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K. W. Oleson, G. B. Bonan, J. Feddema, and M. Vertenstein

= 64 simulations are performed for the morphological subset, and 2 6 = 64 and 2 8 = 256 simulations are performed for the radiative and thermal subsets, respectively. Simulations are conducted for 2–7 December 1993 (Mexico City) and 20–24 August 1992 (Vancouver). The observed fluxes for Mexico City and Vancouver are from Oke et al. (1999) and Voogt and Grimmond (2000) , respectively. The time frequency of the observed and modeled data is hourly, which permits analysis of the diurnal cycle

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K. W. Oleson, G. B. Bonan, J. Feddema, M. Vertenstein, and C. S. B. Grimmond

probable differences between canyon top and measurement height of up to 100 W m −2 in sensible heat flux were possible. A similar analysis for the Vancouver site would be required to determine the contribution of the advective component to differences between simulated and observed fluxes. However, a recent reanalysis at this site suggests that the sea-breeze categorization in MG02 may not be appropriate (A. Porson and C. S. B. Grimmond 2008, unpublished manuscript). This is also consistent with the

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