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Karl Rawer – författare

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5 produkter

  1. Karl Rawer - Geophysik III / Geophysics III. Tillgänglighet: Lägg i varukorg

    Geophysik III / Geophysics III

    Av Karl Rawer

    2014

    1291 kr

    Lägg i varukorg

  2. K. Rawer, K. Suchy, G. Schmidtke, Karl Rawer - Geophysik III / Geophysics III, E-bok. Tillgänglighet: Lägg i varukorg

    Geophysik III / Geophysics III

    Av K. Rawer, K. Suchy m. fl.

    E-bok, 2013

    1427 kr

    Lägg i varukorg

    This Encyclopedia aims, basically, at summanzmg the wealth of well­ established facts and outlining the relevant theories in the different branches of physics. With this as goal, the writers were asked to present their specific field in such a way that access is possible to any scientist without …

  3. G. Schmidtke, K. Suchy, K. Rawer, Karl Rawer - Geophysik III / Geophysics III, Häftad. Tillgänglighet: Lägg i varukorg

    Geophysik III / Geophysics III

    Av G. Schmidtke, K. Suchy m. fl.

    Häftad, 2011

    1095 kr

    Lägg i varukorg

    This Encyclopedia aims, basically, at summanzmg the wealth of well­ established facts and outlining the relevant theories in the different branches of physics. With this as goal, the writers were asked to present their specific field in such a way that access is possible to any scientist without …

  4. Karl Rawer - Geophysics III/Geophysik III, Häftad. Tillgänglighet: Lägg i varukorg

    Geophysics III/Geophysik III

    Part III/Teil III

    Av Karl Rawer

    Häftad, 2012

    1095 kr

    Lägg i varukorg

    Sect. 14. 297 for such slow variations the effect described under 2. above will be by far the most predominant. In fact, the equipment provides a record of the time derivative of the element in question. 6) Records of the time derivatives of magnetic elements can, however, be obtained in a more …

  5. G.M. Nikol'skij, K. Rawer, P. Stubbe, L. Thomas, T. Yonezawa, Karl Rawer - Geophysik III, Häftad. Tillgänglighet: Lägg i varukorg

    Geophysik III

    Av G.M. Nikol'skij, K. Rawer m. fl.

    Häftad, 2012

    1095 kr

    Lägg i varukorg

    83 input to the ions is balanced by a cooling to atomic oxygen, the major neutral constituent, and measurements of the difference between ion and neutral tem­ perature permit the determination of atomic oxygen concentrations. Using this approach, ALCA YDE et al. 6 have shown from data taken above …