000 | 01784nam a22004575i 4500 | ||
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001 | 978-3-540-40963-2 | ||
003 | DE-He213 | ||
005 | 20160624101847.0 | ||
007 | cr nn 008mamaa | ||
008 | 121227s1983 gw | s |||| 0|eng d | ||
020 |
_a9783540409632 _9978-3-540-40963-2 |
||
024 | 7 |
_a10.1007/3-540-12333-4 _2doi |
|
050 | 4 | _aQC19.2-20.85 | |
072 | 7 |
_aPHU _2bicssc |
|
072 | 7 |
_aSCI040000 _2bisacsh |
|
082 | 0 | 4 |
_a530.1 _223 |
245 | 1 | 0 |
_aMathematical Structure of the Singularities at the Transitions Between Steady States in Hydrodynamic Systems _h[electronic resource] / _cedited by Hampton N. Shirer, Robert Wells. |
260 | 1 |
_aBerlin, Heidelberg : _bSpringer Berlin Heidelberg, _c1983. |
|
264 | 1 |
_aBerlin, Heidelberg : _bSpringer Berlin Heidelberg, _c1983. |
|
300 |
_aXI, 281 p. _bonline resource. |
||
336 |
_atext _btxt _2rdacontent |
||
337 |
_acomputer _bc _2rdamedia |
||
338 |
_aonline resource _bcr _2rdacarrier |
||
347 |
_atext file _bPDF _2rda |
||
490 | 1 |
_aLecture Notes in Physics, _x0075-8450 ; _v185 |
|
505 | 0 | _ato contact catastrophe theory -- Rayleigh-BĂ©nard convection -- Quasi-Geostrophic flow in a channel -- Rotating axisymmetric flow -- Stability and unfoldings. | |
650 | 0 | _aPhysics. | |
650 | 0 | _aMathematical physics. | |
650 | 1 | 4 | _aPhysics. |
650 | 2 | 4 | _aMathematical and Computational Physics. |
700 | 1 |
_aShirer, Hampton N. _eeditor. |
|
700 | 1 |
_aWells, Robert. _eeditor. |
|
710 | 2 | _aSpringerLink (Online service) | |
773 | 0 | _tSpringer eBooks | |
776 | 0 | 8 |
_iPrinted edition: _z9783540123330 |
786 | _dSpringer | ||
830 | 0 |
_aLecture Notes in Physics, _x0075-8450 ; _v185 |
|
856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/3-540-12333-4 |
942 |
_2EBK2402 _cEBK |
||
999 |
_c31696 _d31696 |