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<ArticleSet>
<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>3</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2019</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Ellipsoidal spline functions for gravity data interpolation and smoothing</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>1</FirstPage>
			<LastPage>11</LastPage>
			<ELocationID EIdType="pii">75662</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2020.290542.1065</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Mostafa</FirstName>
					<LastName>Kiani Shahvandi</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Nabi</FirstName>
					<LastName>Chegini</LastName>
<Affiliation>Department of  Mathematics, Tafresh University, Tafresh, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2019</Year>
					<Month>03</Month>
					<Day>01</Day>
				</PubDate>
			</History>
		<Abstract>The aim of this paper is to study the theory of spline interpolation and smoothing problems on the surface of a triaxial ellipsoid for the Consecutive Iterated Helmholtz operator and a set of linearly independent evaluation functionals. Spline functions were introduced based on the minimization of a semi-norm in the context of a semi-Hilbert space whose domain was the surface of the ellipsoid. The semi-Hilbert space was decomposed into two different subspaces, a particular Hilbert space and the null space of the desired operator. Using surface Green’s functions for the Consecutive Iterated Helmholtz operator, the reproducing kernel for the Hilbert subspace was constructed. Spline and smoothing functions were explicitly represented based on the reproducing kernel and the evaluation functionals. An approximation formula was derived to facilitate the potential use in Earth’s gravity field data interpolation and smoothing. An application of this technique was presented to show the interpolation of potential fields over Iran. Ellipsoidal and spherical splines were compared as well. It revealed the ellipsoidal splines to be more accurate than the spherical counterparts.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Spline interpolant</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Consecutive Iterated Helmholtz Operator</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Minimization problem, Surface Green's functions, Evaluation functionals</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_75662_9fd478aed2776b7fdc22895e66145243.pdf</ArchiveCopySource>
</Article>
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