Report on the International Workshop for Large-scale Research Cruises

Size: px
Start display at page:

Download "Report on the International Workshop for Large-scale Research Cruises"

Transcription

1 Report on the International Workshop for Large-scale Research Cruises 1. General information Cruise Title: DIO Delve into the Indian Ocean Moderator s Name:K. Takai, K. Katsumata Moderator s Department:Department of Subsurface Geobiological Analysis and Research, Research and Development Center for Global Change Required cruise days (round-trip):approximately 300 days Major Survey Area:Indian Ocean Brief description of the scientific objectives and survey plan of the cruise(s) (up to 200 words) Indian Ocean is the least known among the three oceans; Pacific, Atlantic and Indian. After JAMSTEC large-scale cruise planning workshop, this grand cruise, named as Delve into the Indian Ocean (DIO), is proposed with a common ambition to know major unknowns in the world ocean and will be an important contribution to the international framework of 2 nd International Indian Ocean Expedition (IIOE 2) developed by the Intergovernmental Oceanographic Commission (IOC) and the Scientific Committee on Oceanic Research (SCOR) of UNESCO. The DIO cruise consists of three major initiatives and areas to explore: (1) one is the study of the evolution of the Indian Ocean, its' structure and geological history, and its biosphere based on investigations of water-driven mantle heterogeneity, geodynamo, tectonics, crustal hydrothermal activities and biodiversity and biogeography of deep-sea microbial and faunal communities in the Central Indian Ridge, Southwestern Indian Ridge, hotspots and their flanks; (2) another is the multidisciplinary exploration of geological and oceanographic settings in the eastern Indian Ocean (EIO) such as the seismogenic structures and the ocean upwelling functions in the EIO and the hypoxia biogeochemistry in the Bay of Bengal and the Andaman Sea; (3) a further one is to clarify response of Indian Ocean to the global climate change based on oceanographic observation in the southern and central Indian Ocean. The DIO cruise is planned as a 3-years project: in the first year (e.g., 2016), R/V Yokosuka or Kairei with HOV Shinkai6500 or ROV Kaiko MarkIV will pursue the initiatives (1) and (2) for 100 days; in the second year, R/V Yokosuka or Kairei with HOV Shinkai6500 or ROV Kaiko MarkIV will continue to address the initiatives (1) and (2) for 50 days and R/V Mirai will be in charge of the initiative (3) for 50 days; finally in the third year, a JAMSTEC new ship will complete all the initiatives over 100 days. Keywords (up to 5): IIOE 2, mantle to biodiversity, climate change, seismogenic zone, hypoxia Relationships to the JAMSTEC Mid-term program: Directly connected with (1) Research and Development for Submarine Resources (2) Research and Development for Global Change, (3) Research and Development for Earthquake and Tsunami, and (4) Research and Development for Marine Biosciences declared in the JAMSTEC Mid-term program 1

2 2. Co-proponent *Please add lines if necessary 1 Lynne Talley Name Organization Country Remarks Scripps Institution of Oceanography USA 2 Nobukazu Seama Kobe University Japan 3 Dass Bissessur 4 Olivier Pasnin Oceanography Oceanography 5 Greg Cowie University of Edinburg UK 6 Yasushi Ishihara JAMSTEC Japan 7 Cecilia McHugh Queens College, City Univ. of NY USA 8 Toshiya Kanamatsu JAMSTEC Japan 9 N.D. Hananto Indonesian of Science Indonesia 10 Chong Chen Oxford University UK 11 Greg Moore University of Hawaii USA 12 Yudi Nurul Ihsan Padjadjaran University Indonesia 13 Iwao Ueki JAMSTEC Japan 14 Shinsuke Kawagucci JAMSTEC Japan 15 Marie-Helen Cormier University of Rhode Island USA 16 Toshiya Fujiwara JAMSTEC Japan 17 Ken Takai JAMSTEC Japan 18 Katsuro Katsumata JAMSTEC Japan 19 Prerna Roy Oceanography 20 Arnaud Nicolas Oceanography 21 Yukio Masumoto University of Tokyo Japan 22 Jerome Dyment Institut de Physique du Globe de France Paris 23 Kyoko Okino AORI, University of Tokyo Japan 24 Tomoaki Morishita Kanazawa University Japan 25 Yoshifumi Nogi NIPR Japan 26 Wajih Naqvi National of India Oceanography of India 27 Hirsohi Kitazato JAMSTEC Japan 2

