Titlebook: Solar and Interplanetary Dynamics; M. Dryer,E. Tandberg-Hanssen Book 1980 International Astronomical Union 1980 Variation.astrophysics.cos

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書目名稱Solar and Interplanetary Dynamics影響因子(影響力)




書目名稱Solar and Interplanetary Dynamics影響因子(影響力)學科排名




書目名稱Solar and Interplanetary Dynamics網(wǎng)絡公開度




書目名稱Solar and Interplanetary Dynamics網(wǎng)絡公開度學科排名




書目名稱Solar and Interplanetary Dynamics被引頻次




書目名稱Solar and Interplanetary Dynamics被引頻次學科排名




書目名稱Solar and Interplanetary Dynamics年度引用




書目名稱Solar and Interplanetary Dynamics年度引用學科排名




書目名稱Solar and Interplanetary Dynamics讀者反饋




書目名稱Solar and Interplanetary Dynamics讀者反饋學科排名

TERRA

A Two-Level Solar Dynamo Based on Solar Activity, Convection, and Differential Rotationhere. It seems natural, therefore, to expect the reconnection aspect of conversion to be located there, where the least work needs to be performed. To transfer the generated flux there, we may add to conversion another spontaneous process: . of bipolar structure (Parker, 1955). To transfer the recon

ALIAS

The Origin of Interplanetary Sectorsize the force-free condition, . × . = 0, and in fact make the more restrictive assumption that this region is current free. The magnetic field in this region can be derived from a solution to the Laplace equation.

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Stellar Mass Flux and Coronal Heating by Shock Wavese and dissipation terms. The input parameters are the base pressure, the base temperature and the mechanical flux introduced at chromospheric level in form of shock waves. If these three parameters allow a solar wind expansion, the output results are the radial variations of the density, of the temp

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Book 1980 be understood only by the coupling of solar and interplan- etary topics in an intimate observational and theoretical structure. This book, intended for active research scientists and advanced grad- uate students, is an important step in this direction. The background of solar and interplanetary dyn

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K. V. Sheridan,G. A. Dulkl ein besonders gesch?ftiges Jahr. Wie Richard Bellman es ausdrückte: ?Man wu?te nie, wo Erd?s sich gerade aufhielt, nicht einmal das Land kannte man. Aber man konnte sicher sein, da? er im Laufe eines ganzen Jahres überall erschien. Er kam einem ergodischen Teilchen [eines, das schlie?lich alle phy

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