Incorporating the Land Data Assimilation
System into Water Resource Management and Decision Support Systems
Kristi R. Arsenault, Paul R. Houser, and
David A. Matthews
The Land Data Assimilation System (LDAS) team
at NASA’s Goddard Space Flight Center (GSFC) is developing a
system to aid water resource managers in making flood and drought
assessments and predictions. This system runs multiple land
surface models, assimilating and using the latest surface observations
and remotely sensed data as both operational and retrospective
forcings. The emphasis of LDAS is on capturing the most realistic
representations of land surface states and dynamics over large
areas and at high resolutions. The main hydrometeorological
variables on which LDAS focuses are soil moisture, evaporation,
snow cover, runoff, precipitation, and surface energy budget
variables.
The United States Bureau of Reclamation (Reclamation) relies
heavily on accurate and timely hydrometeorological information
for river basin management. More than 80 percent of the water
supply in the West is provided by snowpack runoff, so to generate
accurate flood forecasts, Reclamation must have accurate estimates
of snow water equivalent and must be able to monitor the evolution
of the snowpack into runoff. In addition to generating flood
forecasts, Reclamation also requires the ability to predict
the effects of drought conditions on agricultural production,
on the public, and on wildfire vulnerability. To address these
important issues, output from LDAS Land Surface Models (LSMs)
can be integrated into the river basin decision support systems
that Reclamation’s managers routinely use to manage western
river systems. Ultimately, using the LDAS LSM will improve overall
flood and drought risk analysis and prediction.
LDAS Background
LDAS research efforts are divided between two main projects:
North American LDAS (NLDAS) and Global LDAS (GLDAS). Both projects
share the same underlying objectives: LSM development, use of
observations as forcing data, and assimilation of different
satellite and radar information. A few differences do exist
between the two projects, but as the projects develop side-by-side
they strengthen each other’s growing utility for applications
and atmospheric prediction models.
Overall, the NLDAS and GLDAS projects are characterized as real-time,
distributed, uncoupled, land-surface simulation systems on a
U.S. national domain at .125-degree resolution and on a global
domain at .25-degree resolution. Both LDAS projects use a suite
of different LSMs running in tandem on these grid systems and
driven by common surface forcing.
Land Surface Models currently incorporated into LDAS include
Mosaic, the National Centers for Environmental Prediction model,
the Oregon State University model, the United States Air Force
model, the Office of Hydrology model, and the Community Land
Model. Additional LSMs being brought into LDAS include the Variable
Infiltration Capacity model and the Catchment Land Surface Model.
Other major components of the LDAS projects include replacement
of atmospheric model-based forcing with observations, assimilation
of remotely sensed and in-situ measurements into the LSMs, and
output validation and calibration of the LSMs. By using observations
to drive land surface models, such as precipitation and radiation,
biases present in coupled atmospheric-land surface model systems
can be avoided.
In the NLDAS project, the modeled precipitation is replaced
with a merged product consisting of Stage IV Weather Service
Radar-88 Doppler, gauge precipitation, and modeled precipitation
from the National Centers for Environmental Protection atmospheric
Eta-based 4-D Data Assimilation System. Downward shortwave and
longwave radiation products used are from GOES satellites. GLDAS
also has replaced some of its modeled fields with satellite-derived
precipitation, such as the NASA GSFC 3-hourly merged-satellite
product, which includes geostationary infrared, Special Sensor
Microwave/Imager, and Tropical Rainfall Measuring Mission data.
As for radiation fields, GLDAS uses global downward shortwave
and longwave radiation products from the Air Force Weather Agency.
LSMs are run over both LDAS domains using vegetation-based “tiles”
to simulate variability below the scale of the model grid squares,
with each tile representing an area covered by a given vegetation
type. Both NLDAS and GLDAS use the 1-km University of Maryland
vegetation classification scheme, which is based on the climatology
of AVHRR remote sensing data. A near-real-time, satellite-based,
leaf-area index derived from AVHRR and MODIS data is currently
being used in some of the LSMs.
Incorporation of Data
Assimilation Techniques
Substantial surface forcing errors in coupled land-atmosphere,
four-dimensional, data assimilation systems are a major reason
why LDAS and data assimilation techniques were developed. In
a real-time context, data assimilation can provide quality assurance
and validation of observations and can provide rapid identification
and diagnosis of barely perceptible problems. Several satellite
products to be used in LDAS include snow cover from MODIS and
soil moisture from the Aqua satellite’s Advanced Microwave Scanning
Radiometer. Assimilating these different satellite data into
LDAS will produce a more accurate description of the Earth system
than can be provided by the satellite observations driving the
land model simulations alone. Such descriptions would benefit
estimates of snow depth and cover in the winter and spring months
needed to forecast amounts that could contribute to river runoff,
especially in river basin areas like the Columbia River that
are heavily affected by spring snow melt. Assimilation of snow
information can directly improve the day-to-day snow states
in the LSM and can act as a means of diagnosing problems in
LSM physics. The improved LSM, unassisted by observational data,
can then provide improved snow simulations.
