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

小客車

書(shū)目名稱Dynamic Planet影響因子(影響力)




書(shū)目名稱Dynamic Planet影響因子(影響力)學(xué)科排名




書(shū)目名稱Dynamic Planet網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Dynamic Planet網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Dynamic Planet被引頻次




書(shū)目名稱Dynamic Planet被引頻次學(xué)科排名




書(shū)目名稱Dynamic Planet年度引用




書(shū)目名稱Dynamic Planet年度引用學(xué)科排名




書(shū)目名稱Dynamic Planet讀者反饋




書(shū)目名稱Dynamic Planet讀者反饋學(xué)科排名

alcohol-abuse

Obstacle

European Sea Level Monitoring: Implementation of ESEAS Quality Control extends to other information such as documentation of datum information, metadata, exchange format, application classification, and levels of quality control. In relation to tsunami-enabled tide gauges, quality control is related to the availability of data in real-time and the use of automatic control and analysis procedures.

意外的成功

gnarled

原始

Regime Switching and the Wage-Price Spirallation length. Combining the MDT characteristics with the estimated geoid errors in the spectral domain resulted in a-posteori error estimates. In the two cases the MDT errors were improved from 20 cm to 6 cm and 5 cm respectively. For the geostrophic surface current components the errors were improved from 23 cm/s to 18 cm/s and 16 cm/s.

原始

Nonlinear Deterministic Theoriesthe spatial-temporal evolution of these signals suggests that the 18–20-month signal is an internal mode of the IO, while that of the 30-month component propagates from the Pacific Ocean, in particular with a much stronger signal during the period from 1998 to 2003.

Nebulous

Regime Switching and the Wage-Price Spiral all satellites the error estimates for the radial component exhibit significant geographical pattern — even for TOPEX. The error components are also taken to calculate time series of relative range biases and geocentre offsets between all altimeter missions.

小口啜飲

Tabulatoren, Tabellen und Diagramme, simulated the gravity measurements on the moving ice sheet by evaluating how well the gravity values of the second set (4 by 4 points) could be estimated from the gravity values of the first sets (5 by 5 points). The result suggests that the measurements with an appropriate data processing enable 10 μGal accuracy even on the moving ice sheet.

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