Advanced Research WRF (ARW) Technical Note - MMM - University ...

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On the coarse grid, the specified boundary condition applies to the horizontal wind components, potential temperature, φ ′ , µ ′ d , and water vapor. The lateral boundary file contains enough information to update the boundary zone values through the entire simulation period. The momentum fields are coupled with µd and the inverse map factor (both at the specific variable’s horizontal staggering location), and the other 3-dimensional fields are coupled with µd. The µ ′ d field is not coupled in the lateral boundary file. Vertical velocity has a zero gradient boundary condition applied in the specified zone (usually the outer-most row and column). Microphysical variables, except vapor, and all other scalars have flow-dependent boundary conditions applied in the specified zone. This boundary condition specifies zero on inflow and zero-gradient on outflow. Since these boundary conditions require only information from the interior of the grid, these variables are not in the specified boundary condition file. 42
Chapter 7 Nesting The ARW supports horizontal nesting that allows resolution to be focused over a region of interest by introducing an additional grid (or grids) into the simulation. In the current implementation, only horizontal refinement is available: there is no vertical nesting option. The nested grids are rectangular and are aligned with the parent (coarser) grid within which they are nested. Additionally, the nested grids allow any integer spatial (∆xcoarse/∆xfine) and temporal refinements of the parent grid. This nesting implementation is in many ways similar to the implementations in other mesoscale and cloudscale models (e.g. MM5, ARPS, COAMPS). The major improvement in the ARW’s nesting infrastruture compared with techniques used in other models is the ability to compute nested simulations efficiently on parallel distributed-memory computer systems, which includes support for moving nested grids. The WRF Software Framework, described in Michalakes et al. (2004), makes these advances possible. In this chapter we describe the various nesting options available in the ARW and the numerical coupling between the grids. 7.1 Overview 1-Way and 2-Way Grid Nesting Nested grid simulations can be produced using either 1-way nesting or 2-way nesting as outlined in Fig. 7.1. The 1-way and 2-way nesting options refer to how a coarse grid and the fine grid interact. In both the 1-way and 2-way simulation modes, the fine grid boundary conditions (i.e., the lateral boundaries) are interpolated from the coarse grid forecast. In a 1-way nest, this is the only information exchange between the grids (from coarse grid to fine grid). Hence, the name 1-way nesting. In the 2-way nest integration, the fine grid solution replaces the coarse grid solution for coarse grid points that lie inside the fine grid. This information exchange between the grids is now in both directions (coarse-to-fine and fine-to-coarse). Hence, the name 2-way nesting. The 1-way nest option may be run in one of two different methods. One option is to produce the nested simulation as two separate ARW simulations as described in the leftmost box in Fig. 7.1. In this mode, the coarse grid is integrated first. Output from the coarse grid integration is then processed to provide boundary conditions for the nested run (usually at a much lower temporal frequency than the coarse grid time step), and this is followed by the complete time integration of fine (nested) grid. Hence, this 1-way option is equivalent to 43
Page 1 and 2:
NCAR/TN-468+STR NCAR TECHNICAL NOTE
Page 3 and 4: Contents Acknowledgments ix 1 Intro
Page 5: 8.4.3 Rapid Update Cycle (RUC) Mode
Page 8 and 9: 9.2 Sketch of the role of Stage 0 c
Page 10 and 11: viii
Page 13 and 14: Chapter 1 Introduction The developm
Page 15 and 16: 1.2 Major Features of the ARW Syste
Page 17 and 18: Chapter 2 Governing Equations The A
Page 19 and 20: 2.3 Inclusion of Moisture In formul
Page 21 and 22: the earth. In this formulation we h
Page 23 and 24: Chapter 3 Model Discretization 3.1
Page 25 and 26: and lead to the acoustic time-step
Page 27 and 28: forward step, i.e., step (1) in Fig
Page 29 and 30: { Δy y u i-1/2,j+1 u i-1/2,j v i,j
Page 31 and 32: In the current version of the ARW,
Page 33 and 34: for Cr > 0, and (U t q) i+ 1 2 = U
Page 35 and 36: Chapter 4 Turbulent Mixing and Mode
Page 37 and 38: Symmetry sets the remaining tensor
Page 39 and 40: If ∆x is less than the user-speci
Page 41 and 42: 4.2 Filters for the Time-split RK3
Page 43: where γr is a user specified dampi
Page 46 and 47: exception of the baroclinic wave te
Page 48 and 49: STATIC DATA GRIB DATA SI SYSTEM GRI
Page 50 and 51: 5.2.3 Generating Lateral Boundary D
Page 52 and 53: a boundary on which the condition i
Page 56 and 57: 1-Way ARW WRF Simulation Two Consec
Page 58 and 59: V V V V U U U U U V V V V V V V
Page 60 and 61: V V V V U U U U U V V V V V V U
Page 62 and 63: coarse grid and fine grid is consis
Page 64 and 65: Table 8.1: Microphysics Options Sch
Page 66 and 67: and it is the water vapor and total
Page 68 and 69: 8.2.2 Betts-Miller-Janjic The Betts
Page 70 and 71: Table 8.3: Land Surface Options Sch
Page 72 and 73: Table 8.5: Radiation Options Scheme
Page 74 and 75: Table 8.6: Physics Interactions. Co
Page 77 and 78: Chapter 9 Variational Data Assimila
Page 79 and 80: supply the following: i) a default
Page 81 and 82: 9.2.4 First Guess at Appropriate Ti
Page 83 and 84: of its useful life. The development
Page 85 and 86: The second stage of gen be (gen be
Page 87: Appendix A Physical Constants The f
Page 90 and 91: Symbols Definition l0 minimum lengt
Page 92 and 93: Subscripts/Superscripts Definition
Page 94 and 95: NWP Numerical Weather Prediction OS
Page 96 and 97: Davies, H. C., and R. E. Turner, 19
Page 98 and 99: Lin, Y.-L., R. D. Farley, and H. D.
Page 100: Walko, R. L., W. R. Cotton, M. P. M
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