File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Simultaneous estimation of both soil moisture and model parameters using particle filtering method through the assimilation of microwave signal

TitleSimultaneous estimation of both soil moisture and model parameters using particle filtering method through the assimilation of microwave signal
Authors
Issue Date2009
Citation
Journal of Geophysical Research Atmospheres, 2009, v. 114, n. 15, article no. D15103 How to Cite?
AbstractSoil moisture is a very important variable in land surface processes. Both field moisture measurements and estimates from modeling have their limitations when being used to estimate soil moisture on a large spatial scale. Remote sensing is becoming a practical method to estimate soil moisture globally; however, the quality of current soil surface moisture products needs to be improved in order to meet practical requirements. Data assimilation (DA) is a promising approach to merge model dynamics and remote sensing observations, thus having the potential to estimate soil moisture more accurately. In this study, a data assimilation algorithm, which couples the particle filter and the kernel smoothing technique, is presented to estimate soil moisture and soil parameters from microwave signals. A simple hydrological model with a daily time step is utilized to reduce the computational burden in the process of data assimilation. An observation operator based on the ratio of two microwave brightness temperatures at different,' frequencies is designed to link surface soil moisture with remote sensing measurements, and a sensitivity analysis of this operator is also cond ucted. Additionally, a variant of particle filtering method is developed for the joint estimation of soil moisture and soil parameters such as texture and porosity. This assimilation scheme is validated against field moisture measurements at the CEOP/Mongolia experiment site and is found to estimate near-surface soil moisture very well. The retrieved soil texture still contains large uncertainties as the retrieved values cannot converge to fixed points or narrow ranges when using different initial soil texture values, but the retrieved soil porosity has relatively small uncertainties. Copyright 2009 by the American Geophysical Union.
Persistent Identifierhttp://hdl.handle.net/10722/321383
ISSN
2015 Impact Factor: 3.318
2020 SCImago Journal Rankings: 1.670
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorQin, Jun-
dc.contributor.authorLiang, Shunlin-
dc.contributor.authorYang, Kun-
dc.contributor.authorKaihotsu, Ichiro-
dc.contributor.authorLiu, Ronggao-
dc.contributor.authorKoike, Toshio-
dc.date.accessioned2022-11-03T02:18:33Z-
dc.date.available2022-11-03T02:18:33Z-
dc.date.issued2009-
dc.identifier.citationJournal of Geophysical Research Atmospheres, 2009, v. 114, n. 15, article no. D15103-
dc.identifier.issn0148-0227-
dc.identifier.urihttp://hdl.handle.net/10722/321383-
dc.description.abstractSoil moisture is a very important variable in land surface processes. Both field moisture measurements and estimates from modeling have their limitations when being used to estimate soil moisture on a large spatial scale. Remote sensing is becoming a practical method to estimate soil moisture globally; however, the quality of current soil surface moisture products needs to be improved in order to meet practical requirements. Data assimilation (DA) is a promising approach to merge model dynamics and remote sensing observations, thus having the potential to estimate soil moisture more accurately. In this study, a data assimilation algorithm, which couples the particle filter and the kernel smoothing technique, is presented to estimate soil moisture and soil parameters from microwave signals. A simple hydrological model with a daily time step is utilized to reduce the computational burden in the process of data assimilation. An observation operator based on the ratio of two microwave brightness temperatures at different,' frequencies is designed to link surface soil moisture with remote sensing measurements, and a sensitivity analysis of this operator is also cond ucted. Additionally, a variant of particle filtering method is developed for the joint estimation of soil moisture and soil parameters such as texture and porosity. This assimilation scheme is validated against field moisture measurements at the CEOP/Mongolia experiment site and is found to estimate near-surface soil moisture very well. The retrieved soil texture still contains large uncertainties as the retrieved values cannot converge to fixed points or narrow ranges when using different initial soil texture values, but the retrieved soil porosity has relatively small uncertainties. Copyright 2009 by the American Geophysical Union.-
dc.languageeng-
dc.relation.ispartofJournal of Geophysical Research Atmospheres-
dc.titleSimultaneous estimation of both soil moisture and model parameters using particle filtering method through the assimilation of microwave signal-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1029/2008JD011358-
dc.identifier.scopuseid_2-s2.0-70350074473-
dc.identifier.volume114-
dc.identifier.issue15-
dc.identifier.spagearticle no. D15103-
dc.identifier.epagearticle no. D15103-
dc.identifier.isiWOS:000268820600001-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats