Development of the WRF-CO2 4D-Var assimilation system v1.0
Regional atmospheric CO<sub>2</sub> inversions commonly use Lagrangian particle trajectory model simulations to calculate the required influence function, which quantifies the sensitivity of a receptor to flux sources. In this paper, an adjoint-based four-dimensional variational (4D-V...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-05-01
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Series: | Geoscientific Model Development |
Online Access: | https://www.geosci-model-dev.net/11/1725/2018/gmd-11-1725-2018.pdf |
Summary: | Regional atmospheric CO<sub>2</sub> inversions commonly use Lagrangian
particle trajectory model simulations to calculate the required influence
function, which quantifies the sensitivity of a receptor to flux sources. In
this paper, an adjoint-based four-dimensional variational (4D-Var)
assimilation system, WRF-CO2 4D-Var, is developed to provide an alternative
approach. This system is developed based on the Weather Research and
Forecasting (WRF) modeling system, including the system coupled to chemistry
(WRF-Chem), with tangent linear and adjoint codes (WRFPLUS), and with data
assimilation (WRFDA), all in version 3.6. In WRF-CO2 4D-Var, CO<sub>2</sub> is modeled as a tracer and its
feedback to meteorology is ignored. This configuration allows most WRF
physical parameterizations to be used in the assimilation system without
incurring a large amount of code development. WRF-CO2 4D-Var solves for the
optimized CO<sub>2</sub> flux scaling factors in a Bayesian framework. Two
variational optimization schemes are implemented for the system: the first
uses the limited memory Broyden–Fletcher–Goldfarb–Shanno (BFGS)
minimization algorithm (L-BFGS-B) and the second uses the Lanczos conjugate
gradient (CG) in an incremental approach. WRFPLUS forward, tangent linear,
and adjoint models are modified to include the physical and dynamical
processes involved in the atmospheric transport of CO<sub>2</sub>. The system is
tested by simulations over a domain covering the continental United States at
48 km × 48 km grid spacing. The accuracy of the tangent linear and
adjoint models is assessed by comparing against finite difference
sensitivity. The system's effectiveness for CO<sub>2</sub> inverse modeling is tested
using pseudo-observation data. The results of the sensitivity and inverse
modeling tests demonstrate the potential usefulness of WRF-CO2 4D-Var for
regional CO<sub>2</sub> inversions. |
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ISSN: | 1991-959X 1991-9603 |