APPENDIX B
REGIONAL MESOSCALE MODEL OUTPUT PRODUCTS
One of the principal functions of the regional mesoscale models, as was noted in Section 2, is to produce the model assimilated and forecast output products for GCIP research, especially for energy and water budget studies. The production of such data sets was an important part of the GCIP Implementation Plan (IGPO 1993). A major thrust area for the production of such data sets from three different regional models was initiated in 1995 with the following objectives:
(i) To produce model assimilated and forecast data
products for GCIP investigators with an emphasis on those variables needed to produce energy and water
budgets over a continental scale with detailed emphasis
in 1997 on the LSA-SW and the LSA-NC and beginning the
application of such detailed emphasis capability to the
LSA-E during 1998, and to the LSA-NW during 1999.
(ii) To produce a quantitative assessment of the accuracy
and reliability of the model assimilated and forecast
data products for applications to energy and water budgets.
(iii) To conduct the research needed to improve the
time and space distribution along with the
accuracy and reliability of the model assimilated and forecast data products.
The activities relevant to the second and third objective above
were described in Section 2. The details of the regional model
output to satisfy the first objective above is given in the remainder of this Appendix.
B.1 Regional Mesoscale Model Output
The list of model output fields needed by GCIP researchers
was given in Table 3, Volume I of the GCIP Implementation Plan
(IGPO 1993). From the beginning of GCIP, it has been the intent
to acquire model output from several different models of varying
resolution, physics and data assimilation systems. The large
volume of data produced by the current generation of atmospheric
models has forced a number of compromises in order to achieve a
tractable data handling solution for model output data. The data
volume is further enlarged by the GCIP need to enhance the
traditional model output to include additional fields needed by
researchers to perform meaningful studies of the water and energy
cycles. The near-term GCIP needs for model output data will be
met by concentrating on three regional mesoscale models:
The model output is divided into three types:
Each model output type is described in the following sections.
B.2 Model Location Time Series
Results from the GCIP Integrated Systems Test (GIST) in 1994
and ESOP-95 demonstrated that the vertical and surface time
series at selected points is a very useful type of output for a
number of applications. Indeed, some energy and water budget
computations are making use of this type of model output data.
GCIP labels this type of model output as Model Location Time
Series (MOLTS) which is produced as an enhanced output containing
a complete set of the "surface" type of state and flux data
needed by GCIP in addition to the basic atmospheric data which
operational centers produce for normal monitoring use and other
applications.
The output variables for the MOLTS are listed in Table B-1.
The variables listed under 2) Surface Variables and 3)
Atmospheric Variables are considered a"fundamental" list. The
MOLTS list from a specific model may add other variables
depending on choice of physics package or other non-GCIP user
requirements. Some examples for the surface variables could
include turbulent kinetic energy and other diabatic heating and
moistening rates, such as those due to vertical and horizontal
diffusion. Some examples of the non-profile variables could
include canopy water content, boundary layer depth, convective
storm stability indices, precipitation type (frozen?), etc.
An assessment of the MOLTS requirements for GCIP, MAGS and
other investigators indicates that a maximum number of 300
locations will satisfy these requirements during the EOP. The
specific number could be less than this maximum number depending
on resources available to the data producers and the changes in
requirements for GCIP during the Enhanced Seasonal Observing
Periods and outside of these periods. GCIP will provide inputs
to the requirements as part of its annual update of the GCIP
Major Activities Plan. The distribution of 300 MOLTS locations is
shown in Figure B-1.
(1) One-dimensional vertical profile and surface time
series at selected locations referred to as Model Location Time Series (MOLTS)
(2) Gridded two-dimensional fields, especially ground
surface state fields, ground surface flux fields,
top-of-the-atmosphere (TOA) flux fields, and
atmospheric fields referred to as Model Output Reduced Data Sets (MORDS)
(3) Gridded three-dimensional atmospheric fields
containing all of the atmospheric variables produced by the models.
Table B-1 Output Variables for the Model Location Time Series (MOLTS) |
1) Identifiers
Valid Date/Time Forecast Length Latitude Longitude Location Elevation (in model) |
2) Surface Variables
Ground surface pressure Total precipitation in past hour Convective precipitation in past hour U wind component at 10 m V wind component at 10 m 2-meter specific humidity 2-meter temperature Skin temperature Soil temperature (all soil layers) Soil moisture (all soil layers) Latent heat flux (surface evaporation) Sensible heat flux Ground heat flux Surface momentum flux Snow phase-change heat flux Snow depth (water equivalent) Snow melt Surface runoff Sub-surface runoff Surface downward short-wave radiation flux Surface upward short-wave radiation flux (gives albedo) Surface downward longwave radiation flux Surface upward longwave radiation flux Top-of-atmosphere net longwave radiative flux Top-of-atmosphere net shortwave radiative flux Top-of-atmosphere pressure for above fluxes |
3) Atmospheric variables at each model vertical level
geopotential height temperature specific humidity U wind component V wind component Omega (vertical motion -- Dp/Dt) convective precipitation latent heating rate stable precipitation latent heating rate shortwave radiation latent heating rate longwave radiation latent heating rate cloud water and/or cloud fraction |
Figure B-1 Geographical Distribution of 300 MOLTS Locations.