3 3. Scientific Objectives of the cruise(s) We propose here a series of grand cruise project named as Delve into the Indian Ocean (DIO) for comprehensive and interdisciplinary understanding of the least-explored ocean, the Indian Ocean, for the evolution of whole Indian Ocean and its biosphere, the structures and functions of unique geological and oceanographic settings in the eastern Indian Ocean (EIO) and the response of Indian Ocean to the global climate change. The cruise comprises six components, each originating from pre-proposals submitted under different disciplines. (1) Road back to Vasco Da Gama (L14-05: Takai et al.; L14-16: Rogers et al.; L14-45: Copley et al.; L14-56: Bissessur et al.). The scientific objectives of this theme are to further extend our understanding of deep-sea hydrothermal systems and their dark ecosystems in the Indian Ocean and the southern Atlantic Ocean. The genetic connectivity of the species will also be assessed for the demarcation of potential offshore MPAs. We will also characterize the structure of the southern part of the Mascarene Plateau and the structure and geological history of the Rodrigues Ridge and investigate the historical climate variability of the region. (2) Observational study of physical and biogeochemical variabilities in the Indian and Southern Oceans (L14-31, Talley et al.). The scientific objectives of this theme are to understand climate-relevant patterns in carbon uptake, upwelling and mixing structure and net community production in the Indian Ocean and Indian sector of the Southern Ocean. (3) Volatiles in the Earth and dynamic Cretaceous (L14-49: Seama et al.; L14-35: Dyment et al.). The scientific objectives of this theme are to clarify heterogeneous volatile content and migration in the mantle and geomagnetic history in the crust of the Indian Ocean and to estimate the impacts on the evolution of Indian Ocean. (4) Hypoxia and sediment biogochemistry of the Bay of Bengal: Benthic ecology and process studies across contrasting margins (L14-59: Cowie et al.). The scientific objective of this theme is to characterize the benthic community structures, functions and successions in different settings of hypoxia in the Bay of Bengal. (5) Intensive observation cruise for eastern Indian Ocean upwelling research initiative (L14-54: Matsumoto et al.; L14-14: Ihsan et al.). The scientific objectives of this theme are to characterize the monsoonal forcing upwelling in the eastern Indian Ocean and to estimate the impact of upwelling and oxygen-depletion on the nutrient distributions, biogeochemical processes, productivity and ecosystem dynamics. (6) Sunda margin geohazards assessment: from passive to active seismological imaging (L14-01: McHugh et al.; L14-41: Singh et al.; L14-57: Cummins et al.). The scientific objectives of this theme are to collect high-resolution bottom and sub-bottom geophysical structures along the Sunda subduction zone and to know the history and the future risk of tunami-earthquake in the eastern Indian Ocean area. These components are grouped into three expedition units or initiatives based on the the scientific objective synergy the observation and survey plans and platforms and the target areas: (1) & (3) can be conducted together in the in the Central Indian Ridge, Southwestern Indian Ridge, hotspots and their flanks; (4), (5) & (6) may have geographic affinity in the eastern Indian Ocean and Bay of Bengal; and (2) require an independent observation strategy for physical oceanography. However, all the proponents are strongly willing to establishing a comprehensive and interdisciplinary ocean exploration to challenge major unknowns in the Indian Ocean. 3

