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Air Quality Response Modeling for Decision Support

Chemical Data Assimilation—An Overview

Computational Science Laboratory, Department of Computer Science, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061-0106, USA
NOAA/OAR/ARL, Silver Spring Metro Center #3, Rm. 3437, 1315 East West Highway, Silver Spring, MD 20910, USA
Author to whom correspondence should be addressed.
The paper is dedicated to the memory of Dr. Daewon Byun, whose work remains a lasting legacy to the field of air quality modeling and simulation.
Atmosphere 2011, 2(3), 426-463;
Received: 7 June 2011 / Revised: 9 August 2011 / Accepted: 19 August 2011 / Published: 29 August 2011
(This article belongs to the Special Issue Air Pollution Modeling: Reviews of Science Process Algorithms)
Chemical data assimilation is the process by which models use measurements to produce an optimal representation of the chemical composition of the atmosphere. Leveraging advances in algorithms and increases in the available computational power, the integration of numerical predictions and observations has started to play an important role in air quality modeling. This paper gives an overview of several methodologies used in chemical data assimilation. We discuss the Bayesian framework for developing data assimilation systems, the suboptimal and the ensemble Kalman filter approaches, the optimal interpolation (OI), and the three and four dimensional variational methods. Examples of assimilation real observations with CMAQ model are presented. View Full-Text
Keywords: chemical transport modeling; data assimilation; Kalman filter; variational methods chemical transport modeling; data assimilation; Kalman filter; variational methods
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MDPI and ACS Style

Sandu, A.; Chai, T. Chemical Data Assimilation—An Overview. Atmosphere 2011, 2, 426-463.

AMA Style

Sandu A, Chai T. Chemical Data Assimilation—An Overview. Atmosphere. 2011; 2(3):426-463.

Chicago/Turabian Style

Sandu, Adrian, and Tianfeng Chai. 2011. "Chemical Data Assimilation—An Overview" Atmosphere 2, no. 3: 426-463.

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