Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Braulio V. Sanchez"'
How could we have an outlier detector that works even with nondimensional data, and ranks together both singleton microclusters ('one-off' outliers) and nonsingleton microclusters by their anomaly scores? How to obtain scores that are principled in o
Externí odkaz:
http://arxiv.org/abs/2403.08027
Autor:
Braulio V. Sanchez
Publikováno v:
Marine Geodesy. 31:181-212
This paper deals with the normal modes of the global oceans. More specifically, it reviews some of the work done in association with the modeling, detection, and application of the barotropic, basin-wide normal modes. The paper presents some results
Publikováno v:
Journal of Physical Oceanography. 27:1371-1385
The quasi-stationary sea surface topography (QSST) and associated oceanic circulation is determined by means of a characteristic function technique. The method was originally implemented in an ideal simplified case. The present application involves a
Publikováno v:
Journal of Geophysical Research. 109
The objective of the investigation is to determine the motion of the rotational axis of Mars as a result of mass variations in the atmosphere and condensation and sublimation of CO2 ice on the polar caps. A planet experiences this type of motion if i
Publikováno v:
Journal of Geophysical Research. 108
[1] Atmospheric rotational effects on Mars are computed and analyzed. Both axial (ΔLOD) and equatorial effects (polar motion) are evaluated. Surface values of stress and pressure from the NASA Ames general circulation model are used as inputs to com
Publikováno v:
Journal of Geophysical Research. 107
[1] We calculate that the oceanic torque vectors (x, y, z components) acting on the solid Earth using the Parallel Ocean Climate Model (POCM) output data at 3-day intervals for the period 1988–1995. This study examined three distinct types of torqu
Autor:
Steven M. Klosko, Nikolaos K. Pavlis, R. G. Williamson, R. S. Nerem, E. C. Pavlis, J. W. Robbins, J. J. McCarthy, J. C. Chan, G. B. Patel, K. E. Rachlin, J. A. Marshall, Francis J. Lerch, Douglas S. Chinn, Scott B. Luthcke, T. L. Felsentreger, S. Kapoor, N. L. Chandler, D. E. Pavlis, Braulio V. Sanchez, B. H. Putney
Publikováno v:
Journal of Geophysical Research
An improved model of Earth's gravitational field, GEM-T3, has been developed from a combination of satellite tracking, satellite altimeter, and surface gravimetric data. GEM-T3 provides a significant improvement in the modeling of the gravity field a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::121700d90c7319e699248e888c3e199e
https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834043
https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834043
Autor:
S. M. Klosko, T. L. Felsentreger, G. B. Patel, Francis J. Lerch, B. H. Putney, James G. Marsh, K. E. Rachlin, T. L. Engelis, E. C. Pavlis, Braulio V. Sanchez, R. G. Williamson, S. Kapoor, N. L. Chandler, L. E. Braatz, J. W. Robbins, W. F. Eddy, Douglas S. Chinn
Publikováno v:
Journal of Geophysical Research
The GEM-T2 is the latest in a series of Goddard Earth Models of the terrestrial field. It was designed to bring modeling capabilities one step closer towards ultimately determining the TOPEX/Poseidon satellite's radial position to an accuracy of 10-c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76385641b10ae825e624294738e7f9c3
https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834035
https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834035
Autor:
Braulio V. Sanchez, Nikolaos K. Pavlis
Publikováno v:
Journal of Geophysical Research. 100:25229
Tidal models for the main diurnal and semidiurnal constituents have been computed from TOPEX altimeter data and a set of Proudman functions computed numerically in the space defined by the ocean basins. The accurate modeling of the ocean tides is nec
Publikováno v:
Marine Geodesy. 9:71-91
An objective analysis technique is described which permits an extrapolation, over the entire basin, of amplitudes and phases of the tidal height field given at a few locations in the basin. The method depends on expansion of the tidal height field in