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Tech Note intro chapter and intro fig mods by JGP 8/8/18
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davegill authored Aug 20, 2018
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Expand Up @@ -556,7 +556,6 @@ Tao, W.-K,, J. Simpson, D. Baker, S. Braun, M.-D. Chou, B. Ferrier, D. Johnson,
Microphysics, radiation and surface processes in the Goddard Cumulus Ensemble (GCE) model.
{\em Meteor. and Atmos. Phys.}, {\bf 82}, 97--137.


\bibitem[Tao et al.(1989)]{tao89}%
Tao, W.-K., J. Simpson, and M. McCumber 1989: An ice-water saturation adjustment,
{\em Mon. Wea. Rev.}, {\bf 117}, 231--235.
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\chapter{Introduction}
\label{introduction_chap}
The Weather Research and Forecasting (WRF) model is
a numerical weather prediction (NWP) and atmospheric simulation
system designed for both
research and operational applications. WRF is supported
as a common tool for the university/research and operational
communities to promote closer ties between them and to
address the needs of both. The development of WRF has been a
multi-agency effort to build a next-generation mesoscale forecast model
and data assimilation system to advance the understanding and prediction
of mesoscale weather and accelerate the transfer of research
advances into operations. The WRF effort has been a collaborative one
among the National Center for Atmospheric Research's (NCAR)
Mesoscale and Microscale Meteorology (MMM) Division, the
National Oceanic and Atmospheric Administration's
(NOAA) National Centers for Environmental Prediction (NCEP) and
Earth System Research Laboratory (ESRL), the Department of Defense's
Air Force Weather Agency (AFWA) and Naval Research Laboratory (NRL),
the Center for Analysis and Prediction of Storms (CAPS) at the University
of Oklahoma, and the Federal Aviation Administration (FAA),
with the participation of university scientists.
The Weather Research and Forecasting (WRF) Model is
an atmospheric modeling system designed for both research and numerical
weather prediction. WRF is an open-source community model, and has been
adopted for research at universities and governmental laboratories,
for operational forecasting by governmental and private entities,
and for commercial applications by industry. WRF took shape in the latter
half of the 1990's with the ideas of building a system shared by research
and operations and of creating a next-generation NWP capability moving
past existing limitations. The new model would be a
common platform on which the broad research community
could develop capabilities that could transition to operations,
while the extra scrutiny of performance in operations
could guide and accelerate development. The WRF system was developed
through a partnership of the National
Center for Atmospheric Research (NCAR), the National Oceanic and Atmospheric
Administration (NOAA) (represented by the National Centers for Environmental
Prediction (NCEP) and, currently, the NOAA Earth System Research Laboratory (ESRL)),
the United States Air Force, the Naval Research Laboratory, the
University of Oklahoma, and the Federal Aviation Administration.
Since the mid-late 2000's, a top-down management structure
of the original partners has shifted to NCAR being responsible for system
oversight and support, with developments reflecting community input.

WRF reflects flexible, state-of-the-art, portable code that is
efficient in computing environments ranging from massively-parallel
supercomputers to laptops.
Its modular, single-source code can be configured for both
research and operational applications. Its spectrum of physics
and dynamics options reflects the experience and input of the
broad scientific community. Its WRF-Var variational data assimilation
system can ingest a host of observation types in pursuit of
optimal initial conditions, while its WRF-Chem
model provides a capability for air chemistry modeling.
WRF consists of flexible, modular, portable code that is
efficient in computing environments ranging from laptops to
massively-parallel supercomputers and is readily-configurable for
a variety of applications. Its extensive menu of physics
and dynamics options reflect wide community input
and make it a powerful NWP tool. WRF has a data assimilation system (WRFDA)
that offers a variety of DA approaches and can ingest a spectrum of
observation types. In addition, for earth system prediction needs
beyond basic weather forecasting, WRF supports a number of tailored capabilities.
These include WRF-Chem (atmospheric chemistry),
WRF-Hydro (hydrological modeling), WRF-Fire (wildland fire modeling),
and WRF-Solar (solar energy forecasting).

