The Global Energy and Water Cycle Experiment (GEWEX) Continental-scale
International Project (GCIP) was established to improve scientific understanding and to model
on a continental scale the coupling between the atmosphere and the land surface for climate
prediction purposes. Predicting variations in the earth's climate requires improved
understanding of interaction between the atmosphere and land surface. Generally, the
sensitivity of the earth's climate is determined by the energetic processes of the fast climate
system". The fast climate processes are manifested by clouds, insolation, precipitation, soil
characteristics (moisture), vegetation, state of water resources, and the coupling processes
between land surface moisture in (1) the partitioning of energy flux between latent and
sensible heat, (2) interpreting precipitation variability; and (3) providing knowledge on
infiltration and runoff, and its impact on energy and water budgets. The GCIP activities are
focused on the Mississippi River basin (see Figure 1-1) to take advantage of the existing
meteorological and hydrological networks that are being upgraded with new Doppler radars,
wind profilers, and automatic weather stations. The operational or enhanced observing period
(EOP) of GCIP began in October 1995 and is planned to continue for five years.
Figure 1-1 The Mississippi River basin, the focus of GCIP activities.
A recently completed review by the NAS/NRC GEWEX Panel recommended
that GCIP should focus more on the seasonal to interannual prediction problem and
recommended the following scientific mission for GCIP:
"To demonstrate skill in predicting changes in water resources on time scales up to
seasonal, annual, and interannual as an integral part of the climate prediction system."
The Panel further recommended some restatement of the original science objectives to more
clearly focus on the seasonal to interannual prediction problem and to add an objective
pertaining to data management. GCIP has adopted these modified objectives to better reflect
the emphasis of the Project which has evolved over the past five years since the completion
of the GCIP Science Plan (World Meteorological Organization, 1992). The GCIP objectives
are:
2) Develop and evaluate coupled hydrologic/atmospheric models at resolutions
appropriate to large-scale continental basins.
3) Develop and evaluate atmospheric, land, and coupled data assimilation schemes
that incorporate both remote and in-situ observations.
4) Improve the utility of hydrologic predictions for water resources management
up to seasonal and interannual time scales.
5) Provide access to comprehensive in-situ, remote sensing and model output data
sets for use in GCIP research and as a benchmark for future studies.
The GCIP Implementation Plan, comprising three volumes, was completed in 1993
and 1994. Volume I of the GCIP Implementation Plan (IGPO, 1993) is the overall planning
document for the Project. It addresses the organizational framework for GCIP, the
observational and database needs, and the upgrades to be made to existing operational
analysis and prediction streams that produce routine four-dimensional data assimilation
(4DDA) analyses for the GCIP and global domains. Volume II (IGPO, 1994a) examines the
elements of a GCIP research program needed to assist the research community in addressing
the specific scientific questions in the GCIP Science Plan. The overall plans for data
management through the duration of the GCIP Project are described in Volume III of the
GCIP Implementation Plan (IGPO, 1994b).
GCIP is making use of existing operational and research programs to meet the
research objectives. An important example is the U.S. Department of Energy, Atmospheric
Radiation Measurement (ARM) Program, whose data from the Clouds and Radiation Testbed
(CART) site are being made available to the GCIP effort. Opportunities for cooperation are
being exploited with projects being formulated under other streams related to World Climate
Research Programme (WCRP), such as the Climate Variations (CLIVAR) and the Global
Ocean Atmosphere Land Surface (GOALS) Program. For example, the Pan American
Climate Studies (PACS) project is being formed as a U.S. contribution to CLIVAR/GOALS
to conduct research on the role of large-scale forcing from the tropics on continental
precipitation in the Americas. A more complete description of collaborative research activities
is given in Section 8.
GCIP research involves a systematic multiscale approach to accommodate physical
process studies, model development, data assimilation, diagnostics, and validation topics.
Such a multiscale developmental framework for the GCIP effort has three attributes:
(2) Capacity for sequential expansion to support the evolution of research
themes (e.g., initial emphasis on hydrological implications of warm-
season convective precipitation, moving next to issues related to
midlatitude cold-season hydrology).
(3) Flexibility to develop methods and algorithms that can be applied in
data-sparse areas of the globe outside the Mississippi River basin.
The understanding and modeling of a continental scale require, from the outset,
consideration of nonlinear-scale interactions in the aggregation of smaller processes to the
larger scale and vice versa. Progress in this area requires that methodologies be developed to
represent the coupling of processes that are important in one medium (e.g., the atmosphere) to
those that are important in another (e.g., the land surface). These techniques must be suitable
at the resolution of operational prediction and general circulation models (GCM) (about 10 to
100 km) and hence must be capable of representing in aggregate the effects of high levels of
heterogeneity in the underlying ground surface (WMO, 1992). Accordingly, the GCIP
research approach addresses activities on four scales (IGPO, 1994a):
Large-scale area (LSA) activities that occur in a phased timetable and emphasize a
particular region with special characteristics for a period of about two years. Scale
size is about 10^5 to 10^6 km^2. Four LSAs have been identified that in aggregate cover
most of the GCIP domain, as shown in Figure 1-2. The time phasing of activities
within each of these areas is also shown in the figure.
