The impact of lateral boundary data errors on the simulated climate of a nested regional climate model |
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| Authors: | Emilia Paula Diaconescu René Laprise Laxmi Sushama |
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| Institution: | (1) Département des Sciences de la Terre et de l’Atmosphère, UQAM - Ouranos, 550, rue Sherbrooke Ouest, 19e étage, Tour Ouest, Montréal, QC, Canada, H3A 1B9 |
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| Abstract: | In this study, we investigate the response of a Regional Climate Model (RCM) to errors in the atmospheric data used as lateral
boundary conditions (LBCs) using a perfect-model framework nick-named the “Big-Brother Experiment” (BBE). The BBE has been
designed to evaluate the errors due to the nesting process excluding other model errors. First, a high-resolution (45 km)
RCM simulation is made over a large domain. This simulation, called the Perfect Big Brother (PBB), is driven by the National
Centres for Environmental Prediction (NCEP) reanalyses; it serves as reference virtual-reality climate to which other RCM
runs will be compared. Next, errors of adjustable magnitude are introduced by performing RCM simulations with increasingly
larger domains at lower horizontal resolution (90 km mesh). Such simulations with errors typical of today’s Coupled General
Circulation Models (CGCM) are called the Imperfect Big-Brother (IBB) simulations. After removing small scales in order to
achieve low-resolution typical of today’s CGCMs, they are used as LBCs for driving smaller domain high-resolution RCM runs;
these small-domain high-resolution simulations are called Little-Brother (LB) simulations. The difference between the climate
statistics of the IBB and those of PBB simulations mimic errors of the driving model. The comparison of climate statistics
of the LB to those of the PBB provides an estimate of the errors resulting solely from nesting with imperfect LBCs. The simulations
are performed over the East Coast of North America using the Canadian RCM, for five consecutive February months (from 1990
to 1994). It is found that the errors contained in the large scales of the IBB driving data are transmitted to and reproduced
with little changes by the LB. In general, the LB restores a great part of the IBB small-scale errors, even if they do not
take part in the nesting process. The small scales are seen to improve slightly in regions with important orographic forcing
due to the finer resolution of the RCM. However, when the large scales of the driving model have errors, the small scales
developed by the LB have errors as well, suggesting that the large scales precondition the small scales. In order to obtain
correct small scales, it is necessary to provide the accurate large-scale circulation at the lateral boundary of the RCM. |
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