WRF is maintained and
supported as a community model to facilitate wide use internationally,
for research, operations, and teaching.
It is suitable for a broad span of applications across
scales ranging from large-eddy to global simulations. Such applications
include real-time NWP, data assimilation
development and studies, parameterized-physics research, regional
climate simulations, air quality modeling, atmosphere-ocean coupling, and
idealized simulations. As of this writing,
the number of registered WRF users exceeds 6000, and WRF is in
operational and research use around the world.
WRF is supported as a community model, facilitating system development
and broad use for research, operations, and education. It supports
atmospheric simulations across scales from large-eddy to global.
WRF's applications include real-time NWP, weather event and
atmospheric process studies, data assimilation development,
parameterized-physics development, regional climate simulation, air
quality modeling, atmosphere-ocean coupling, and idealized-atmosphere studies.

The principal components of the WRF system are depicted in Figure 1.1.
The WRF Software Framework (WSF) provides the infrastructure
that accommodates the dynamics solvers, physics packages
that interface with the solvers, programs for initialization,
WRF-Var, and WRF-Chem. There are two dynamics solvers in the WSF: the
Figure 1.1 depicts the principal components of the WRF system.
The WRF Software Framework (WSF) is the infrastructure
that contains the dynamics solvers, physics packages, utilities
for initialization, WRFDA, and integrated capabilities such as WRF-Chem.
Within the WSF there are two dynamics solver options: the
Advanced Research WRF (ARW) solver (originally referred to
as the Eulerian mass or $``$em" solver) developed primarily at NCAR, and
the NMM (Nonhydrostatic Mesoscale Model) solver developed at NCEP.
Community support for the former is provided by the MMM Division of NCAR
and that for the latter is provided by the Developmental Testbed Center (DTC).
The Mesoscale and Microscale Meteorology Laboratory of NCAR provides
support for the ARW, and oversees the WRF repository and releases.
This document describes the ARW (Version 4) and the system components
shared by both solvers.


%
Expand All @@ -65,38 +67,41 @@ \chapter{Introduction}
\caption{\label{figure:1}WRF system components.}
\end{figure}

\section {Advanced Research WRF}
\section {Advanced Research WRF (ARW)}

The ARW is the ARW dynamics solver together with other
components of the WRF system compatible with that solver and
used in producing a simulation. Thus, it is a subset of
the WRF modeling system that, in addition to the ARW solver,
The ARW is a configuration of the WRF system featuring
the ARW dynamics solver together with other compatible components
to produce a simulation. Thus,
it is a subset of the WRF system that, in addition to the specific solver,
encompasses physics schemes, numerics/dynamics options,
initialization routines, and a data assimilation package (WRF-Var).
The ARW solver shares the WSF with the NMM solver and all other
WRF components within the framework. Physics packages are
largely shared by both the ARW and NMM solvers, although specific
initialization routines, and a data assimilation package (WRFDA).
The ARW solver has the WSF in common with the NMM solver and all other
WRF components within the framework. While physics packages are
largely shared by both the ARW and NMM solvers, specific
compatibility varies with the schemes considered.
The association of a component of the WRF system with
the ARW subset does not preclude it from being a
component of WRF configurations involving the NMM solver.
Note that the association of a component of the WRF system with
the ARW does not preclude the component from being in
WRF configurations that use the NMM solver.
The following section highlights the major features of the
ARW, Version 4, and reflects elements of WRF Version 4,
which was first released in May 2018.
ARW Version 4, first released in May 2018.

This technical note focuses on the scientific and algorithmic
approaches in the ARW, including the solver, physics options,
initialization capabilities, boundary conditions, and grid-nesting techniques.
The WSF provides the software infrastructure.
WRF-Var, a component of the broader WRF system, was
adapted from MM5 3DVAR \citep{barker04} and is encompassed within the ARW.
While WRF-Chem is part of the ARW, Version 4, it is described
outside of this technical note. Those seeking details on
WRFDA, the data assimilation system for WRF, was
originally adapted from the MM5
(Pennsylvania State University--NCAR Mesoscale Model 5)
3DVAR (3-dimensional variational data assimilation) system
\citep{barker04} and is encompassed within the ARW.
While WRF-Chem and other tailored systems
(e.g., WRF-Hydro, etc.) use the ARW solver, they are
not covered by this technical note. Those seeking details on
WRF-Chem may consult \citet{Grelletal05} and
http://ruc.fsl.noaa.gov/wrf/WG11/status.htm .
For those seeking information on running the ARW system,
the {\wrf} User's Guide \citep{wang08}
has the details on its operation.
https://ruc.noaa.gov/wrf/wrf-chem/. Furthermore, for information on
actually running the ARW system, the ARW Version 4 Modeling System User's Guide
(http://www2.mmm.ucar.edu/wrf/users/docs/user_guide_V4/WRFUsersGuide.pdf)
covers model operation.