Intermediate-scale area (ISA) activities that will be phased in with those for the
LSAs and will serve as the basis for the regionalization of the parameters and
coefficients of land surface hydrological models. Scale size is about 10^3 to 10^4 km^2.
Small-scale area (SSA) activities that typically occur in association with efforts
requiring intensive observing periods (IOP) over a concentrated region to study a
focused set of issues. Scale size is less than 10^2 km^2.
Figure 1-2 Boundaries for LSAs and temporal emphasis for each LSA from 1994
through 2000.
The analyses and diagnostic studies conducted on the CSA, LSA, and ISA scales will
derive their data primarily from existing sources, with augmentation of some observing
systems as required. A major element of the rationale for carrying out the GCIP effort in the
Mississippi River basin is the potential for full utilization of a number of observing systems
(e.g., wind profiles and Doppler radars) not available to the same extent anywhere else in the
world. In a number of LSAs, data from the existing synoptic and climatological networks
operated by the National Weather Service can be augmented by data from relatively dense
climatological networks established and operated by other Federal agencies and state
organizations.
To the extent possible, the SSAs will be collocated with existing research basins, for
example, the Little Washita Experimental Watershed in Oklahoma operated by the U.S.
Department of Agriculture. The analyses, diagnostic studies, and model development on the
SSA scale will be derived from operational data sources (augmented as necessary), existing
research instrument complexes, and specially designed field programs of limited duration.
A fundamental thrust of the GCIP implementation strategy is that although the
developmental activities will be initiated in limited regions, they lead toward an integrated
continental-scale capability. Full continental domain studies have been
important in GCIP from the beginning of the EOP in 1995. Retrospective analyses and
baseline studies of water and energy balance will continue to be the main focus in the near-
term. In fact, as the EOP proceeds, the GCIP-derived budgets based on regional mesoscale
models will likely be superior in accuracy to budget estimates from other sources. These
diagnostic studies will also be valuable for validating hydrological aspects of climate model
simulations and understanding planetary-scale influences on North American hydrology.
The completion of the GCIP Science Plan in early 1992 heralded the beginning of a
number of major activities in GCIP that have progressed steadily over the past four years.
Some of the key accomplishments during this period are summarized in the remainder of this
section within the scientific/technical implementation framework as outlined in the following
section.
The two pivotal components of GCIP are (1) the development of a comprehensive
observational database for the Mississippi River basin that will be available for GCIP
analyses, and (2) the establishment of an evolving program of model development that will
permit the observations to be extended spatially within GCIP or applied globally with new
observations. A series of planned and ad hoc research and technical activities addressing
observing systems, algorithm development, quality assurance issues, and water and energy
budget studies link these pivotal components, as shown in Figure 1-3 (WMO, 1992).
Figure 1-3 Strategy framework for implementing GCIP.
With the interest in climate as a science over the past decade or so, computer models of the
earth/atmosphere system have taken place along two separate paths.
Many of the improvements in global models for weather prediction have occurred in, or in
close cooperation with, the major operational analysis centers such as the U.S. National
Center for Environmental Prediction (NCEP) and the European Centre for Medium Range
Weather Forecasts (ECMWF). Developments in global climate models, which have their
origins in the global weather models, have generally occurred in the U.S. in large research
establishments such as the NOAA/Geophysical Fluid Dynamics Laboratory (GFDL), the
NASA Goddard Space Flight Center (GSFC) and the National Center for Atmospheric
Research (NCAR). In the early development of strategies for implementing GCIP, it was
recognized that it would be necessary to draw on the strengths offered by both of these paths.
A further key strategy that was adopted early in GCIP was the need to fully exploit the high
resolution, limited area models that were being applied to regional weather prediction tasks
through various nesting procedures in the global models.
The GCIP research activities got underway in 1993 with primary support from NOAA.
The achievements to date can be grouped under four headings of data analysis, model
development, diagnostics of model output, and observing system enhancements. A more
comprehensive review of this activity was published in a special issue of the Journal of
Geophysical Research Volume 101, Number D3, March 20, 1996.
Since the approaches being taken by the principal operational analysis centers (e.g., the
U.S. National Environmental Prediction Center [NCEP], the Canadian Meteorological Centre
[CMC] and the ECMWF) are different, it is important that GCIP researchers have access to
data from more than one assimilation scheme. The NMC Eta Model and the NOAA Forecast
Systems Laboratory MAPS Model are both high resolution nested regional models, the
ECMWF and NMC operate global models at coarser resolution while the CMC uses a
variable grid approach with the Regional Finite Element (RFE) imbedded within a global
model. All these model outputs are being made available to GCIP researchers with special
efforts being made to archive the output from the regional mesoscale at a central location as
described in Section 11.
Improved land surface schemes were implemented in the three regional models prior
to the Enhanced Seasonal Observing Period from 1 April to 30 September 1996.
The GCIP Science Plan (WMO, 1992) recognized that the building of a database for
GCIP scientists would be a major undertaking and that the amount and different types of data
needed for GCIP studies would require an efficient data collection and management strategy.
