Title: NAME HYDROMETEOROLOGICAL WORKING GROUP
1NAMEHYDROMETEOROLOGICALWORKINGGROUP
- Motivation and Coordinated Activities
2Connecting the Hydrologic Cycle Exploration of
Terrestrial Linkages
- Leverage on the body of scientific and human
dimensions research currently proposed under NAME
to
-
- Improve hydrometerological and hydroclimatic
process knowledge and contribute to dynamic
management of water resources in the NAM region.
3Hydroclimatic Linkages in NAME
Precipitation
Evaporation
Runoff
Control Structures
Deep Percolation
4Hydroclimatic Linkages in NAME
Precipitation
Intensity Frequency Duration Areal Coverage
Forcing
Evaporation
Soils Vegetation Dynamics Antecedent Moisture
Forcing
Runoff Timing Local v Large-Scale Controls
W.R.
5Previous Findings(Dettinger and Diaz, JHM 1(4),
289-310 Gochis et al., 2003, JHM, in press. )
- Latitudinal transition to a summer-dominated
regime proceeding southward from Mogollon Rim.
6Previous Findings
- Climatological peak flows tend to lag peak
precipitation by 1-2 months (Dett.Diaz, ibid.) - Interannual streamflow values are linked to both
ENSO (Magana,1999) and PDO (Brito-Castillo et
al., Atmosfera, 2002) but there exists both
constructive and destructive tendencies in
correlation structure. - Evidence via diagnostics and modeling results of
possible feedbacks between soil moisture and snow
cover and the strength of the North American
Monsoon system (NAMS).
7Previous Findings
- Existence of a midsummer drought in parts of
Mexico, peripheral to the core monsoon region
of the SMO. - Smaller scale basin responses dominated by
precipitation structure short-duration
(0.5-1.0hr) high-intensity (10-100mm/hr) storms.
(Michaud et al. 2001) - Butlikely that many catchment-scale studies
remain to be translated from Spanish-speaking
literature and CNA reports !
8Lingering Uncertainties
- How are seasonal and shorter term, higher-order
precipitation characteristics related to
streamflow? - Given the uncertainty in precipitation
observations, what confidence is there in
existing estimations of runoff fractions? What
fraction is recycled to the atmosphere? - What influences do the meso-climates, terrain and
vegetation of the SMO, the Mexican plateau and
the coastal regions have on hydrological
cycling/partitioning?
9Meso-climate aspects of the NAM
Precipitation
Intensity Frequency Duration Areal Coverage
Forcing
Evaporation
Soils Vegetation Dynamics Antecedent Moisture
Forcing
10Meso-climate aspects of the NAM
11Lingering Uncertainties
- How are seasonal and longer term, higher-order
precipitation characteristics related to
streamflow? - Given the uncertainty in precipitation
observations, what confidence is there in
existing estimations of runoff fractions? What
fraction is recycled to the atmosphere? - What influences do the meso-climates, terrain and
vegetation of the SMO, the Mexican plateau and
the coastal regions have on hydrological
cycling/partitioning? - To what extent do soil moisture and snow
anomalies affect the evolution of the North
American Monsoon, and can such relationships (if
any) be demonstrated using long-term derived soil
moisture and snow data sets?
12Broad Goals of the NHWG
- Build relationships to Mexican and U.S. water
resource managers and the NAME atmospheric
research community for determination of critical
information requirements necessary for dynamic
water resources management. - Inventory and document availability and quality
of hydrographic and physiographic data over the
NAM region. - Identify critical processes and scales, which
govern the generation of runoff, its movement
over catchments, streamflow and moisture
recycling to the atmosphere. - Improve existing frameworks for hydrologic
simulation, ultimately resulting in measured
increases in predictability.
13Avenues for Opportunity.
Mexican Investigators International NAME
Research Comm.
Land Surface Forcing/Feedback Studies
Rainfall-Runoff Process Studies
Improved Process Understanding and Improved
Hydrologic Predictability
14Building NHWG Linkages
- International NAME
- Research Comm.
- intra-seasonal variability (MJO)
- remote forcing (SST)
- extreme event likelihood (T.S.s)
NHWG
- Mexican Investigators
- water user/manager informatics
- local practices/policies
- data retrieval and sharing
- technology transfer
15Hydrographic Data Archive
NAME NETWORK
MEXICAN NETWORK
Unified, Quality Controlled Dataset Standardized
Data Formats w/ Metadata
16Data Synthesis for Hydrological Modeling
Radiation Temperature Wind Precipitation Soil
Moisture
INITIALIZATION FORCING DATA
GIS FIELDS
Unified, Quality Controlled Dataset Standardized
Data Formats w/ Metadata
17Endgame Improve Existing Frameworks
in SimulationResulting in Increased
Predictability
Increased Process Knowledge
Standardized Data Archive for Simulation, Calibra
tion and Verification
Knowledge of Large- Scale Hydroclimatic Controls
Increased Awareness of Water User/Manager Needs
and Constraints
NHWG
18THE END . Thank You!