Titlebook: Dynamic Planet; Monitoring and Under Paul Tregoning,Chris Rizos Book 2007 Springer-Verlag Berlin Heidelberg 2007 Ocean.Planet.Tide.geodesy.

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Dynamic Planet978-3-540-49350-1Series ISSN 0939-9585 Series E-ISSN 2197-9359

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0939-9585 Overview: Proceedings of the IAG conference Dynamic Planet - Monitoring and Understanding a Dynamic Planet with Geodetic and Oceanographic Tools978-3-662-50115-3978-3-540-49350-1Series ISSN 0939-9585 Series E-ISSN 2197-9359

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Nonlinear Deterministic Theories derived DOT map. This independent knowledge of surface currents from the altimetry/geoid derived DOT is used in combination with the salinity and temperature data from NOAA’s WOA01 to retrieve the ocean currents as a function of depth. At 2000db, comparisons of the retrieved velocities of the deep

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The Dynamic Role of Wages and Pricesations, all of which are either co-located or close to tide gauges. In this paper, we compare vertical land movements obtained from both geodetic methods with estimates of vertical land movements from high quality, independent geological and geophysical evidence, and derive a GPS-specific bias for w

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Wages, Regime Switching, and Cyclesnow accumulation rate in the first half of 2005 ever recorded in the past decade since the inception of the GC-Net. The QSCAT algorithms developed for Greenland are adapted for Antarctica. QSCAT results show strong melt in 2002 and prolonged melt in 2005 at McMurdo. New extensive ice layers, created

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The Dynamic Role of Wages and Pricesels. The inter-comparison in terms of mean value and standard deviation of the differences between the tidal heights on the 15′ × 15′ grid resulted in mean values up to 3 mm and standard deviations ranging from 16 to 26 mm. However, maximum values of differences exceed several dm. On the other hand,

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Tabulatoren, Tabellen und Diagramme,ment while La Nina episodes delay the occurrence of upwelling events in the area. The intensity or strength of El Niño and La Niña episodes seems to influence the extent/ magnitude of the upwelling area.

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Datenaustausch mit Windows-Anwendungen,ments, etc). We then discuss the solutions obtained by different analysis centres (when available) for all DORIS stations in the Antarctic region. In particular, we use several ITRFs (from the early ITRF96 to ITRF2000) to see their impact on the derived velocities in Antarctica. An emphasis is given