B.3 Model Output Reduced Data Set
An analysis of the different GCIP requirements for the
gridded two- and three-dimensional fields indicates that most of
the requirements can be met by a selected set of two-dimensional
gridded fields. [NOTE: Some of the requirements for three-dimensional
fields can be met with the MOLTS , e.g. by placing
the locations around the boundaries of a river basin to do budget
studies.] Some of the other 3-D field requirements can be met by
a vertical integration through the atmosphere, e.g. vertically
integrated atmospheric moisture divergence needed to calculated
water budgets. GCIP will make use of this concentration of
requirements to further the tractability of the model output data
handling problem. A Model Output Reduced Data Set (MORDS) will
continue to be produced as two-dimensional fields with the
expectation that the MORDS can meet most of the GCIP requirements
at a significantly reduced data volume over that needed to
provide the information as three-dimensional fields. GCIP is
proposing a total of 60 output variables for MORDS separated into
the following four components:
A. Near-surface fields which will include all the sub-surface
and surface land characteristics and hydrology variables plus the surface
meteorological variables including wind components at 10 meters.
B. Lowest-level atmospheric fields which includes the
lowest model level and the mean value in a 30 hpa layer above the surface.
C. Upper atmosphere fields at a few standard levels plus
the tropopause height and the top-of-atmosphere radiation as a time average.
D. Metadata fixed fields as one-time companion file to the MORDS.
The specific model output variables in each of the four
components are listed in Table B-2.
Output from the regional mesoscale models on the AWIPS 212
Lambert Conformal Map base at a 40 km resolution constitutes
about 30 Kilobytes per field for each output step. The 55 fields
from the list of variables shown in Table B-2 will produce about
1.5 Mb for a single forecast or analysis valid time. The MORDS
output of analysis, assimilation, and forecast fields for both
0000 UT and 1200 UT cycles comes to a daily total of about 40 Mb
per day from each of the regional mesoscale models or about 1.2
Gb per month. This is significantly less than the data volume
generated from each of the regional models output in three-dimensional fields.
B.4 Gridded Three-Dimensional Fields
The descriptions given in Section B.2
on MOLTS and Section B.3
on MORDS are aimed primarily at reducing the need to handle
the full three-dimensional output fields from each of the
regional models. This should make the model output more readily
accessible for the GCIP investigators. It is also, in part,
needed due to the limitations in the data handling capacity for
the full model output by the Model Output Data Source Module in
the GCIP Data Management and Service System. These limitations
mean it will be possible to collect the three-dimensional fields
at this location for the Eta model only. GCIP encourages the
producers of the three-dimensional fields for the other two
regional models to store them locally to the extent possible.
The description given above on how GCIP plans to meet the
model output data requirements within the data handling
limitations experienced is applicable for the near-term
requirements. It is expected that these requirements will evolve
as the land physics packages of these models demonstrate their
utility. GCIP will reevaluate this area on an annual basis as
part of preparing updates to the GCIP Major Activities Plan.
Table B-2 Output Variables for the Model Output Reduced Data Set |
A. Near-Surface Fields
2 - Surface pressure at 2 meters 3 - Temperature at 2 meters 4 - Specific humidity at 2 meters 5 - U component wind speed at 10 meters 6 - V component wind speed at 10 meters 7 - Surface latent heat flux (time avg) 8 - Surface sensible heat flux (time avg) 9 - Ground heat flux (time avg) 10 - Snow phase change heat flux (time avg) 11 - Surface momentum flux (time avg) 12 - Vertically integrated moisture convergence (time avg) 13 - Vertically integrated energy convergence (time avg) 14 - Total precipitation (time accumulated) 15 - Convective precipitation (time accumulated) 16 - Surface runoff (time accumulated) 17 - Subsurface runoff (time accumulated) 18 - Snow melt (time accumulated) 19 - Snow depth (water equivalent) 20 - Total soil moisture (within total active soil column) 21 - Canopy water content (if part of surface physics) 22 - Surface skin temperature 23 - Soil temperature in top soil layer 24 - Surface downward shortwave radiation (time avg) 25 - Surface upward shortwave radiation (time avg) 26 - Surface downward longwave radiation (time avg) 27 - Surface upward longwave radiation (time avg) 28 - Total cloud fraction (time avg) 29 - Total column water vapor 30 - Convective Available Potential Energy (CAPE) |
B. Lowest level Atmospheric Fields
32 - Specific humidity (lowest model level) 33 - U component wind speed (lowest model level) 34 - V component wind speed (lowest model level) 35 - Pressure (lowest model level) 36 - Geopotential (lowest model level) 37 - Temperature (mean in 30 hpa layer above ground) 38 - Specific humidity (mean in 30 hpa layer above ground) 39 - U component wind speed (mean in 30 hpa layer above ground) 40 - V component wind speed (mean in 30 hpa layer above ground) |
C. Upper Atmospheric Fields
42 - 700 hpa vertical motion (omega -- Dp/Dt) 43 - 850 hpa height 44 - 850 hpa temperature 45 - 850 hpa specific humidity 46 - 850 hpa U component wind speed 47 - 850 hpa V component wind speed 48 - 500 hpa height 49 - 500 hpa absolute vorticity 50 - 250 hpa height 51 - 250 hpa U component wind speed 52 - 250 hpa V component wind speed 53 - Tropopause height (or pressure) 54 - Top-of-atmosphere net longwave radiation (time avg) 55 - Top-of-atmosphere net shortwave radiation (time avg) |
D. Meta Data Fixed Fields (as one-time companion file to MORDS)
b - model roughness length c - model max soil moisture capacity d - model soil type e - model vegetation type |