\section {Major Features of the ARW System, Version 4}

Expand All @@ -112,14 +117,14 @@ \chapter{Introduction}
%
\item{$\bullet$} {\em Prognostic Variables:}
Velocity components $u$ and $v$ in Cartesian coordinate, vertical velocity $w$,
perturbation potential temperature, perturbation geopotential,
perturbation moist potential temperature, perturbation geopotential,
and perturbation surface pressure of dry air.
Optionally, turbulent kinetic energy and any number of scalars
such as water vapor mixing ratio, rain/snow mixing ratio,
cloud water/ice mixing ratio, and chemical species and tracers.
%
\item{$\bullet$} {\em Vertical Coordinate:}
Terrain-following, hybrid sigma-pressure coordinate based on dry hydrostatic presure,
Terrain-following, mass-based, hybrid sigma-pressure vertical coordinate based on dry hydrostatic presure,
with vertical grid stretching permitted.
Top of the model is a constant pressure surface.
%
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\begin{description}
\setlength{\itemsep}{-5pt}
\item{$\bullet$} {\em Microphysics:} Schemes ranging from simplified
physics suitable for idealized studies to sophisticated mixed-phase
physics suitable for process studies and NWP.
physics suitable for idealized studies to mixed-phase, multi-moment, and aerosol-aware
approaches to support process studies and accurate NWP.
%
\item{$\bullet$} {\em Cumulus parameterizations:}
Adjustment and mass-flux schemes for mesoscale modeling.
Adjustment, mass-flux, and scale-aware schemes available.
%
\item{$\bullet$} {\em Surface physics:}
Multi-layer land surface models ranging from a simple thermal model to full
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\end{description}

\vskip 12pt
{\noindent\bf WRF-Var System}
{\noindent\bf WRFDA System}
\vskip 12pt

\begin{description}
\setlength{\itemsep}{-5pt}
\item{$\bullet$} WRF-Var merged into WRF software framework.
\item{$\bullet$} Data assimilation capability merged into WRF software framework.
%
\item{$\bullet$} Incremental formulation of the model-space cost function.
%
\item{$\bullet$} Quasi-Newton or conjugate gradient minimization algorithms.
%
\item{$\bullet$} Analysis increments on unstaggered Arakawa-A grid.
%
\item{$\bullet$} Representation of the horizontal component of background error ${\bf B}$ via
recursive filters (regional) or power spectra (global). The
\item{$\bullet$} Representation of the horizontal component of background
error ${\bf B}$ via recursive filters (regional) or power spectra (global). The
vertical component is applied through projection onto climatologically-averaged
eigenvectors of vertical error. Horizontal/vertical errors are
non-separable (horizontal scales vary with vertical eigenvector).
Expand All @@ -230,12 +235,12 @@ \chapter{Introduction}
%
\item{$\bullet$} Flexible choice of background error model and control variables.
%
\item{$\bullet$} Climatological background error covariances estimated via either the
NMC-method of averaged forecast differences or suitably averaged
\item{$\bullet$} Background error covariances estimated via either the
NMC-method of averaged forecast differences or suitably-averaged
ensemble perturbations.
%
\item{$\bullet$} Unified 3D-Var (4D-Var under development), global
and regional, multi-model capability.
\item{$\bullet$} 3DVAR, 4DVAR, hybrid ensemble-3DVAR approaches available.
Global and regional, multi-model DA capability.
%
\end{description}

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%
\item{$\bullet$}
Separation of scientific codes from parallelization and other
architecture-specific issues.
architecture-specific aspects.
%
\item{$\bullet$}
Input/Output Application Program Interface (API) enabling various external
Input/output Application Program Interface (API) enabling various external
packages to be installed with WRF, thus allowing WRF
to easily support various data formats.
%
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