Kyoji Sassa Executive Director

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Kyoji Sassa Executive Director
The first 5 years of IPL and themes
         for further 5 years
                    Kyoji Sassa
                     Executive Director
       International Consortium on Landslides (ICL)

Round Table Discussion “Towards a dynamic and global
   development of the International Programme on
                 Landslides (IPL)”
                  10:00-17:00 on 9 May 2011
     Organizer: IPL Global Promotion Committee
Kyoji Sassa Executive Director
Establishment of International Consortium on Landslides
                    January 21, 2002

Leading landslide researchers and UNESCO, WMO, UNISDR, MOFA,
  MEXT joined the foundation meeting of ICL during the UNESCO-
                 Kyoto University Joint Symposium.
         To create an International Programme on Landslides
       (The first international science programme proposed from Japan)
   To create an international platform putting Science into Practice
Kyoji Sassa Executive Director
Establishment of the International
        Programme on Landslides (IPL)
1. The initial IPL was established at UNESCO in November 2002.
2. ICL, UNESCO, UNISDR etc organized the Thematic Session on IFI
    and IPL during the World Conference on Disaster Reduction
    (WCDR) in January 2005 in Kobe, and adopted the Letter of Intent
    “to promote research and learning for landslide risk reduction”.
3. The Round Table Discussion “Strengthening Research and Learning
    on Earth System Risk Analysis “ -Toward a dynamic global network
    of International Programme on Landslides (IPL)- was organized in
    January 2006 at UNU by ICL, UNESCO, UNISDR, ICSU etc with
    supports from MOFA, MEXT, etc. and adopted the 2006 Tokyo
    Action Plan to establish a new IPL as a global scientific programme
4. The International Programme on Landslides (IPL) was established by
    the Tokyo Action Plan as a global scientific programme .
   UNESCO, WMO, FAO, UNISDR, UNU, ICSU, WFEO exchanged
    MoU with ICL to implement IPL within the Year 2006.
Kyoji Sassa Executive Director
Exchange of MOU
between ICL and UNESCO

Launching Ceremony of
the Organizing Committee
of The First World
Landslide Forum (below)
         Participants:
         ICL, UNESCO,
         UNU, CAO,
         MOFA, MEXT,
         MAFF, MLIT,
         Kyoto Univ.
        22 August 2006
        at ANA Hotel in
        Tokyo
Kyoji Sassa Executive Director
The International Programme on Landslides (IPL) is an international
programme promoting the United Nations International Strategy for
Disaster Risk Reduction (ISDR). IPL is managed by the IPL Global
Promotion Committee
Chair: Salvano Briceno, Director of UNISDR,
Deputy: Badaoui Rouhban, Director for Disaster Reduction of UNESCO
          Kyoji Sassa, Director of IPL World Centre (Secretariat of IPL)
          Paolo Canuti, President of ICL
It consists of ICL and UNESCO, WMO, FAO, UNISDR, UNU, ICSU,
WFEO, and IUGS.
IPL Includes Publication of Journal “Landslides”, IPL projects (43
topics), Identification of World Centres of Excellence (WCoEs) (12),
organization of World Landslide Forum (WLF1 at UNU, Tokyo in 2008,
WLF2 at FAO, Rome in 2011, WLF3 2014 in Beijing, China)
Kyoji Sassa Executive Director
Albania (1): Albania Geological Survey               16. Nepal (1): ICIMOD

Bulgaria(1): Univ. of Mining & Geo. (in process)     17. Nigeria(1): University of Nigeria

1. Cameroon (1): University of BUEA                  18. Norway (1): ICG, NGI

2. Canada (1): Geological Survey of Canada           19. Peru (1): Grudec Ayar,

3. China (5): China Geological Survey, et al.        20. Russia (5): Moscow State University

4. Columbia (1): Univ. Nacional de Columbia          Serbia (1): Univ of Belgrade (in process)

5. Croatia (1): Rijeka Univ. + Zagreb Univ.          21. Slovakia (1): Comenius University

6. Czech Republic (1): Charles University            22. Slovenia (2): Univ. Ljubljana, Geological Survey

7. Germany (1) :Technische Univ. Darmstadt           23.South Africa(1): Council for Geoscience

8. Indonesia (1): Gadjah Mada University             24.Sri Lanka (1): Cent. Eng. Consul. Bur.
9. India (1): Inst. of Disaster Management           25. Thailand (2): Ministry of Agri, ADPC

