Biología general by Alvarado, Salustio

By Alvarado, Salustio

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GOCE Level 2 harmonic expansion to degree 200 and to degree 360 simulating the collocation solution Figure 4. Covariance functions of the MDT and the geostrophic surface current components based of the MDT degree variance model shown in Figure 3. Chapter 3 Detecting Ocean Currents from Satellite Altimetry, Satellite Gravity and Ocean Data Zizhan Zhang 1'2 Yang L u 1'3 Houtse HSU 1'3 1 Institute of Geodesy and Geophysics, Chinese Academy of Sciences, 340 Xudong Street, Wuhan, China, 430077 2 Graduate School of the Chinese Academy of Sciences, Beijing, China, 100049 3 Unite Center for Astro-geodynamics Research, CAS, Shanghai, China, 200030 Abstract: With the preparation and launch of the high accuracy geodetic missions CHAMP, GRACE and GOCE, the geoid models have been improved greatly.

Deg. °12t ................... _ .... 01 Lag [sph. degrees] 0 1 2 3 4 lag (deg) Figure 2. GOCE Level 2 harmonic expansion to degree 200 and to degree 360 simulating the collocation solution Figure 4. Covariance functions of the MDT and the geostrophic surface current components based of the MDT degree variance model shown in Figure 3. Chapter 3 Detecting Ocean Currents from Satellite Altimetry, Satellite Gravity and Ocean Data Zizhan Zhang 1'2 Yang L u 1'3 Houtse HSU 1'3 1 Institute of Geodesy and Geophysics, Chinese Academy of Sciences, 340 Xudong Street, Wuhan, China, 430077 2 Graduate School of the Chinese Academy of Sciences, Beijing, China, 100049 3 Unite Center for Astro-geodynamics Research, CAS, Shanghai, China, 200030 Abstract: With the preparation and launch of the high accuracy geodetic missions CHAMP, GRACE and GOCE, the geoid models have been improved greatly.

4 degrees for the MSS data. The estimated MDT and it error estimates are shown in Figure 3. Compared to the MDTs in Figure 2 this MDT show the same general pattern though much more details are recovered. Those details are probably spurious in terms of ocean circulation are may be caused by edge effects at coastlines and by unrecovered errors in the data. Furthermore the Southeastern sub-region appeared to be biased by long wavelength signals that are not recovered fully within each of the sub-regions.

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