Jekeli 1981
Web白希选,闫昊明,朱耀仲,彭鹏1 中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室,武汉 430077 2中国 ... 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 …
Jekeli 1981
Did you know?
Web1 set 2009 · Spatial low‐pass filtering is necessary for processing the GRACE time‐variable gravity (TVG) data which are otherwise plagued with short‐wavelength noises. Here we … WebSummaries. It looks like we don't have any Plot Summaries for this title yet. Be the first to contribute! Just click the "Edit page" button at the bottom of the page or learn more in the …
Web28 mag 2024 · Some examples are the Pellinen filter (Meissl 1971), the truncated Gaussian filter (Jekeli 1981, p. 20; Piretzidis and Sideris 2024), the Hanning filter ... Kostelecký J (1981) Some possibilities for determining the influence of earth body tides on the motion of artificial satellites. Adv Space Res 1(6):29–35. WebChristopher Jekeli Report No. 327 Geodetic and GeoInformation Science Department of Civil and Environmental Engineering and Geodetic Science The Ohio State University …
WebAlternative methods to smooth the Earth's gravity field. C. Jekeli. Published 1 December 1981. Geology. Convolutions on the sphere with corresponding convolution theorems are … 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 nov 2013 · The (Gaussian) weighted function resembles for small α and geopotential global models (e.g. EGM2008 and GOCE up to degree was normalized so that the global integral of W(α) is equal to 1. and order 250) so that we can make comparisons between the grav- In terms of the spherical harmonic development, Jekeli (1981) ity anomalies at …
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 … rubbermaid bicycle shed partsWeband Jekeli (1981). The contents of this paper have been organised as follows. The derivations of the strict integral formulas for the geoid and gravity anomaly biases are … rubbermaid bottles bpa freeWebThe oblate and prolate spheroidal harmonic expansions as well as the triaxial ellipsoid harmonics can be applied to express the gravitational field to agree with the shape of the body (Jekeli 1981 ... rubbermaid blue ice lunch packWebBack to Results. Alternative methods to smooth the Earth's gravity field Convolutions on the sphere with corresponding convolution theorems are developed for one and two … rubbermaid brilliance 20 pcWeband Jekeli (1981). The contents of this paper have been organised as follows. The derivations of the strict integral formulas for the geoid and gravity anomaly biases are outlined in Sect. 2. The next section introduces the corresponding binomial expansions. It is then shown how the geoid bias can be used in geoid determination by an EGM and rubbermaid blue ice twin lunch packWebAs for spatial smoothing, apart from the classical isotropic filter (Jekeli 1981; Wahr et al. 1998), non-isotropic Gaussian filters were also proposed (Han et al. 2005a; Guo et al. 2010). rubbermaid box graterWebFlyygeli ja kaakeli (TV Movie 1982) cast and crew credits, including actors, actresses, directors, writers and more. rubbermaid blue recycling bin