Combining altimetric/gravimetric and ocean model mean dynamic topography models in the GOCINA region

9Citations
Citations of this article
14Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Initially, existing mean dynamic topography (MDT) models were collected and reviewed. The models were corrected for the differences in averaging period using the annual anomalies computed from satellite altimetry. Then a composite MDT was derived as the mean value in each grid node together with a standard deviation to represent its error. A new synthetic MDT was obtained from the new mean sea surface (MSS) KMS04 combined with a regional geoid updated using GRACE gravity and gravimetric data from a recent airborne survey. Compared with the composite MDT the synthetic MDT showed very similar results. Then combination methods were tested for the computation of MDT models from gravity data and MSS data. Both a rigorous and an iterative combination method have been tested in the GOCINA region. At this stage, the iterative combination method with its efficient handling of large data sets covering the whole region appears to give the best solution. Naturally, the errors associated with the MDT can be obtained using the rigorous method only. © Springer-Verlag Berlin Heidelberg 2007.

Cite

CITATION STYLE

APA

Knudsen, P., Andersen, O. B., Forsberg, R., Föh, H. P., Olesen, A. V., Vest, A. L., … Schaeffer, P. (2007). Combining altimetric/gravimetric and ocean model mean dynamic topography models in the GOCINA region. In International Association of Geodesy Symposia (Vol. 130, pp. 3–10). https://doi.org/10.1007/978-3-540-49350-1_1

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free