ $$aSpringer geophysics
000807147 504__ $$aIncludes bibliographical references.
000807147 5050_ $$aAcknowledgements; Contents; Abstract; 1 Introduction; References; 2 Theory; 2.1 Definitions; 2.2 Comments on the Theory; References; 3 Data; 3.1 Recent High-Resolution Gravitational Field Model EIGEN 6C4; 3.2 Bedrock Topography Model BEDMAP 2; 3.3 A Combination of the Gravity and Bedrock Topography Data RET 14; 3.4 Other Data; 3.5 Practical Guide to Figures in this Atlas; References; 4 Antarctica-A General Look; References; 5 Segments and Selected Details; References
000807147 506__ $$aAccess limited to authorized users.
000807147 520__ $$aThis book presents maps of Antarctica, exploring various aspects of its disturbing geopotential and based on the EIGEN 6C4 model, arguably the best gravitational field model currently available. It also provides the latest data on Antarctica?s bedrock topography according to Bedmap 2. In an extensive series of segment maps the book highlights (i) a gravity anomaly (disturbance), (ii) the Marussi tensor of the second derivatives of the disturbing geopotential, (iii) invariants and their ratios, (iv) the strike angle, and (v) virtual deformations. Due to their various degrees of sensitivity to the density contrasts of causative bodies under the Earth?s surface, these maps provide many details that have a range of potential geo-applications. They guide the reader through the entire continent, in segments divided by 30 degrees of longitude, and through geodetic latitudes of between 60 and 90 degrees south. Each segment is complemented by detailed zoom-in maps for selected localities of special interest.
000807147 588__ $$aOnline resource; title from PDF title page (viewed June 7, 2017).
000807147 650_0 $$aGravity$$zAntarctica$$vAtlases.
000807147 650_0 $$aGravitational fields$$vAtlases.
000807147 7001_ $$aKostelecký, Jan.
000807147 7001_ $$aBezděk, Aleš,$$d1970-
000807147 77608 $$iPrint version:$$z3319566385$$z9783319566382$$w(OCoLC)975131978
000807147 830_0 $$aSpringer geophysics.
000807147 852__ $$bebk
000807147 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-319-56639-9$$zOnline Access$$91397441.1
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000807147 980__ $$aEBOOK
000807147 980__ $$aBIB
000807147 982__ $$aEbook
000807147 983__ $$aOnline
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