Estimation of a Linear Transformation.

The problem which suggested this study arose in glaciology. Markers were placed in a glacier at points (xi sub c) and their positions, as measured by surveying techniques, were recorded at x sub i. Several years later a new survey was made by the same method yielding measurements y sub i of the true...

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Bibliographic Details
Main Authors: Gleser,Leon Jay, Watson,Geoffrey S.
Other Authors: PRINCETON UNIV N J DEPT OF STATISTICS
Format: Text
Language:English
Published: 1972
Subjects:
Eta
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0747977
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0747977
id ftdtic:AD0747977
record_format openpolar
spelling ftdtic:AD0747977 2023-05-15T16:37:42+02:00 Estimation of a Linear Transformation. Gleser,Leon Jay Watson,Geoffrey S. PRINCETON UNIV N J DEPT OF STATISTICS 1972-08 text/html http://www.dtic.mil/docs/citations/AD0747977 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0747977 en eng http://www.dtic.mil/docs/citations/AD0747977 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Statistics and Probability (*STATISTICAL ANALYSIS DECISION THEORY) (*GLACIERS MOTION) MATHEMATICAL MODELS STATISTICAL DISTRIBUTIONS TRANSFORMATIONS(MATHEMATICS) RANDOM VARIABLES PROBABILITY MATRICES(MATHEMATICS) DEFORMATION SIMULATION MAXIMUM LIKELIHOOD ESTIMATION NORMAL DENSITY FUNCTIONS Text 1972 ftdtic 2016-02-19T02:00:04Z The problem which suggested this study arose in glaciology. Markers were placed in a glacier at points (xi sub c) and their positions, as measured by surveying techniques, were recorded at x sub i. Several years later a new survey was made by the same method yielding measurements y sub i of the true positions eta sub i. It was assumed that eta sub i = B(xi sub i) where the matrix B describing the deformation of the glacier is the object of interest. It seemed reasonable to assume a multivariate normal distribution for the errors on both occasions with a covariance matrix (sigma squared) E, with E known and so the problem can be transformed to make E = I. This paper deals with this problem where the vectors are p dimensional. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Eta ENVELOPE(-62.917,-62.917,-64.300,-64.300)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Statistics and Probability
(*STATISTICAL ANALYSIS
DECISION THEORY)
(*GLACIERS
MOTION)
MATHEMATICAL MODELS
STATISTICAL DISTRIBUTIONS
TRANSFORMATIONS(MATHEMATICS)
RANDOM VARIABLES
PROBABILITY
MATRICES(MATHEMATICS)
DEFORMATION
SIMULATION
MAXIMUM LIKELIHOOD ESTIMATION
NORMAL DENSITY FUNCTIONS
spellingShingle Snow
Ice and Permafrost
Statistics and Probability
(*STATISTICAL ANALYSIS
DECISION THEORY)
(*GLACIERS
MOTION)
MATHEMATICAL MODELS
STATISTICAL DISTRIBUTIONS
TRANSFORMATIONS(MATHEMATICS)
RANDOM VARIABLES
PROBABILITY
MATRICES(MATHEMATICS)
DEFORMATION
SIMULATION
MAXIMUM LIKELIHOOD ESTIMATION
NORMAL DENSITY FUNCTIONS
Gleser,Leon Jay
Watson,Geoffrey S.
Estimation of a Linear Transformation.
topic_facet Snow
Ice and Permafrost
Statistics and Probability
(*STATISTICAL ANALYSIS
DECISION THEORY)
(*GLACIERS
MOTION)
MATHEMATICAL MODELS
STATISTICAL DISTRIBUTIONS
TRANSFORMATIONS(MATHEMATICS)
RANDOM VARIABLES
PROBABILITY
MATRICES(MATHEMATICS)
DEFORMATION
SIMULATION
MAXIMUM LIKELIHOOD ESTIMATION
NORMAL DENSITY FUNCTIONS
description The problem which suggested this study arose in glaciology. Markers were placed in a glacier at points (xi sub c) and their positions, as measured by surveying techniques, were recorded at x sub i. Several years later a new survey was made by the same method yielding measurements y sub i of the true positions eta sub i. It was assumed that eta sub i = B(xi sub i) where the matrix B describing the deformation of the glacier is the object of interest. It seemed reasonable to assume a multivariate normal distribution for the errors on both occasions with a covariance matrix (sigma squared) E, with E known and so the problem can be transformed to make E = I. This paper deals with this problem where the vectors are p dimensional.
author2 PRINCETON UNIV N J DEPT OF STATISTICS
format Text
author Gleser,Leon Jay
Watson,Geoffrey S.
author_facet Gleser,Leon Jay
Watson,Geoffrey S.
author_sort Gleser,Leon Jay
title Estimation of a Linear Transformation.
title_short Estimation of a Linear Transformation.
title_full Estimation of a Linear Transformation.
title_fullStr Estimation of a Linear Transformation.
title_full_unstemmed Estimation of a Linear Transformation.
title_sort estimation of a linear transformation.
publishDate 1972
url http://www.dtic.mil/docs/citations/AD0747977
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0747977
long_lat ENVELOPE(-62.917,-62.917,-64.300,-64.300)
geographic Eta
geographic_facet Eta
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0747977
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766028008721743872