10. Iran (3): Agri. Res. and Edu. Organization etc   26. The Netherland (1): ITC School

11. Italy (4): University of Firenze, ISPRA, etc     27. Ukraine (1): Inst.Telecom. & Infor.

12. Japan (6): Kyoto Univ, Japan Landslide Soc.      28. USA (1): US Geological Survey

13. Korea (1): Korea Inst. (KIGAM)                   29. Uzbekistan (1): Institute Hydroingeo

14. Malaysia (2): Public Works Depart.               30. Vietnam (1): Inst. Transport S & T.

15. Mexico (1): Institute of Geography, UNAM         UNESCO, WMO, FAO, UNISDR, UNU, ICSU,
                                                     WFEO, IUGS
Kyoji Sassa Executive Director
The First World Landslide Forum
                     18-21 November 2008, at UNU, Tokyo
   Organizers: ICL, UNESCO, WMO, FAO, UNISDR, UNU, ICSU, WFEO, etc
     Cosponsors: CAO, MOFA, MEXT, MAFF, MLIT, JMA, SCJ, JICA, etc

The Forum was financially supported by MOFA (20 million JPY)
through UNISDR and the Grant-in-Aid of MEXT(10 million JPY) , etc
430 persons attended from 48 countries with those funds.
It was the largest meeting on landslides in the past.
Kyoji Sassa Executive Director
Kyoji Sassa Executive Director
Example of IPL (IPL-157)
    Risk Assessment Technology of Earthquake
    Induced On-land and Submarine Megaslides
   Landslides cause big disaster in many countries.
   Landslides are triggered by rains, earthquakes, and
    also often the combined effects of both triggers.
   Catastrophic megaslides often occur near the Plate
    borders on-land and also under the sea.
   Submarine landslides may trigger or enhance
    Tsunami wave.
   Risk Assessment Technology and Preparedness for
    earthquake induced on-land and submarine
    landslides are needed to prepare landslide disasters.
Kyoji Sassa Executive Director
2011 Tohoku Earthquake
                           JAPAN

       浅い地震
Distribution of shallow earthquakes in 1964-2006
Aratozawa landslide triggered
by 2008 Iwate-Miyagi Earthquake in Japan
1500

                                     1000
                                                                                 EW

                Accelaration (gal)
The Maximum                            500
Tohoku                                   0
Earthquake                            -500

Record at                            -1000

                                     -1500
MYG004                                       0   50   100      150        200        250   300
                                     3000
                                                            Time (sec)
                                     2000
               Accelaration (gal)
                                                                                 NS
                                     1000

                                         0
                                     -1000
                                                               Range of control signal
                                     -2000                     used for ring shear test
                                     -3000
                                             0   50   100      150        200        250   300
                                     2000
                                     1500                   Time (sec)
                                                                                 UD
              Accelaration (gal)

                                     1000
                                      500
                                        0
                                      -500
                                     -1000
                                     -1500
                                     -2000
                                             0   50   100      150        200        250   300
                                                            Time (sec)
Simulating
                         the sliding
                           surface

   Normal    axis      Normal
    stress              stress

                           ar s tress
                        She
Sliding             Sample
surface

      Dynamic Loading undrained ring shear test
                for Landslide Dynamic s:
 Geotechnical simulation of the sliding surface formation
       and post-failure motion within laboratory
The undrained dynamic loading ring shear
apparatus for landslide dynamics developed
in 1996 by 1 million USD (Right)
Portable ring shear apparatus (0.1 million
USD) under development by the Croatia-
Japan Joint project (IPL-161) in 2010. A
doctoral student invited from Croatia is
handling it at the initial test (Left and Center)
IPL-157 “Dynamics of subaerial and
    Mt. Fuji                                 submarine megaslides” studies a
           600 m

