Abstract
Despite the significance of water, our knowledge of it as part of the global,
interacting system is meager. Consequently, we are far from understanding
how the hydrologic cycle will respond to a changing Earth system, or the
nature of water's influence across the components of the system. To address
these issues, the primary research strategy of this investigation, centers
on nesting or coupling coarse resolution GCMs, with high resolution mesoscale
models, with models including soil moisture, vegetation, and surface and
groundwater hydrology. In this manner, we are attempting to produce global
change predictions, in response to a variety of factors ranging from increases
in greenhouse gas concentrations to changes in land cover, at a spatial
scale which is appropriate to assess their impact. This research strategy
is accomplished through an emphasis on integrated regional studies and the
development of coupled earth system models. A basic requirement to accomplish
these goals is also to develop data sets for initialization and validation
of the various models at a variety of spatial scales, and to focus on critical
limitations in current models (e.g. cloud parameterizations). During this
process, we also contribute to the production of data sets which describe
changes in climate and the nature of climate variability.
The critical facets of climate and hydrology research needs have been described
in NRC reports (e.g. 1985), in planning documents of the USGCRP and the
WCRP (e.g. CLIVAR and GEWEX), and in "Earth System Science: A program
for global change." The primary research objectives are clear: determine
and understand the dynamics of the major reservoirs of water, the mechanisms for transfers of water between global reservoirs, predict changes in the distributions, volumes, fluxes of water resulting from change and
from human activities, and understand better the coupling of water with
other components of the Earth system.
We proposed to develop methodology and modeling capabilities to describe
quantitatively the presently uncertain rates associated with the sources,
sinks, and fluxes of the global water cycle with the ultimate goal of increasing
our ability to predict changes in the hydrologic cycle associated with
natural variability and human activities. A key element is to address changes
in the hydrologic cycle at a scale appropriate for considering its impact
on human activities, including agriculture and water resources. The proposed
research included 31 specific objectives, which are summarized here, for
the sake of brevity, as 12 primary objectives:
- Evaluate GCM capability to simulate hydrologic cycle components
- Evaluate GCM sensitivity to lower boundary forcing
- Generate global data sets for documentation of global change, specifically
for hydrologic variables, and for global model validation and verification
- Develop improved treatment of cloud and precipitation processes
- Develop and test components of high resolution regional atmospheric
models critical for water and energy fluxes
- Test the adaptability of terrestrial hydrologic models for sensitivity
to spatial and topographic scales
- Develop and test indirect measures of soil water content, with the objective
of integrating these results into mesoscale model simulations
- Develop and test coupled (nested) GCM-Mesoscale-Hydrologic Forecast
models
- Develop comprehensive databases and GIS for regions, such as the Susquehanna
River Basin, the Cape Region, and others, to facilitate the development
and evaluation of the nested model approach to regional prediction.
- Determine ice sheet mass balance, linking climate and hydrologic changes
to the future evolution of the cryosphere
- Develop and test a landscape evolution model in order to link climate
and hydrologic changes to the evolution of the land surface
- Develop improved climate-agriculture models in order to link climate
and hydrologic changes to the human dimensions of global change
These objectives incorporate three major integrating elements: (1) Documentation
of Earth system change (4-dimensional multiphase water, temperature and
diabatic heating, ice sheet mass balance, and regional scale terrestrial
and atmospheric water and energy budgets), (2) focused studies on controlling
processes (cloud processes, the interface of the atmosphere with ocean,
cryosphere, biosphere and land surface), and (3) integrated conceptual and
predictive models (extension of predictive capability across a spectrum
of spatial scales, verification and validation of hydrologic cycle predictive
capability, and coupled Earth system models).
The objectives and the integrating elements include a large number of challenging
scientific issues requiring focused research and the interactions of a significant
number of disciplines. Such a comprehensive set of objectives presents challenges
for even a large team of investigators. As a practical element, the significant
advances of this project are occurring because of the development of regional-scale
"experiments" designed to improve understanding of important physical
processes, develop coupled models, and assess and validate model predictions.
Almost the entire research team contributes to these regional-scale experiments,
each cooperatively seeking to advance the research objectives outlined
above.
To date, much of the emphasis of the project has focused on the Susquehanna
River Basin, with additional research on the Cape region of Florida. Much
of the future work is proposed for the Ohio and Tennessee River Basins.
These regions have been the focal point for assessing GCM capability, coupling
and evaluating GCMs with mesoscale models, incorporating improved surface
processes within the mesoscale models, integrating soil moisture measurements
and models, evaluating and linking terrestrial hydrologic models of surface
flow and groundwater, developing comprehensive GIS with a full spectrum
of data for specification of model boundary conditions and evaluating predictions,
and linking these models with other elements of the Earth system (e.g. landscape
evolution) and societally-important issues (e.g. impacts of changes in the
hydrologic cycle on agriculture).
The primary research strategy of this investigation, therefore, centers
on nesting or coupling coarse resolution GCMs, with high resolution mesoscale
models, with models including soil moisture, vegetation, and surface and
groundwater hydrology. In this manner, we are attempting to produce global
change predictions, in response to a variety of factors ranging from increases
in greenhouse gas concentrations to changes in land cover, at a spatial
scale which is appropriate to assess their impact. Such a strategy introduces
the potential that we will link the errors of one model with the errors
of each of the nested models. However, we have not jumped to make regional
global change predictions. Rather, our efforts are directed to a series
of careful studies designed to improve understanding and assess model capability
critically. The completed and planned studies of this investigation are
not only describing the uncertainties, but are, perhaps more importantly,
substantially increasing our knowledge of a variety of processes, and providing a strong foundation for high resolution, coupled Earth system models.
We are establishing a greater capability to utilize EOS observations to
describe key hydrologic and climatic processes, to further develop and validate
models, increasing our understanding of the past and the future and their
relationships to Earth system components and thus providing a more robust
predictive capability.
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