The near-term objectives for this thrust area are:
A summary of the model output tasks is given in Task 11.2.1 for the Eta model,
Task 11.2.2 for the RFE model, and Task 11.2.3 for the MAPS model.
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ENHANCED OBSERVATIONS AND DATA PRODUCTS TASK SUMMARY
__________________________________________________________________________________________
TASK TITLE -- 11.2.1 Eta Model Output
OBJECTIVE -- To provide the model output products from the operational Eta model to the
GCIP Data Management System.
PRODUCT DESCRIPTION -- A series of analyzed and forecast products are produced each
day by the Eta model running in an operational mode at the NOAA/NCEP. During
operational production , NCEP significantly expands the number and type of fields produced
with emphasis on those needed by GCIP investigators to compute atmospheric and ground
surface energy budgets following the guidelines of the GCIP Implementation Plan , Vol I,
Section 5 (IGPO, 1993).
PROJECTED IMPROVEMENTS -- A description of the planned improvements to the Eta
model is given in Section 2 of Part I. Some GCIP specific improvements expected during the
next two to three years are:
SCHEDULE -- Operational product sent by NOAA/NCEP each month to the GCIP Model
Output Data Source Module.
GCIP USER AVAILABILITY --Three months after the end of the Eta product month.
RESOURCE SUPPORT -- Development support from NOAA GEWEX Program through the
NWS CORE Project for GCIP. The operational product is a contribution from the
NOAA/NCEP.
TASK LEADER -- K. Mitchell, NOAA/NCEP
GCIP PRA COORDINATION -- Coupled Modeling and Data Assimilation
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ENHANCED OBSERVATIONS AND DATA PRODUCTS TASK SUMMARY
__________________________________________________________________________________________
TASK TITLE -- 11.2.2 RFE Model Output
OBJECTIVE -- To provide the model output products from the operational RFE model to the
GCIP Data Management System
PRODUCT DESCRIPTION -- A series of analyzed and forecast products are produced each
day by the RFE model operated by the AES/CMC in Canada. The focus of the output from
the RFE model during the second year of the EOP will be on the MOLTS and the MORDS.
PROJECTED IMPROVEMENTS -- A description of the planned improvements to the RFE
model was given in Section 2 of Part I. Some specific improvements expected during the
next two to three years are:
SCHEDULE -- Operational product sent by the AES/CMC each month to the GCIP Model
Output Data Source Module.
GCIP USER AVAILABILITY -- Three months after the end of the RFE product month.
RESOURCE SUPPORT -- Development support from the Canadian GEWEX Program. The
operational product is a contribution from the AES/CMC
TASK LEADER -- H. Ritchie, AES/RPN
GCIP PRA COORDINATION -- Coupled Modeling and Data Assimilation
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ENHANCED OBSERVATIONS AND DATA PRODUCTS TASK SUMMARY
__________________________________________________________________________________________
TASK TITLE -- 11.2.3 MAPS Model Output
OBJECTIVE -- To provide the model output products from the experimental MAPS model to
the GCIP Data Management System
PRODUCT DESCRIPTION -- A series of analyzed and forecast products from the MAPS 3-
hr cycle are produced each day for the MAPS model running in an experimental mode at the
NOAA/FSL. During the second year of the EOP, the focus of the output from MAPS will be
on the MOLTS and the MORDS concentrating on the LSA-SW.
PROJECTED IMPROVEMENTS -- A description of the planned improvements to the MAPS
model was given in Section 2 of Part I. Some specific improvements expected during the
next two to three years are:
1) Addition and improvement of soil/vegetation model for improved flux
forecasts;
SCHEDULE -- Experimental products sent by the NOAA/FSL each month to the GCIP
Model Output Data Source Module.
GCIP USER AVAILABILITY -- Three months after the end of the MAPS product month.
RESOURCE SUPPORT -- Development support from the NOAA GEWEX Program.
TASK LEADER -- S. Benjamin; NOAA/FSL
GCIP WORKING GROUP COORDINATION -- Coupled Modeling and Data Assimilation
The output variables for the MOLTS are listed in Table 11-1. 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
period 1997 to 1999. 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 11-1.