            300 m
                                             large-scale submarine landslide in
                                             Suruga bay. The size is 30x40 km.
                                 0m
                                             Depth is 800 m (similar to Usoy on-
                                             land landslide triggered by an
                                             earthquake in Tajikstan)
A                                                Submarine landslide induced by 2009 Suruga
               A’
                                                 bay earthquake
                    -300 m

                                                 2009 Surga bay earthquake
                        -600 m

    Suruga Bay     -900 m
                                             A                                        A’
                                      (km)
                                         0

                                        -1

0         50km                          -2
                                             0         10         20         30        40 (km)
Fig.1 A                            JAPAN                                                   C
                                                                                     0

                                       B                         Pacific                   H
                                      ough                       Plate
                                   Tr
                                                                                               VA

                          nkai
                       Na                                                                       S

      B                                                      IODP EXP333
                                                                                     100

   2000m

                                                                     Sample                     VA
   2500m
                                                                      for ring
   3000m                                                             shear test

   3500m

    10km
                                                                             3500
           8km
                                               C0018                        10km
                 6km                                                                            VA
                                                                      8km                        S
                       4km
                                                               6km                  200
                             2km                       4km
                                                2km
                                   0       0
Cyclic loading test (using an apparatus developed by IPL161-
Croatia project) on 190 m deep submarine deposit drilled by
IODP. The result presents landslide will occur on gently slope
on 9 degrees. Cyclic Loading No.8 (2011.4.5) RubberCorrection
                                  1200                                                     3000

                                             Normal stress

                                  900                                                      2500
                                                             Pore pressure

                                                                                                  Shear displacement (mm)
        Stress & Pressure (kPa)

                                  600                                                      2000

                                                                 Control signal
                                  300                                                      1500

                                     0                                                     1000
                                                                 Shear resistance

                                  -300                                                     500

                                                                      Shear displacement
                                  -600                                                     0
                                         0   100        200          300            400
                                                          Time (sec)
The Tohoku earthquake wave can trigger a submarine landslide in the Nankai Trough
The instant of failure (initiation of landslide).
The triggered landslide continues to move after earthquake
Global Network of IPL WEB: http://www.iplhq.org/
                  France (UNESCO, ICSU, WFEO)
                   Switzerland (UNISDR, WMO)

                                     Croatia

Global Network of IPL may be promoted through Journal, IPL Projects, WCOE,
WLF and New Initiatives of:
1.Establishment of the Regional Consortium on Landslides, such as Adriatic-Balkan,
ASEAN, Latin-American, possibly African and South-Asian, Arabian, etc. proposed
in December 2010.
2.Development of Landslide School Network with ICL and Non-ICL organizations
approved in November 2010.
3.World Reports on Landslides (Database) agreed in January 2011 in Kyoto
Secretarial meeting and read to upload in IPL WEB.
10th Anniversary of ICL
   ICL was established in Kyoto to create IPL on 21
    January 2002 with participants from UNESCO,
    UNISDR, WMO with supports from the Government of
    Japan.
   ICL and IPL have developed through this decade.
   The 10th Anniversary of ICL, Symposia on IPL projects,
    the programme planning meeting of WLF-3 in Beijing,
    2014, and the Round Table Discussion to make a strategy
    for the next decade will be organized in Kyoto on 18-20
    January 2012.
    Let’s meet and further discuss again in Kyoto at the 10th
    anniversary of ICL
Wishing Further Development of
                        Global Network of IPL
                        from Usoy landslide dam in
                        Tajikstan.

                            Usoy landslide source area

Usoy landslide dam
                                                     Sarez lake
           Triggered by 1911 earthquake in Tajikstan
 Volume of landslide: 1.1 billion m 3. The Dam Crest is 567 m. ,
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