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  • American Geophysical Union (AGU)  (7)
  • 1990-1994  (7)
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  • American Geophysical Union (AGU)  (7)
Language
Years
  • 1990-1994  (7)
Year
  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1994
    In:  Eos, Transactions American Geophysical Union Vol. 75, No. 13 ( 1994-03-29), p. 149-149
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 75, No. 13 ( 1994-03-29), p. 149-149
    Abstract: Bruce M. Jakosky of the University of Colorado, Boulder, has been named editor of the Journal of Geophysical Research —Planets for a term extending through the end of 1998. He succeeds Clark Chapman of the Planetary Science Institute, Tucson, Ariz. The transition will begin late this summer. Jakosky's goal as editor will be to ensure the continued success of the journal as a first‐rate place to publish major new results in all aspects of planetary sciences. Noting that the planets section of the journal has only been in existence for 3 years, Jakosky attributes its success to “the value that the planetary science community places in interactions with other areas of geophysics.” AGU's planetology section and JGR —Planets are in a special place, he says, because the planetary topics overlap with the science in AGU sections and that published in other sections of JGR. “This reflects the interdisciplinary nature of planetary science and of geophysics as a whole. There must be a good relationship with the journals and scientists working in the areas of overlap, such as tectonics or solar wind interactions. The journal should ultimately reflect the interdisciplinary nature of the field.”
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1994
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1994
    In:  Eos, Transactions American Geophysical Union Vol. 75, No. 26 ( 1994-06-28), p. 290-290
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 75, No. 26 ( 1994-06-28), p. 290-290
    Abstract: Many models have been put forward to explain how the on‐going collision between India and Asia has yielded the world's highest mountains and most expansive plateau, the Tibetan plateau. Now scientists from Dalhousie University in Halifax, Nova Scotia, Canada, writing in the journal Nature, propose a new solution:
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1994
    detail.hit.zdb_id: 24845-9
    detail.hit.zdb_id: 2118760-5
    detail.hit.zdb_id: 240154-X
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Solid Earth Vol. 95, No. B9 ( 1990-08-30), p. 14089-14089
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 95, No. B9 ( 1990-08-30), p. 14089-14089
    Abstract: This dedicated issue of the Journal of Geophysical Research contains papers dealing with all aspects of Martian science. The impetus for the issue was the Fourth International Conference on Mars, held in Tucson on January 10–13, 1990. The third conference had been held 7 years earlier (see Journal of Geophysical Research , 87 (B12), 1982); in the intervening time period, significant new analysis of the existing data has taken place, and further robotic exploration of Mars has been both planned and carried out. The papers contained in this issue reflect the mature nature of our understanding of the Martian environment, and they contain new results that significantly affect our view of the planet.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1993
    In:  Eos, Transactions American Geophysical Union Vol. 74, No. 6 ( 1993-02-09), p. 65-69
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 74, No. 6 ( 1993-02-09), p. 65-69
    Abstract: Geologists are in a quandary over the correct interpretation of paleomagnetic data for Jurassic rocks of the North American plate. Conflicting reference paleopoles and alternate methods of constructing apparent polar wander (APW) paths have led to a controversy regarding the configuration of Jurassic APW for cratonic North America. These differences have been recently disputed at meetings (see Eos , Spring Meeting Supplement, April 7, 1992, p. 94) and in an exchange of letters in the Journal of Geophysical Research‐Solid Earth [ Butler et al ., 1992; Van Fossen and Kent , 1992a]. At stake is important information concerning the Jurassic paleogeography of North America and the whole of Pangea, as well as the nature and driving mechanism of plate movements. In addition, cratonic paleopoles provide a reference frame for measuring relative displacements of tectonostratigraphic terranes.
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1993
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1993
    In:  Eos, Transactions American Geophysical Union Vol. 74, No. 4 ( 1993-01-26), p. 42-42
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 74, No. 4 ( 1993-01-26), p. 42-42
    Abstract: The Journal of Geophysical Research‐Solid Earth is planning to commemorate AGU's 75th anniversary in 1994 with a series of special invited papers dealing with particularly interesting and important frontier areas of solid Earth research. Papers concerning the full sweep of topics published in JGR‐Solid Earth are of interest. The purpose of this note is to solicit topics for these papers and the names of potential authors. Two manuscripts will be solicited for each topic, which will include such topics as the core/mantle boundary, the occurrence and role of fluids in the Earth, and the nature and origin of the geomagnetic field. We hope that these papers will document the role of AGU and its publications in the advancement of the geophysical sciences. One paper will be a historical overview of the current state of the research and how we arrived there, and the other will take a more future‐looking approach and discuss major problems remaining in the field and how they might be investigated.