1) Identifiers
Figure 11-1 Proposed geographical Distributions of 300 MOLTS locations.
A. Near-Surface Fields
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.
A description of the River Forecast Center (RFC) hydrological model and details of
the hydrological model outputs were provided in Table 1 and in Appendix B of the GCIP
Major Activities Plan for 1995, 1996 and Outlook for 1997 (IGPO, 1994c).
It is foreseen that these operational hydrological model outputs could be useful in
several types of GCIP research studies especially in the computation of water budgets.
However, this type of model output has not been archived in the past and there is no
experience or infrastructure to make such data readily available to research users. To remedy
this situation, the NOAA/OH is developing a pilot data set of Hydrology Model output to
provide to potential users of these new types of data for research as part of the NOAA Core
Project for GCIP.
-- Implement the multi-layer Oregon State University (OSU) soil/vegetation, now
executing for evaluation purposes in NMC's mesoscale Eta model, in the
Eta/EDAS system that is providing Eta output to GCIP (within the next year).
GCIP DATA SOURCE MODULE -- Model Output (Contact:R. Jenne, NCAR)
-- Implement the hourly National "Stage IV" precipitation analysis and assimilate 1-3
hourly precipitation into the EDAS
-- Implement the so-called "N+1" surface layer approach in the Eta/EDAS system,
providing an explicit forecast of u,v, T, Q at 10 meters above the ground.
-- Implement the Land-surface Data Assimilation System (LDAS) in which the Eta
model's land surface physics is executed independently from the Eta/EDAS in order to
utilize forcing from observed precipitation and satellite-derived surface radiation
-- Assimilate new satellite-based atmospheric moisture retrievals.
1) Modified surface layer treatments for better surface temperature, humidity, and
wind forecasts;
GCIP DATA SOURCE MODULE -- Model Output (Contact: R. Jenne)
2) explicit cloud water and cloud fraction prediction schemes;
3) improved radiation and convection parameterizations; and
4) increasing horizontal and vertical resolution throughout the three year period.
2) Explicit microphysics, with forecasts of cloud water, rain water, snow and ice
mixing ratios;
3) Addition of new data types, including radar reflectivity and radial winds,
satellite
radiances, Global Positioning System (GPS), and aircraft high-resolution
ascent/descent data;
4) Use of surface fields from NMC's LDAS, or implement MAPS-based LDAS, if
necessary.
5) Increased horizontal and vertical resolution.
GCIP DATA SOURCE MODULE -- Model Output (Contact: R. Jenne)
11.3 Model Location Time Series
Results from the GCIP Integrated Systems Test (GIST) and ESOP-95 indicate 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.
Table 11-1. Output Variables for the Model Location Time Series (MOLTS)
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Location ID
Valid Date/Time
Forecast Length
Latitude
Longitude
Location Elevation (in model)
2) Surface Variables
Mean sea level pressure
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
G round 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
pressure
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
11.4 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.
The specific model output variables in each of the four components are listed in Table
11-2.
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 11-2 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. 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.
Table 11-2. Output Variables for the Model Output Reduced Data Set
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1 - Mean sea level pressure
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
31 - Temperature (lowest model level)
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
41 - 1000 hpa height
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)
a - model terrain height
b - model roughness length
c - model max soil moisture capacity
d - model soil type
e - model vegetation type
11.5 Gridded Three-Dimensional Fields
The descriptions given in Section 11.3 on MOLTS and
Section 11.4 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 means 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.
11.6 Hydrological Model Output
The NOAA/OH is collecting and archiving operational model output from the
National Weather Service River Forecast System (NWSRFS) in the Mississippi River basin.
The NWSRFS is a system which integrates a variety of hydrological models into a
comprehensive river forecast system. It includes models of runoff-generating processes and
runoff and streamflow routing. The NWSRFS data being archived by NOAA/OH include
values every six hours of all of the available elements of the daily water budget:
precipitation, runoff (surface runoff and baseflow), evaporation and soil moisture storage for
individual soil moisture accounting (SMA) areas and the downstream routed streamflows.