9,551 research outputs found

    Geoid undulations and gravity anomalies over the Aral Sea, the Black Sea and the Caspian Sea from a combined GEOS-3/SEASAT/GEOSAT altimeter data set

    Get PDF
    Satellite-based altimetric data taken by GOES-3, SEASAT, and GEOSAT over the Aral Sea, the Black Sea, and the Caspian Sea are analyzed and a least squares collocation technique is used to predict the geoid undulations on a 0.25x0.25 deg. grid and to transform these geoid undulations to free air gravity anomalies. Rapp's 180x180 geopotential model is used as the reference surface for the collocation procedure. The result of geoid to gravity transformation is, however, sensitive to the information content of the reference geopotential model used. For example, considerable detailed surface gravity data were incorporated into the reference model over the Black Sea, resulting in a reference model with significant information content at short wavelengths. Thus, estimation of short wavelength gravity anomalies from gridded geoid heights is generally reliable over regions such as the Black Sea, using the conventional collocation technique with local empirical covariance functions. Over regions such as the Caspian Sea, where detailed surface data are generally not incorporated into the reference model, unconventional techniques are needed to obtain reliable gravity anomalies. Based on the predicted gravity anomalies over these inland seas, speculative tectonic structures are identified and geophysical processes are inferred

    User's guide: Programs for processing altimeter data over inland seas

    Get PDF
    The programs described were developed to process GEODYN-formatted satellite altimeter data, and to apply the processed results to predict geoid undulations and gravity anomalies of inland sea areas. These programs are written in standard FORTRAN 77 and are designed to run on the NSESCC IBM 3081(MVS) computer. Because of the experimental nature of these programs they are tailored to the geographical area analyzed. The attached program listings are customized for processing the altimeter data over the Black Sea. Users interested in the Caspian Sea data are expected to modify each program, although the required modifications are generally minor. Program control parameters are defined in the programs via PARAMETER statements and/or DATA statements. Other auxiliary parameters, such as labels, are hard-wired into the programs. Large data files are read in or written out through different input or output units. The program listings of these programs are accompanied by sample IBM job control language (JCL) images. Familiarity with IBM JCL and the TEMPLATE graphic package is assumed

    Analysis of altimetry over inland seas

    Get PDF
    Satellite-based altimetric data taken by GEOS-3 and SEASAT over the Black Sea and Caspian Sea are analyzed and a least squares collocation technique is used to predict the geoid undulation on a .25-degree by .25-degree grid and to transform these geoid undulations to free air gravity anomalies. This project entailed processing satellite altimeter data over inland seas for recovery of area mean gravity information. Gravity information in this area of the world is not readily available, so the possibility of obtaining it from the processing of altimeter observations is attractive. The principal objective was to complete and extend analyses done in a previous study, verify those results, and document the results and techniques. A secondary objective was to improve the algorithms and results, if possible. The approach used involved editing geoid height data to remove overland data; evaluating geoid height differences at crossover points; removing orbit errors from geoid heights using crossover differences; gridding geoid height data at .25-degree by .25-degree intervals; and estimating the gravity anomalies from gridded geoid heights using the collocation technique

    Analysis of altimetry over the Aral Sea

    Get PDF
    Satellite based altimetric data taken by GEOS-3, SEASAT, and GEOSAT over the Aral Sea are analyzed and a least squares collocation technique is used to predict the geoid undulations on a 0.25 by 0.25 degree grid and to transform these geoid undulations to free air gravity anomalies. Rapp's 180 by 180 geopotential model is taken as the empirical model. The collocation procedure is performed with a set of local residual empirical covariance functions. For comparison, Rapp's global covariance functions and Jordan's self-consistent theoretical covariance functions based on Jordan's formulation and on locally derived parameters are also used to grid geoid undulations and to predict gravity anomalies. The sensitivity of the collocation results to the choice of covariance functions is discussed

    SHOP2: An HTN Planning System

    Full text link
    The SHOP2 planning system received one of the awards for distinguished performance in the 2002 International Planning Competition. This paper describes the features of SHOP2 which enabled it to excel in the competition, especially those aspects of SHOP2 that deal with temporal and metric planning domains

    Solicitor-Client Privilege and Litigation Privilege in Civil Litigation

    Get PDF
    This paper examines the nature and scope of solicitor-client privilege and litigation privilege. Contrary to a recent article suggesting that there are no real differences between them, it is argued that the two privileges are distinct in terms of both their underlying purposes and the requisite conditions to invoke them. Most importantly, confidentiality is a requirement of solicitor-client privilege but not of litigation privilege. Moreover, extending solicitor-client privilege to communications from third parties (as proposed in the recent article) would be dangerous. It would stretch the scope of that privilege beyond its justification of necessity, and open the way for lawyers to develop and offer a new product line : namely, confidentiality. Whatever third party communications a client desires to keep secret could conveniently be clothed with privilege simply by having lawyers act as a conduit for such communications and asking them for their legal opinion thereon (as it now appears the tobacco industry has been doing for some time with research data). A strong policy reason for confining solicitor-client privilege to direct communications between lawyer and client is to limit the potential abuse of the privilege. Further, since the assertion of privilege inevitably impedes the truth finding process, the public interest is best served by confining the scope of solicitor-client privilege within narrow limits. For the same reason, the concept of agents must be accorded a narrow meaning in the context of solicitor-client privilege, so as not to render agency a back-door through which third party communications attract solicitor-client privilege

    Standardizing the reporting of Mendelian randomization studies

    Get PDF
    • …
    corecore