(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 2000.
(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 details of the regional model output to satisfy the first objective above is given in the remainder of this Appendix.
(1) One-dimensional vertical profile and surface time series at selected locations referred to as Model Location Time Series (MOLTS)Each model output type is described in the following sections.(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.
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.
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.
1) Identifiers
Location ID2) Surface Variables
Valid Date/Time
Forecast Length
Latitude
Longitude
Location Elevation (in model)
Mean sea level pressure3) Atmospheric variables at each model vertical level
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
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
Figure B-1 Distribution of 300 MOLTS
Locations
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.
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. Near-Surface Fields
1 - Mean sea level pressureB. Lowest level Atmospheric 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)
C. Upper 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)
41 - 1000 hpa heightD. Meta Data Fixed Fields (as one-time companion file to MORDS)
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)
a - model terrain height
b - model roughness length
c - model max soil moisture capacity
d - model soil type
e - model vegetation type