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1993
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Space Physics Vol. 95, No. A11 ( 1990-11), p. 18791-18808
    In: Journal of Geophysical Research: Space Physics, American Geophysical Union (AGU), Vol. 95, No. A11 ( 1990-11), p. 18791-18808
    Abstract: The structure of intermediate shocks is studied on the basis of the resistive, nonviscous two‐fluid equations. Electron inertia effects are neglected so that the generalized Ohm's law contains only the Hall current and the electron pressure terms in addition to the usual resistive term and the electric field. As for the case of purely resistive MHD, reported recently by Hau and Sonnerup ( Journal of Geophysical Research, 94, 6539, 1989), fixed‐point analysis is performed to examine the nature of the magnetic structure near the upstream and downstream states of the intermediate shock. The one‐dimensional, steady state, resistive Hall MHD equations are then integrated numerically to generate complete shock structures which are presented in the form of magnetic hodograms. These hodograms describe fast and slow shocks in addition to intermediate shocks. As expected, the calculations show that the main effect of Hall currents is to remove the symmetry between left‐hand and right‐hand polarized shock structures found in the purely resistive case and sometimes to convert the smooth shock transitions obtained from the resistive MHD model into transitions that incorporate oscillatory standing wave train structures at their upstream and/or downstream edge. The magnetic structure in the plane of the shock near the possible upstream and downstream states of the intermediate shock, which in the case of purely resistive MHD is either a node or a saddle, can be either a node, a saddle or a spiral point, the latter corresponding to a standing wave train, when the Hall term is included. As a result, the number of possible types of magnetic hodogram topology increases from 3 in the resistive case, to a total of 20. However, it appears that the constraints provided by the shock jump conditions make certain of these topologies unattainable: only 13 of the 20 cases have been found and are reported in the paper. The relationship between small‐amplitude dispersive waves in the flow upstream or downstream of a shock and the nature of the corresponding fixed point is also discussed.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1993
    In:  Journal of Geophysical Research: Planets Vol. 98, No. E3 ( 1993-03-25), p. 5457-5458
    In: Journal of Geophysical Research: Planets, American Geophysical Union (AGU), Vol. 98, No. E3 ( 1993-03-25), p. 5457-5458
    Abstract: The Third International Conference on Laboratory Research for Planetary Atmospheres (3rd ICLRPA) was held in Palo Alto, California, on November 3, 1991, preceding the 23rd Annual Meeting of the Division for Planetary Sciences of the American Astronomical Society (DPS/AAS). These conferences continue to highlight important progress in laboratory studies with an emphasis on their relationships to models and theories of planetary atmospheres, and importantly, with a focus on those needs for data most critical both to the analyses of ground‐based and spacecraft measurements, and to the planning of new missions. This special section of the Journal of Geophysical Research‐Planets (JGR‐Planets) includes several invited and contributed papers originally presented at the 3rd ICLRPA. I. de Pater and D. Mitchell (University of California, Berkeley) discussed radio observations of planetary atmospheres and solid surfaces, and explained the role of laboratory data in the analysis of these astronomical observations. They also noted the absence of certain relevant laboratory results needed to further develop our understanding of physical properties of planets. D.C. Reuter and J.M. Sirota (NASA Goddard Space Flight Center, Greenbelt, Maryland) discussed the utility of a spectroscopic system consisting of tunable diode lasers at wavelengths out to 28 microns; a liquid helium‐4 cooled, back‐illuminated, bounded impurity‐band (BIBIB) detector; and a 100‐m White cell to measure infrared transitions in molecules of planetary interest at very high spectral resolution and detectivity. B. Bezard (Observatory of Paris, Meudon, France) considered molecular spectra for Titan to be measured from the Infrared Space Observatory and the Cassini mission over a great range of wavelengths, from the infrared to the submillimeter, with high spectral resolution. He discussed the detectability of certain hydrocarbons and nitriles, and the corresponding need for spectroscopic measurements in the laboratory. H.A. Weaver (Space Telescope Science Institute, Baltimore, Maryland) reviewed the physical and chemical nature of cometary comae, and the connection of molecules and atoms therein with the composition of cometary nuclei. P.J. Gierasch (Cornell University, Ithaca, New York) reviewed the dynamics and thermal structure of the atmospheres of the outer planets, summarizing important measurements that are feasible with remote‐sensing spectroscopic techniques. He discussed precise observations of temperatures, velocities, and abundances to determine seasonal variations in global stratospheric circulations, winds, wave phenomena, and global oscillations. W.T. Huntress (NASA Headquarters, Washington, D.C.) introduced a program for state‐of‐the‐art, integrated systems of laboratory instruments designed for planetary applications. He noted that the establishment of these Centers for Laboratory Planetary Science Studies would facilitate, for all qualified experimentalists, the complex analytical studies needed to support planetary space missions.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1993
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    BibTip Others were also interested in ...
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