11.1
Numerical Investigation of the Cause of Shallow Summertime Mixing Depths in the San Joaquin Valley
Nelson Seaman, Penn State Univ., University Park, PA; and K. Alapaty
During the summer, especially during episodes having high concentrations of ozone, mixing depths in the San Joaquin Valley (SJV) of CA are known to be quite low, compared to other semi-arid regions of the western U.S. Shallow mixing depths tend to concentrate pollutants near the surface and reduce ventilation. Thus, understanding the causes of shallow mixing depths over the valley is important for explaining air quality in this region. While it is common during this season for daytime surface temperatures to exceed 35 C and for mixed layers to exceed 3 km in semi-arid areas, the mixing depths in the SJV are often only 500-800 m despite similar surface temperatures. Also, the inversion that caps the SJV mixed layer is often quite weak, despite very strong capping inversions typically found over the Pacific Ocean a few hundred kilometers away. Prior numerical modeling studies have indicated that models often have difficulty simulating the very shallow mixing depths in the SJV. Therefore, a study was conducted to understand the origin of the shallow SJV mixing depths and to reproduce them in a 3-D mesoscale numerical model.
Using the non-hydrostatic Penn State/National Center for Atmospheric Research mesoscale model (MM5), a series of experiments was conducted to learn the influence on SJV mixing depths due to several factors: model physics, numerics and data assimilation. All experiments covered the polluted episode from 2 - 6 August 1990 during the SARMAP study and used model domains having 36-km, 12-km and 4-km meshes. For the physics, the non-local Blackadar scheme and a 1.5-order turbulent-kinetic-energy (TKE) predicting boundary layer scheme were used alternatively. For the numerics, experiments were run with and without a 108-km outer mesh, with different sizes of 4-km domain, and with either 32 or 62 vertical layers. For the data-assimilation tests, runs were made with and without careful detailed initialization of the shallow marine boundary layer, and with alternative four-dimensional data assimilation (FDDA) strategies used on the 36-km and 12-km domains (no FDDA was used on the 4-km domain). Comparisons of the 4-km solutions revealed that the choice of the type of boundary-layer scheme and the vertical resolution were the two most important factors needed to correctly simulate the shallow mixing depths in the SJV. The unusually shallow boundary layer of the valley appears to result primarily from subsidence in the return branch of the local mountain-valley circulations of this region. When air-stagnation occurs, subsided air from a prior day may remain over the valley, so that the next day's circulation causes further subsidence heating. Consequently, the afternoon mixing depths were found to decline steadily during the four-day simulation period.
Session 11, Transport and dispersion in complex terrain: Part II (Parallel with Session 12)
Wednesday, 12 January 2000, 1:30 PM-2:30 PM
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