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IAHS

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???? (Takeuchi Kuniyoshi) ????????? ?????????????(???????) ??????????????? ... Observe by RS: GPM, MW, SAR, GPS, laser altimeter, GRACE Resolutn, interpretn, GT data ... – PowerPoint PPT presentation

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Title: IAHS


1
IAHS
  • PUB
  • UNESCO, WMO FRIEND, HELP, WWAP
  • IAEA JIIHP
  • ICSU WCRP (GEWEX), IGBP, SCOWAR
  • IWALC (IWRA, IAHR, IWA, ICID, ICOLD)
  • WWC B of G
  • WWF3 PUB, IWALC, C-W Dialogue

2
Water in Political Arena
  • UN Water Conference 1977 Mal del Plata
  • Dublin Conference 1992
  • Rio Summit 1992 Agenda 21
  • Stockholm Water Conference
  • WWC, GWP 1996
  • WWF Marakech, Hague, Kyoto
  • WWAP, UN Y of Freshwater

3
???? (Takeuchi Kuniyoshi)
  • ????????? ?????????????(???????)
  • ???????????????
  • ???????(IAHS)??(2001-2005)
  • UNESCO???????(IHP)?????????
  • ?????RR2002??????????

4
Promotes the study of Hydrology as an aspect of
the earth sciences and of water resources.
International Association of Hydrological Sciences
Since 1922. Belongs to ICSU under IUGG. About
3000 members. Free of charge. Newsletters, HSJ,
Red Books. Scientific Assembly, Symposia, WSs.
http//www.cig.ensmp.fr/iahs/
5
International Commissions
  • Surface Water (ICSW)
  • Groundwater (ICGW)
  • Continental Erosion (ICCE)
  • Snow and Ice (ICSI)
  • Water Quality (ICWQ)
  • Water Resources Systems (ICWRS)
  • Remote Sensing Data Transmission (ICRSDT)
  • Atmosphere-Soil-Vegetation Relations (ICASVR)
  • Tracers (ICT)

6
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7
IAHS Decade of Prediction in Ungaged Basins (PUB)
  • An IAHS initiative to integrate hydrological
    sciences and technologies to make hydrological
    predictions possible in ungaged basins.

8
International Association of Hydrological Sciences
http//www.cig.ensmp.fr/iahs
9
PUB Operational Programm 1.     
Introduction 1.1 What is an Ungauged Basin? 1.2
Nature of Predictions 1.2.1 But what do we
want to predict? 1.2.2       Definition of
"Prediction in Ungauged Basins" 1.2.3 Natural
and Human-Induced Variability 1.3 Available
Options for PUB 1.4 Causes of the PUB Problem
Scientific Challenges Ahead 1.4.1 Fundamental,
Theoretical Deficiencies 1.4.2 Inadequacy of
Models and Modelling Approaches 1.4.3
Inadequate, Inappropriate Data 1.5 Opportunities
that Can Assist The Way Forward 1.5.1
Fundamental, Theoretical Deficiencies 1.5.2
Inadequacy of Models and Modelling Approaches
1.5.3 Inadequate, Inappropriate Data 2. PUB
Scientific Programme PUB Scientific Theme 1
Theoretical Hydrology PUB Scientific Theme 2
Observational Hydrology PUB Scientific Theme 3
Model Diagnostics and Inter-Comparison PUB
Scientific Theme 4 Advanced Data Collection
Technologies 3. PUB Basin Network 4. PUB
Implementation Programme PUB Implementation
Theme 5 Application Strategies and
Connectivity Connectivity to existing
programs Connectivity to Existing Commission
Activities PUB Implementation Theme 6
Developing Countries and Capacity Building
10
What is PUB?
  • PUB is an IAHS decadal initiative to provide
    hydrological data necessary for development and
    management in ungaged or information poor basins.
  • PUB is a scientific endeavor to assemble, promote
    and capacity-build the sciences and technology to
    predict and estimate the hydrological phenomena
    without depending on calibration data.

11
What to be predicted and estimated?
  • The hydrological phenomena to be predicted and
    estimated include precipitation, land surface
    processes, stream flow, groundwater flow, snow
    and ice, sediments, water quality etc.

12
What to be used for PUB?
  • The knowledge and means to be utilized include
    all currently and potentially available sciences
    and technology such as theoretical hydrology,
    remote sensing, GIS, tracers, physically based
    distributed hydrological models, meso-scale met
    models, all the knowledge to be learned from in
    situ observations in experimental basins etc.

