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<div class="csl-entry">Zwieback, S. (2011). <i>Probabilistic fusion of Ku and C band scatterometer data for determining the freeze/thaw state</i> [Diploma Thesis, Technische Universität Wien]. reposiTUm. https://resolver.obvsg.at/urn:nbn:at:at-ubtuw:1-41872</div>
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The transition of the landscape from frozen to non-frozen conditions has far-reaching consequences on numerous geo- and biophysical processes such as plant growth and the hydrologic cycle.<br />Microwave remote sensing has been shown to be an apt tool for monitoring the landscape freeze/thaw state. As the measured signal sigma0 is sensitive to different factors at different radar frequencies, the combination of distinct data sources can potentially lead to improved results.<br />In light of this observation, a novel sensor fusion algorithm is proposed -- it estimates the F/T state based on scatterometer data: SeaWinds on QuikScat in Ku band and ASCAT on MetOp in C band. In addition, a widely used backscatter model for snow packs is extended, whose purpose is twofold: firstly, it can give insight into the dependence of sigma0 on various factors and secondly, it facilitates the parameterization of the aforementioned sensor fusion model.<br />The sensor fusion approach is based on a probabilistic model, an adaptation of the well-known Hidden Markov model (HMM). The F/T state is assumed to be a Markov chain, whose value is not directly observable. At each epoch, however, its current state influences the measurements: sigma0 at both frequency bands. The simple structure assures that inference can be done efficiently, e.g. the calculation of the probability of the state on a given day. The algorithm does not use training data; the parameters are estimated for each time series in an unsupervised fashion. This is achieved by maximizing the marginal likelihood in the framework of the Expectation Maximization algorithm.<br />The algorithm is analyzed and tested in a study area in Russia and northern China, which encompasses the region of 120 - 130 E and 50 - 75 N. The time series of the probability of the state are validated with in-situ snow and temperature data as well as global climate models. In general, the accuracy exceeds 90%, but the algorithm can fail in agriculturally used land (fields, pastures) and bare rock outcrops in mountainous regions. On a more qualitative level, the study affirms the importance of using two distinct frequencies, as particularly dry snow, vegetation and the freezing of the soil water manifest themselves differently at Ku and C band.<br />
en
dc.language
English
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dc.language.iso
en
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dc.rights.uri
http://rightsstatements.org/vocab/InC/1.0/
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dc.subject
Remote Sensing
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dc.subject
Scatterometer
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dc.subject
Freeze/Thaw State
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dc.subject
Hidden Markov model
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dc.subject
Graphical Model
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dc.subject
Expectation Maximization algorithm
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dc.subject
Backscatter modelling
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dc.subject
Fernerkundung
de
dc.subject
Scatterometer
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dc.subject
Frier/Tau Zustand
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dc.subject
Hidden Markov Model
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dc.subject
Graphisches Modell
de
dc.subject
Expectation Maximization Algorithmus
de
dc.subject
Rückstreumodellierung
de
dc.title
Probabilistic fusion of Ku and C band scatterometer data for determining the freeze/thaw state
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dc.type
Thesis
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dc.type
Hochschulschrift
de
dc.rights.license
In Copyright
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dc.rights.license
Urheberrechtsschutz
de
dc.contributor.affiliation
TU Wien, Österreich
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dc.rights.holder
Simon Zwieback
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tuw.version
vor
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tuw.thesisinformation
Technische Universität Wien
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dc.contributor.assistant
Bartsch, Annett
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dc.contributor.assistant
Melzer, Thomas
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tuw.publication.orgunit
E120 - Institut für Photogrammetrie und Fernerkundung