4 4. Survey Plan of the cruise(s) (maps required) The DIO cruise is best implemented by three platform types: (1) surface ships (R/V Yokosuka or Kairei) with deep-sea vehicles (HOV Shinkai6500 or Kaiko MarkIV); (2) oceanographic ship (R/V Mirai) with a full array of mooring, Argo buoy and oceanographic and atmospheric observation tools; and (3) a new JAMSTEC ship capable of both operations. Effectively to use these different platforms and quite long round-trip tracks of research ships from Japan to various sites in the Indian Ocean, three years of expedition plan will be required. Although the feasibility and the detail planning of each of the expeditions will be discussed and optimized among the proponents of DIO cruise and with the JAMSTEC ship operation committees and department, we provide here a brief survey plan of the cruise to cover all the scientific objectives and target areas (Figure 1). In the first year (probably in 2016): R/V Yokosuka or Kairei with HOV Shinkai6500 or ROV Kaiko MarkIV will first visit the Andaman Sea to conduct the seafloor observation for hydrothermal systems (8 days on sites and travels tentatively counted) and then will visit the Bay of Bengal (including the Lombok Basin) for seismogenic zone research and hypoxia ecosystem research (25 days) under the international framework as shown by yellow lines in Figure 1. Next, parts of the researches for the Indian Ocean mantle heterogeneity and the CIR deep-sea hydrothermal vents and ecosystems will be conducted by multidisciplinary onboard scientists from India to (19 days). Then, parts of the researches for the SWIR deep-sea hydrothermal vents and ecosystems and the geomagnetic survey in the northern flank of SWIR will be done (24 days) and move to the western Australia. Finally, parts of the oceanographic observations of upwelling in the EIO and the geophysical surveys in the southern parts of the Sunda Trench will be conducted before returning to Japan (24 days). The several parts of this first year cruise may contain the themes already approved themes by JAMSTEC (e.g., the CIR and SWIR hydrothermal vents and ecosystems research). In the second year: Two platforms will be operated for two legs. Leg 1 using R/V Kairei and ROV Kaiko MarkIV will visit the Indian Ocean but start with the geophysical survey for the seismogenic zones of the Sunda subduction zone as shown by purple lines in Figure 1 (15 days). Next, parts of the researches for the Indian Ocean mantle heterogeneity and the CIR deep-sea hydrothermal vents and ecosystems will be conducted by multidisciplinary onboard scientists from Indonesia to, including recovery of instruments deployed in the first year (20 days). Finally, parts of the oceanographic observations of upwelling in the EIO and the geophysical surveys in the Sunda Trench will be conducted before going back to Japan (15 days). Leg 2 using R/V Mirai will conduct the oceanographic observation along E80 from Kerguelen to Sri Lanka (40 days) and then will take in charge of geophysical surveys in the northern parts of the Sunda Trench (10 days). In the third year: JAMSTEC new ship will finalize the DIO cruise. First, the expedition will be conducted for the oceanographic observation along E57 from t o the off coast of Antarctic (45 days), and then the geomagnetic survey in the southern flank of SWIR and the seafloor observation of the SWIR hydrothermal vents and ecosystems will be done (25 days) to move to the South Africa. In the way back to Japan, parts of the oceanographic observations of upwelling in the EIO and the geophysical surveys in the Sunda Trench will be conducted (30 days). 4

