Development of a regional climate model for US midwest applications. Part I: Sensitivity to buffer zone treatment

Citation
Xz. Liang et al., Development of a regional climate model for US midwest applications. Part I: Sensitivity to buffer zone treatment, J CLIMATE, 14(23), 2001, pp. 4363-4378
Citations number
52
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF CLIMATE
ISSN journal
08948755 → ACNP
Volume
14
Issue
23
Year of publication
2001
Pages
4363 - 4378
Database
ISI
SICI code
0894-8755(2001)14:23<4363:DOARCM>2.0.ZU;2-O
Abstract
A regional climate model (RCM) is being developed for U.S. Midwest applicat ions on the basis of the newly released Pennsylvania State University-NCAR Fifth-Generation Mesoscale Model (MM5), version 3.3. This study determines the optimal RCM domain and effective data assimilation technique to accurat ely integrate lateral boundary conditions (LBCs) across the buffer zones. T he LBCs are constructed from both the NCEP-NCAR and ECMWF reanalyses to dep ict forcing uncertainties. The RCM domain was chosen to correctly represent the governing physical processes while minimizing LBC errors. Sensitivity experiments are conducted for the Midwest 1993 summer flood to investigate buffer zone treatment impacts on RCM performance. The results demonstrate the superiority of the buffer zone treatment that c onsists of the physically based domain choice and revised assimilation tech nique. Given this treatment, the RCM realistically simulates both temporal variations and spatial distributions in the major flood area (MFA). This su ccess is identified with the accurate representation of both the midlatitud e upper-level jet stream and Great Plains low-level jet (LLJ). The RCM repr oduces different climate regimes, where observed rainfall was identified wi th the periodic (5 day) passage of midlatitude cyclones in June and persist ent synoptic circulations in July. The model also correctly simulates the M FA rainfall diurnal cycle (with the peak amount at 0900 UTC), which follows the LLJ cycle by approximately 3 h. On the other hand, RCM performance is substantially reduced when the southern buffer zone extends to the Tropics, where large forcing errors exist. In particular, the RCM generates a weake r LLJ and, as a consequence, a decreased amount and delayed diurnal cycle o f the MFA rainfall. In addition, the MM5 default LBC data assimilation tech nique produces considerable model biases, whereas the revised technique imp roves overall RCM performance and reduces sensitivity to domain size.