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Erin B. Munsell, Fuqing Zhang, Jason A. Sippel, Scott A. Braun, and Yonghui Weng

cycling was performed every 3 h until the dissipation of Edouard. As in all forecasts produced by the PSU WRF–EnKF system, ensemble initial and lateral boundary conditions were generated by adding perturbations derived from the background error covariance of the WRF variational data assimilation system ( Barker et al. 2004 ) to the pressure, temperature, moisture, and horizontal wind fields of the initial and boundary conditions. The EnKF analysis perturbations from 1200 UTC 11 September were used to

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E. P. Nowottnick, P. R. Colarco, S. A. Braun, D. O. Barahona, A. da Silva, D. L. Hlavka, M. J. McGill, and J. R. Spackman

moisture condensation on the instrument window and telescope, as well as attenuation by clouds during the first four legs of the flight over Nadine and the SAL; therefore, only the components of the flight where dust was observed and CPL was not affected by lens condensation are shown. Despite these limitations, MODIS Terra observed a broad region of dust to the east of Nadine, which was also observed by CPL on the latter legs of the flight. Figure 1b shows the 550-nm total AOT from the GEOS-5 FP

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