5 5. Relevance to other scientific projects in Japan and/or abroad The DIO cruise is primarily based on the JAMSTEC Mid-term program and the JAMSTEC COE leadership of international ocean exploration. On the other hand, this cruise will represent the significant JAMSTEC s and Japanese contribution to 2nd International Indian Ocean Expedition (IIOE 2) developed by the Intergovernmental Oceanographic Commission (IOC) and the Scientific Committee on Oceanic Research (SCOR) of UNESCO to celebrate the 50 th anniversary of International Indian Ocean Experiment. In addition, this cruise will greatly contribute many other international oceanographic, earth science and marine biological programs such as XXX, InterRidge (e.g., Circum-Antarctic Ridges WG), IODP and XXXX. 6. Remarks Figure 1. A map showing a survey plan of the DIO cruise to cover all the scientific objectives and target areas. Yellow lines, circles and boxes indicate the proposed survey plan in the first year for the expedition with R/V Yokosuka or Kairei with HOV Shinkai6500 or ROV Kaiko MarkIV. Purple lines, circles and boxes indicate the proposed survey plan in the second year for the expedition with R/V Kairei with ROV Kaiko MarkIV and grey lines show the proposed survey plan in the second year for the expedition with R/V Mirai. White lines, circles and boxes are the proposed survey plan in the third year for the expedition with JAMSTEC new ship. 5

6 Appendix Maps in each of the pre-proposals that are finally merged into the DIO cruise. 6

The International Indian Ocean Expedition. Mika ODIDO IOC Sub Commission for Africa and the Adjacent Island States

The International Indian Ocean Expedition. Mika ODIDO IOC Sub Commission for Africa and the Adjacent Island States The International Indian Ocean Expedition Mika ODIDO IOC Sub Commission for Africa and the Adjacent Island States INDIAN OCEAN Facts and Figures 3rd largest ocean (after Pacific and Atlantic) Extent from

More information

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor Multibeam echo sounders - Research vessel Scripps Institution of Oceanography R/V Roger Revelle depth Source: Scripps Institution of Oceanography http://woodshole.er.usgs.gov/project-pages/caribbean/movie1.html

More information

Fluid-Rock Interactions and the Sub-Seafloor Biosphere

Fluid-Rock Interactions and the Sub-Seafloor Biosphere Fluid-Rock Interactions and the Sub-Seafloor Biosphere BACKGROUND DATA Examples of Key Scientific Questions (OOI Science Plan) Scientific Priorities (San Juan Meeting) Example ORION Experiments (San Juan

More information

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level.

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level. Interpreting Tectonic and Bathymetric Maps. The purpose of this lab is to provide experience interpreting the bathymetry of the seafloor in terms of tectonic and geologic settings and processes. Use the

More information

R/V Kairei Cruise Report KR Seismic study in the northwestern Pacific region. Jan. 4, 2011 Jan. 20, 2011

R/V Kairei Cruise Report KR Seismic study in the northwestern Pacific region. Jan. 4, 2011 Jan. 20, 2011 R/V Kairei Cruise Report KR11-01 Seismic study in the northwestern Pacific region Jan. 4, 2011 Jan. 20, 2011 Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Contents: 1.Cruise Information:

More information

The Indian Ocean. Copyright 2010 LessonSnips

The Indian Ocean. Copyright 2010 LessonSnips The Indian Ocean One of the five major geographic divisions of the world s ocean, the Indian Ocean is located in the Eastern Hemisphere. The Indian Ocean is bounded by three continents: Africa to the west,

More information

The Emerging SIBER Initiative of IMBER/IOGOOS: Biogeochemical Observing Programs and Modeling Needs in the Indian Ocean

The Emerging SIBER Initiative of IMBER/IOGOOS: Biogeochemical Observing Programs and Modeling Needs in the Indian Ocean The Emerging SIBER Initiative of IMBER/IOGOOS: Biogeochemical Observing Programs and Modeling Needs in the Indian Ocean Raleigh R. Hood (chair), Lynnath E. Beckley and S. Wajih A. Naqvi GSSC-XII Workshop,

More information

Chapter 02 The Sea Floor

Chapter 02 The Sea Floor Chapter 02 The Sea Floor Multiple Choice Questions 1. One of the following is not one of the world's major ocean basins: A. Atlantic Ocean B. Arctic Ocean C. Indian Ocean D. Antarctic Ocean E. Pacific