Integration of LDAS LSM Output into Reclamation’s
Decision Support Systems
Demonstrating the use and added value of LDAS output in Reclamation’s
operations and decision-support tools is becoming a major part
of LDAS’s applications research. Reclamation applies the latest
emerging technologies in decision support modeling to enable
river systems operations managers to make better-informed decisions.
The key river basin modeling technology includes RiverWare and
the Agricultural Water Resources Decision Support — Evapotranspiration
Toolbox system (AWARDS-ET Toolbox). RiverWare is a river modeling
and water accounting system that provides a flexible framework
for developing and running site-specific models that incorporate
the “law of the river” and other policy constraints. RiverWare
simulates the routing of the river flow operations through dams
and hydropower plants and maintains water delivery contracts
to irrigators and to recreational, municipal, and industrial
users. Even though Reclamation uses several hydrological modeling
tools for RiverWare, such spatially-distributed fields as soil
moisture are not fully accounted for in their operations. Including
such fields in their operations could help increase the accuracy
of Reclamation’s water resource accounting.
Determining the value added by LDAS output into RiverWare and
ET Toolbox will require an examination at various spatial and
temporal scales of the different vegetation and soil parameters
being used for LDAS and for running the LSMs. This examination
may improve water use estimates, especially during prolonged
drought. The ET Toolbox estimates the daily surface water use
requirements of riparian and crop vegetation and of open water
evaporation estimates. Integrating different LSM output into
the ET Toolbox and transferring the LSM parameterizations and
physics to different resolutions should improve ET drought estimates.
A plan to estimate how soil moisture fields can improve ET estimates
and the efficiency of water management is another major goal.
Two means of collaboration between LDAS and Reclamation include
(1) the exchange of data to help evaluate the ability and suitability
of the current LDAS to fit into Reclamation’s water management
operations and decision support tools, and (2) mutual validation
efforts that will improve the parameterization and physics of
LDAS LSMs and that will incorporate scaling issues to render
improved output specific to Reclamation’s needs. NASA recently
funded an LDAS extension project called Land Information Systems
(LIS). LIS is designed to run outlined LSMs at 1 km resolution
and to be used as a significant high-end computing applications
project, which would provide Reclamation even higher resolution
output to facilitate their need for information at the catchment
levels.
Acknowledgments
Funding for the GLDAS project is provided through the NASA
Earth Science Enterprise Program. The NLDAS project has been
funded primarily through the NASA Land Surface Hydrology Program.
Special thanks are expressed toward Brian Cosgrove, Jon Gottshalck,
and Dr. Xiwu Zhan for their comments and feedback on this article
and to the River Systems and Meteorology Team at Reclamation
for providing additional information. Also, we gratefully acknowledge
all those who have contributed to the overall LDAS projects
from NASA GSFC, other agencies, and universities.
About the Authors
Kristi Arsenault is a research analyst with the University
of Maryland, Baltimore County, Goddard Earth Science and Technology
Center, and she conducts her research at NASA GSFC. Ms. Arsenault
has been involved for almost two years with the GLDAS project
and investigates ways in which both the NLDAS and GLDAS projects
could be applied to different societal issues, such as water
resources management. Ms. Arsenault can be contacted at kristi
@hsb.gsfc.nasa.gov.
Dr. Paul Houser is in charge of the Hydrological Sciences Branch
at NASA GSFC. Dr. Houser is a leading investigator on the two
LDAS projects, and his research interests include local to global
land surface-atmospheric observation (both in-situ and remotely
sensed) and numerical simulation, development and application
of hydrologic data assimilation methods, and multi-scale moisture
investigations. He may be contacted at houser@hsb. gsfc.nasa.gov.
Dr. David A. Matthews is the manager of the River Systems and
Meteorology Group at the Bureau of Reclamation. Dr. Matthews’
group works on the Watershed and River Systems Management Program,
NEXRAD algorithm development and testing for snow water equivalent
estimates, agricultural water conservation decision support
system development for water supply and demand analysis and
forecasting, and early warning system applications of NEXRAD
data for dam safety. Dr. Matthews can be contacted at [email protected].
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