WebA normalized version of Christopher Jekeli’s Gaussian averaging function Calling Sequence from geoid_toolkit.gauss_weights import gauss_weights wl = 2.0 * np . pi * gauss_weights ( hw , LMAX ) Web25 giu 2024 · Limited by the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) measurement principle and sensors, the spatial resolution of mass flux solutions is about 2–3° in mid-latitudes at monthly intervals. To retrieve a mass flux solution in the Tibetan Plateau (TP) with better visual spatial resolution, we …
Additional methods for the stable calculation of isotropic Gaussian ...
WebA comparison is made of the errors in determining the geoid undulation according to the conventional Molodenskii truncation theory and its modifications as suggested by Molodenskii (1958) and Meiss... WebFlyygeli ja kaakeli: With Heikki Helakorpi, Risto Hiltunen. rob burrows before and after
Improved convergence rates for the truncation error in …
WebFinally, Gaussian smoothing (Jekeli 1981) is applied. We test various radii for the Gaussian function, from 500 km to 0 km in order to evaluate which represents the best agreement wih steric corrected altimetry in the Black Sea. Since the degree-one coefficients are not part of these GRACE solutions, an estimate of Web1 dic 2024 · A quick way to remove random and systematic errors from GRACE models is by using a low-pass filter, with the isotropic Gaussian filter (Jekeli, 1981) being the most prevalent choice. The filtering is performed in the spherical harmonic domain, i.e., by multiplying the spherical harmonic coefficients of the GRACE models with the … Web27 ago 2024 · The GF of Jekeli (1981, Eq. 56) oscillates for some high degrees, which is a problem that limits its application for smoothing the gravity anomalies inside the cap. For … robbs vets motherwell