More information

Major IODP planning workshops

Major IODP planning workshops 9 Major IODP planning workshops Neville Exon Planning workshops for proposed future IODP drilling are critically important in generating ideas that can lead to successful drilling proposals that can address

More information

Originally published as:

Originally published as: Originally published as: Henstock, T., McNeill, L., Dean, S., Barton, P., Tilmann, F., Rietbrock, A., Robinson, D., Gulick, S., Austin, J., Djajadihardja, Y., Natawidjaja, D., Permana, H., Bonneville,

More information

IODP drilling and core storage facilities

IODP drilling and core storage facilities 4 IODP drilling and core storage facilities Neville Exon As the knowledge obtainable from ocean drilling is various and extensive, its end-users are similarly various and extensive. Scientific ocean drilling

More information

Practice Questions: Plate Tectonics

Practice Questions: Plate Tectonics Practice Questions: Plate Tectonics 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which type of plate boundary is shown? A) divergent

More information

Marine Science and Oceanography

Marine Science and Oceanography Marine Science and Oceanography Marine geology- study of the ocean floor Physical oceanography- study of waves, currents, and tides Marine biology study of nature and distribution of marine organisms Chemical

More information

The Sea Floor. Chapter 2

The Sea Floor. Chapter 2 The Sea Floor Chapter 2 Geography of the Ocean Basins World ocean is the predominant feature on the Earth in total area Northern Hemisphere = 61% of the total area is ocean. Southern Hemisphere = about

More information

USU 1360 TECTONICS / PROCESSES

USU 1360 TECTONICS / PROCESSES USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest

More information

You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science:

You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science: Ocean History You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science: Phoenicians Arabs Micronesians Polynesians Aristotle Erikson Columbus

More information

Geography of the world s oceans and major current systems. Lecture 2

Geography of the world s oceans and major current systems. Lecture 2 Geography of the world s oceans and major current systems Lecture 2 WHY is the GEOMORPHOLOGY OF THE OCEAN FLOOR important? (in the context of Oceanography) WHY is the GEOMORPHOLOGY OF THE OCEAN FLOOR important?

More information

Actual bathymetry (with vertical exaggeration) Geometry of the ocean 1/17/2018. Patterns and observations? Patterns and observations?

Actual bathymetry (with vertical exaggeration) Geometry of the ocean 1/17/2018. Patterns and observations? Patterns and observations? Patterns and observations? Patterns and observations? Observations? Patterns? Observations? Patterns? Geometry of the ocean Actual bathymetry (with vertical exaggeration) Continental Continental Basin

More information

Fig Available seismic reflection, refraction, and magnetic profiles from 107 the Offshore Indus Basin close to the representative profile GCDH,

Fig Available seismic reflection, refraction, and magnetic profiles from 107 the Offshore Indus Basin close to the representative profile GCDH, List of Figures Page No. Fig. 1.1 Generalized physiography of the Indian Ocean along with 2 selected (200 m, 1000 m, 2000 m, and 3000 m) bathymetric contours. Fig. 1.2 Lithospheric plates in the Indian

More information

SIBER: Sustained Indian Ocean Biogeochemistry and Ecosystem Research

SIBER: Sustained Indian Ocean Biogeochemistry and Ecosystem Research SIBER: Sustained Indian Ocean Biogeochemistry and Ecosystem Research Report to IIOE-2 Steering Committee Raleigh R. Hood (Chair) and Michael Roberts (co-chair) Sponsors: IIOE-2 SC1 Meeting, February 3

More information

A. Cruise summary. (4) Science proposals of cruise Affiliation PI Proposal titles AORI / The Univ. Tokyo

A. Cruise summary. (4) Science proposals of cruise Affiliation PI Proposal titles AORI / The Univ. Tokyo 1. Cruise information (1) Cruise designation (research vessel) MR11-3 (R/V MIRAI) A. Cruise summary (2) Cruise title (principal science proposal) and introduction Change in material cycles and ecosystem

