000			03652nam a22004575i 4500
001			978-1-4020-6637-5
003			DE-He213
005			20251006084536.0
007			cr nn 008mamaa
008			100531s2007 ne | s |||| 0|eng d
020			_a9781402066375
020			_a99781402066375
024	7		_a10.1007/978-1-4020-6637-5 _2doi
082	0	4	_a520 _223
100	1		_aAlperovich, Leonid S. _eauthor.
245	1	0	_aHydromagnetic Waves in the Magnetosphere and the Ionosphere _h[electronic resource] / _cby Leonid S. Alperovich, Evgeny N. Fedorov.
264		1	_aDordrecht : _bSpringer Netherlands, _c2007.
300			_bonline resource.
336			_atext _btxt _2rdacontent
337			_acomputer _bc _2rdamedia
338			_aonline resource _bcr _2rdacarrier
347			_atext file _bPDF _2rda
490	1		_aAstrophysics and Space Science Library, _x0067-0057 ; _v353
505	0		_aPartially Ionized Plasma -- Electrodynamic Properties of Space -- ULF-Waves on the Ground and in Space -- Magnetohydrodynamic Waves -- Hydromagnetic Resonators -- FLR in Plasma Configurations -- MHD-Waves in Layered Media -- Propagation of MHD-Beams -- Inhomogeneous Ionosphere -- Effective Conductivity of a Cloudy Ionosphere -- ULF-Sounding of Magnetosphere and Earth -- MHD-Wave Exposure on the Ionosphere -- MHD-Wave Generation by HF-Heating -- Active Cloud Releases and MHD-Emission -- MHD After-Effects of a Sound Impact.
520			_aThe book deals with Ultra-Low-Frequency (ULF)-electromagnetic waves observed on Earth and in Space. These are so-called geomagnetic variations or pulsations. Alfvén's discovery related to the influence of the strong magnetic field on the conducting fluids (magnetohydrodynamics) led to development of the concept that the ULF-waves are magnetospheric magnetohydrodynamic (MHD)-waves. MHD-waves at their propagation gather information about the magnetosphere, ionosphere, and the ground. There are two applied aspects based on using the ULF electromagnetic oscillations. The first one is the ground-based diagnostics of the magnetosphere. This is an attempt to monitor in the real time the magnetosphere size, distance to the last closed field-lines, distribution of the cold plasma, etc. The second one is the deep electromagnetic sounding of the Earth. The basis for these studies is the capability of any electromagnetic wave to penetrate a conductor to a finite depth. The ULF-waves can reach the depth of a few hundred kilometers. Thus, geophysicists now have a unique tool that can be applied to study the solid Earth as well as its gas-plasma shells - the ionosphere and magnetosphere. This book integrates topics pertaining to all scales of the MHD-waves, emphasizing the linkages between the ULF-waves below the ionosphere on the ground and magnetospheric MHD-waves. It will be most helpful to graduate and post-graduate students, familiar with advanced calculus, who study the science of MHD-waves in the magnetosphere and ionosphere.
650		0	_aPHYSICS.
650		0	_aASTRONOMY.
650		0	_aASTROPHYSICS.
650	1	4	_aPHYSICS.
650	2	4	_aASTRONOMY, ASTROPHYSICS AND COSMOLOGY.
650	2	4	_aEXTRATERRESTRIAL PHYSICS, SPACE SCIENCES.
700	1		_aFedorov, Evgeny N. _eauthor.
710	2		_aSpringerLink (Online service)
773	0		_tSpringer eBooks
776	0	8	_iPrinted edition: _z9781402066368
830		0	_aAstrophysics and Space Science Library, _x0067-0057 ; _v353
856	4	0	_uhttp://dx.doi.org/10.1007/978-1-4020-6637-5 _zVer el texto completo en las instalaciones del CICY
912			_aZDB-2-PHA
942			_2ddc _cER
999			_c61796 _d61796