The Efficiency of Data Assimilation
dc.contributor.author | Nearing, Grey | |
dc.contributor.author | Yatheendradas, Soni | |
dc.contributor.author | Crow, Wade | |
dc.contributor.author | Zhan, Xiwu | |
dc.contributor.author | Liu, Jicheng | |
dc.contributor.author | Chen, Fan | |
dc.contributor.other | University of Alabama Tuscaloosa | |
dc.contributor.other | National Aeronautics & Space Administration (NASA) | |
dc.contributor.other | NASA Goddard Space Flight Center | |
dc.contributor.other | University of Maryland College Park | |
dc.contributor.other | United States Department of Agriculture (USDA) | |
dc.contributor.other | National Oceanic Atmospheric Admin (NOAA) - USA | |
dc.date.accessioned | 2023-09-28T19:35:40Z | |
dc.date.available | 2023-09-28T19:35:40Z | |
dc.date.issued | 2018 | |
dc.description.abstract | Data assimilation is the application of Bayes' theorem to condition the states of a dynamical systems model on observations. Any real-world application of Bayes' theorem is approximate, and therefore, we cannot expect that data assimilation will preserve all of the information available from models and observations. We outline a framework for measuring information in models, observations, and evaluation data in a way that allows us to quantify information loss during (necessarily imperfect) data assimilation. This facilitates quantitative analysis of trade-offs between improving (usually expensive) remote sensing observing systems versus improving data assimilation design and implementation. We demonstrate this methodology on a previously published application of the ensemble Kalman filter used to assimilate remote sensing soil moisture retrievals from Advanced Microwave Scattering Radiometer for Earth (AMSR-E) into the Noah land surface model. | en_US |
dc.format.medium | electronic | |
dc.format.mimetype | application/pdf | |
dc.identifier.citation | Nearing, G., Yatheendradas, S., Crow, W., Zhan, X., Liu, J., & Chen, F. (2018). The Efficiency of Data Assimilation. In Water Resources Research (Vol. 54, Issue 9, pp. 6374–6392). American Geophysical Union (AGU). https://doi.org/10.1029/2017wr020991 | |
dc.identifier.doi | 10.1029/2017WR020991 | |
dc.identifier.orcid | https://orcid.org/0000-0001-6178-7976 | |
dc.identifier.uri | https://ir.ua.edu/handle/123456789/11506 | |
dc.language | English | |
dc.language.iso | en_US | |
dc.publisher | American Geophysical Union | |
dc.subject | data assimilation | |
dc.subject | information theory | |
dc.subject | Bayesian efficiency | |
dc.subject | soil moisture | |
dc.subject | ATMOSPHERE TRANSFER SCHEME | |
dc.subject | LAND-SURFACE SCHEME | |
dc.subject | SOIL-MOISTURE | |
dc.subject | RUNOFF | |
dc.subject | PARAMETERIZATION | |
dc.subject | INFORMATION | |
dc.subject | RETRIEVALS | |
dc.subject | MODEL | |
dc.subject | Environmental Sciences | |
dc.subject | Limnology | |
dc.subject | Water Resources | |
dc.title | The Efficiency of Data Assimilation | en_US |
dc.type | Article | |
dc.type | text |
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