More information

Data & Information Management in IIOE-2 IndOOS and sources of IO data

Data & Information Management in IIOE-2 IndOOS and sources of IO data Data & Information Management in IIOE-2 IndOOS and sources of IO data Louise Wicks IOC Perth Programme Office IOC/IIOE2-OTGA and IORA Joint Training Course: Research Data Management 22-26 May 2016: Kuala

More information

12. The diagram below shows the collision of an oceanic plate and a continental plate.

12. The diagram below shows the collision of an oceanic plate and a continental plate. Review 1. Base your answer to the following question on the cross section below, which shows the boundary between two lithospheric plates. Point X is a location in the continental lithosphere. The depth

More information

Studying the Ocean Using Live Data

Studying the Ocean Using Live Data Studying the Ocean Using Live Data Overview The Argo buoy project is a major oceanographic study that harnesses the power of automated unmanned buoys traveling the world s oceans (http://www.argo.ucsd.edu/).

More information

Indian Ocean Tsunami Warning System: Example from the 12 th September 2007 Tsunami

Indian Ocean Tsunami Warning System: Example from the 12 th September 2007 Tsunami Indian Ocean Tsunami Warning System: Example from the 12 th September 2007 Tsunami Charitha Pattiaratchi 1 Professor of Coastal Oceanography, The University of Western Australia Email: chari.pattiaratchi@uwa.edu.au

More information

Biogeochemistry of trace elements and isotopes in the Indian Ocean

Biogeochemistry of trace elements and isotopes in the Indian Ocean Biogeochemistry of trace elements and isotopes in the Indian Ocean Sunil Kumar Singh Geosciences Division Physical Research Laboratory Ahmedabad 380009 Ministry of Earth Sciences Government of India 2

More information

Chapter 9 Lecture Outline. Oceans: The Last Frontier

Chapter 9 Lecture Outline. Oceans: The Last Frontier Chapter 9 Lecture Outline Oceans: The Last Frontier The Vast World Ocean Earth is referred to as the blue planet 71% of Earth s surface is oceans and marginal seas Continents and islands comprise the remaining

More information

International Research Collaboration in Indonesia: LIPI as a special reference

International Research Collaboration in Indonesia: LIPI as a special reference Workshop on Science & Technology Cooperation With Developing Countries on Global Issues. Tokyo, 8 October 2008 International Research Collaboration in Indonesia: LIPI as a special reference Hery Harjono

More information

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are 11.1 Ocean Basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are w the Pacific w the Atlantic w the Indian w the Southern w the Arctic The

More information

R/V Kairei Cruise Report KR Seismic study in Nansei-Shoto Region. November 17, 2013 December 14, 2013

R/V Kairei Cruise Report KR Seismic study in Nansei-Shoto Region. November 17, 2013 December 14, 2013 R/V Kairei Cruise Report KR13-18 Seismic study in Nansei-Shoto Region November 17, 2013 December 14, 2013 Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Contents: 1.Cruise Information:

More information

Do NOT open the test until instructed to do so.

Do NOT open the test until instructed to do so. Raw Score: Rank: School: Team Number: Names: Boyceville Invitational, December 2, 2017 Dynamic Planet Plate Tectonics and Geographical Impacts Do NOT open the test until instructed to do so. 2011 Tohoku

More information

PRINCIPLE OF OCEANOGRAPHY PBBT101 UNIT-1 INTRODUCTION OF OCEANIC ENVIRONMENT. PART-A (2 Marks)

PRINCIPLE OF OCEANOGRAPHY PBBT101 UNIT-1 INTRODUCTION OF OCEANIC ENVIRONMENT. PART-A (2 Marks) PRINCIPLE OF OCEANOGRAPHY PBBT101 UNIT-1 INTRODUCTION OF OCEANIC ENVIRONMENT 1. Define marine ecosystem. 2. What is geography? 3. Give two Oceanic zones 4. What is sea? 5. Define oceanography? 6. Enlist