The accomplishments to date in database development are in the areas of Pre-EOP
data collection, compilation of several initial data sets, and the implementation of a distributed
data management and service system. Each of these items is summarized in Part II of this
Major Activities Plan.
The responsibilities of the GCIP Data Management and Service System (DMSS) are to
provide data services to GCIP investigators, adapt to the evolving data requirements, and
compile the information on a five-year consolidated data set at the completion of the EOP.
Carrying out these responsibilities involves an implementation approach with evolutionary
improvements during the different stages of GCIP.
The DMSS implementation strategy makes maximum use of existing data centers to
minimize the lead time and expense required for development. These existing data centers
are made an integral part of the GCIP-DMSS through four data source modules that specialize
by data types (i.e., in situ, model output, satellite remote sensing, and GCIP special data) as
depicted in Figure 1-4. These four data source modules are connected to a GCIP central
information source that provides "single-point access" to the GCIP-DMSS. The primary
responsibilities for the data source modules along with their major functions and activities
were described in Volume III of the GCIP Implementation Plan (IGPO, 1994b).
Figure 1-4 Organization of GCIP Data Management System.
The purpose of the Major Activities Plan is to project a description of GCIP research
and associated activities over the next two to three years to preclude the need for frequent
revisions to the three volumes of the GCIP Implementation Plan. The initial version of the
Major Activities Plan covered the two-year period of 1995 and 1996 with an outlook for 1997
(IGPO, 1994c) and was updated last year (IGPO, 1995).
The description of planned activities is based on what should be done in an orderly
progression toward the end objectives of GCIP and with a realistic assumption about the
resources that will be available to do it. Adjustments are made the following year, as
appropriate, to rationalize the plans with the actual resources. The adjustments are used as a
starting point for projections in the following year's update.
This update of the Major Activities Plan covers the water years of 1997, 1998 and
outlook for 1999. It was shown in Figure 1-2 that during this period there will be an
emphasis on the four LSAs for two or more years. The structure of the Major Activities Plan
during the first two years was to concentrate on the activities in each of the LSAs. Since
activities are planned for each of the four LSAs, this will spread out the descriptions
pertaining to specific objectives. For this reason the Plan is divided into two parts. Part I
entitled Research devotes a section to each of the four science objectives and is described in
Sections 2,3,4, and
5. A number of variables were deemed critical to the success of GCIP and
were designated as Principal Research Areas for GCIP. These include precipitation, soil
moisture, land surface characteristics, streamflow and runoff, and, clouds and radiation. The
research activities for each of these critical variables are described in section 6.
A summary of the research activities planned for each of the four LSAs and the CSA is given in
section 7. The increasing importance of the collaborative research
activities is described in section 8.
The activities related to the data management objective are described in Part II of this
plan entitled Data Collection and Management.
1.1. Background
1.2 GCIP Objectives
1) Determine and explain the annual, interannual and spatial variability of the
water and energy cycles within the Mississippi River basin.
1.3 Project Implementation
1.3.1 Research Approach
(1) Support for a hierarchy of scales for observational work, algorithm and
model development, and validation and diagnostic studies leading to a
continental-scale capability.
Continental-scale area (CSA) activities that span the entire domain of the Mississippi
River basin with a scale size of about 3.2 x 10^6 km^2.
1.3.2 Continental Domain Synthesis
1.4 Accomplishments to Date
1.4.1 Scientific/Technical Implementation Framework
1.4.2 Research Path Achievements
i. Data Analysis
- Precipitation variability and extreme events: Implications for climate models
and climate change
ii. Model Development
- Physically-based subgrid scale statistical parameterization of rainfall: Coupling
mesoscale meteorology with small scale statistical descriptions
- Characterization and modeling of snow distribution and associated
land surface hydrology over mountainous watersheds
- Snow cover as an indicator of anthropogenic change
- Analysis and modeling of the hydrological cycle using Russian data
- Dynamic land surface/atmosphere parameterization at different spatial scales
for the South Platte River Drainage
iii. Diagnostics of Model Output
- Project for Intercomparison of Land-Surface Parameterization Schemes
(PILPS)
- Coupled boundary-layer formulation and land surface processes
- Using the Mesoscale Kinetic Energy (MKE) to Parameterize Subgridscale
(Mesoscale) Processes in General Circulation Models
- Evaluation of GCM Land-Surface Schemes in GCIP
- Summaries of North American continental-scale hydrology using ETA Model
analysis/forecast products
iv. Observing System Enhancements
- North American land surface/atmosphere hydrological cycle
- Prediction and diagnosis of atmospheric moisture and surface hydrology
variations over North America
- Aircraft Water Vapor Sensing System
- Automated soil moisture and temperature profile measurements at the DoE
ARM/CART Southern Great Plains Site for GCIP
- Surface flux measurements in the Little Washita Watershed in Oklahoma and
Bondville, Illinois
- Surface Radiation (SURFRAD) measurements at three sites in the Mississippi
River basin.
1.4.3 Achievements in the Operational Centers
1.4.4 Database Development
1.4.5 Data Management and Service System
1.5 Role and Structure of GCIP Major Activities Plan