13
Why is PUB now? PUB has always been an ultimate
goal of hydrology ever since its birth.
  • Hydrological data are endangered species.
  • Urgent needs for data especially in developing
    countries for their development and management
    of water. (Water crisis)
  • Current theoretical and technological
    developments are remarkable on hydrological
    process studies, scale issues, physically based
    hydrological modeling, remote sensing, meso-scale
    met models etc. (Readiness)
  • Time to show how science is useful and provide
    the necessary data to whom and where needed.

14
  • Decline of hydrological observation networks
  • Available technologies

15
Dynamic of the river gauges in the pan-Arctic
drainage basin and data available in total
Russian Arctic Net.
From Jeanna Balanishnikova, State Inst. of
Hydrology, Russia
16
1986
1992
17
Why data network declines?
  • In many cases, data closure results from
    withdrawal of government subsidies, forcing
    operational services to recoup costs through
    commercial sales, often with limited success.

18
Available Options for PUBs
  • Observe on site FRIEND, HELP ltFunding gt
  • Analogy from nearby gaged basins Statistical
    inform transfer. lttransferability, nearby basinsgt
  • Observe by RS GPM, MW, SAR, GPS, laser
    altimeter, GRACE ltResolutn, interpretn, GT datagt
  • Hydrol model simulation Dist phys based hydrol
    models. ltData, param ident, model
    transferability.gt
  • Integrated meteo hydro model simulation
    4DDAmeso-scale nesting, pbdhm. ltmodel, datagt

19
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21
Meso-scale meteorological nesting models
  • RAMS (Ibbit et al., 1999)
  • MRI/NPD-NHM (Saito et al., 2001)
  • MM5 (Chen and Dudhia, 2001)
  • IRSHAM (Kavvas et al., 1995)
  • ARPS (U. Oklahoma)

22
??????????????????????????????????(IRSHAM)???????
????????(??)
?????? ????
1995? 3?1? 3?2? 3?3?
????????? 19,501 km2
??????? ??????NCEP/NCAR (200km,
1947-present) DEM, ???????USGS EROS
(1km) ??UN-FAO (0.925 km)
23
RAMS Model Rainfall Nov 4-10, 199477x77 10 km
grid cells
mm rain
Tasman Sea
km10
PacificOcean
km10
24
170E
Tasman Sea
45S
PacificOcean
25
Orari
Opihi
Timaru
Pareora
26
Buller River at Te Kuha (6350 km2) - modelled
flow using RAMS model rain based on GWM analyses
6350
5080
Measured flow
Flow m3/s
Modelled flow
2540
  • Calibration of models to flow data makes only a
    small improvement to flood forecast quality.

1270
0
Time in hours
27
Hydrological Simulation of
Large Basins
28
BTOPMC (A YAMANASHI Model)
Both OF and BF generate at each
gridcell, according to local SD reflecting
block average SD SD(i) SD m ( ? - ?(i)) Flow
routing over all the flow segments.
Stream Network
At each gridcell i
For all stream segments
29
The Digital Stream network of Mekong Basin
94E, 34N
1. DEM data source GTOPO30(USGS Global 30
Arc Second Elevation Data Set Http//www1.gsi-mc.
go.jp/gtopo30/ Gtopo30.html)
(Threshold 3 grids)
2. Precipitation NOAA CD-ROM daily at 15
stations in 1987
3. Streamflow L. Mekong Hy. Y. B. daily at 5
sites in 1987
Grid size dx5.3km, dy5.54km
112E, 8N
30
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32
Time Table of PUB
  • 28-29 March 2002 Preparation WS in Kofu.
  • June 2002 Draft Science implementation plans
  • 20-22 November 2002 Kick-off WS in Brasilia
  • 2002-03 AGU, CGS, EGS, BAHC
  • .
  • March 2003 Participate to WWF3, Kyoto. Science
    for Society What can hydrology do for ungaged
    basins?
  • July 2003 Sapporo IUGG/IAHS S1.W7.JMH
  • Many more to come.

33
FIRST ANNUNCEMENT   Kick-Off Workshop on IAHS
DECADE OF PREDICTION IN UNGAGED BASINS (PUB) -
Hydrological Sciences on Mission -  
20-22 November 2002 Brasilia, Brazil
Organized by IAHS and Brasilia University (UNB),
CGEE Center of Strategic Studies Management and
Brazilian WR Association   Sponsored by IAHS,
MEXT Japan, IAEA, WWF3 (WWAP, NAH) Supported
by UNESCO, WMO, CEOP, GEWEX, HELP, FRIEND, CHASM,
CAUHSI (IWRA, IGBP-BAHC, WCRP, NASA, NASDA, ESA )
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