More information

The Ocean Floor Earth Science, 13e Chapter 13

The Ocean Floor Earth Science, 13e Chapter 13 The Ocean Floor Earth Science, 13e Chapter 13 Stanley C. Hatfield Southwestern Illinois College The vast world ocean Earth is often referred to as the blue planet Seventy-one percent of Earth s surface

More information

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,

More information

Korean Arctic Research 2015 update

Korean Arctic Research 2015 update FARO Annual Meeting, ASSW 2016 Fairbanks, Alaska, 12 March 2016 Korean Arctic Research 2015 update International Cooperation Department Korea Polar Research Institute Outline KOPRI and Korean Arctic research;

More information

Air-Sea Interaction Study in the Tropics by JAMSTEC

Air-Sea Interaction Study in the Tropics by JAMSTEC Air-Sea Interaction Study in the Tropics by JAMSTEC History : Major Activities related to Air-Sea Interaction Study 1987 JENEX-87 (Japanese El Niño Experiment - 87) * This was the first trial for El Niño

More information

CGSN Overview. GSN Sites CSN Sites Shore Facilities

CGSN Overview. GSN Sites CSN Sites Shore Facilities GSN Sites CSN Sites Shore Facilities CGSN Overview Coastal Pioneer Array Endurance Array Global Irminger Sea Southern Ocean Station Papa Fixed assets Surface mooring Subsurface mooring Mobile assets Ocean

More information

Bay of Bengal Surface and Thermocline and the Arabian Sea

Bay of Bengal Surface and Thermocline and the Arabian Sea DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Bay of Bengal Surface and Thermocline and the Arabian Sea Arnold L. Gordon Lamont-Doherty Earth Observatory of Columbia

More information

The Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College

The Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College The Ocean Floor Chapter 14 Essentials of Geology, 8e Stan Hatfield and Ken Pinzke Southwestern Illinois College The vast world ocean Earth is often referred to as the water planet 71% of Earth s surface

More information

Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-cho, Yokosuka, Kanagawa, , JAPAN

Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-cho, Yokosuka, Kanagawa, , JAPAN LARGE EARTHQUAKE AND ASSOCIATED PHENOMENA OBSERVED WITH SEAFLOOR CABLED OBSERVATORY NEAR EPICENTER - AN IMPLICATION FOR POSSIBLE ADDITIONAL MEASUREMENT WITH TELECOMMUNICATION NETWORKS FOR IDENTIFICATION

More information

Earth s Structure and Surface

Earth s Structure and Surface Earth s Structure and Surface Structure of the Earth The earth is thought have originated about 4.5 billion years ago from a cloud or clouds of dust. The dust was the remains of a huge cosmic explosion

More information

The Major Ocean Basins and Their Features

The Major Ocean Basins and Their Features Where Submarines Lurk Recent satellite studies and deep-sea mapping programs have revealed in dramatic fashion that the ocean floor is not flat. Indeed, the terrain of the ocean floor surpasses that of

More information

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,

More information

MR99-K04 Cruise Summary

MR99-K04 Cruise Summary MR99-K04 Cruise Summary 1. Introduction Oceanic conditions in the subtropical and subarctic gyres, especially in and around the Kurishio Extension, are thouth to be important to the North Pacific decadal/interdecadal

More information

Deep Submergence Science Committee A summary of Activities, Plans, Issues from Patricia Fryer, Chair

Deep Submergence Science Committee A summary of Activities, Plans, Issues from Patricia Fryer, Chair Deep Submergence Science Committee A summary of Activities, Plans, Issues from 2003 Patricia Fryer, Chair NDSF Chief Scientist Replacement A decision was made to search outside WHOI for a replacement for

More information

The Ocean Networks Canada Observatory Science, Industry and Society

The Ocean Networks Canada Observatory Science, Industry and Society The Ocean Networks Canada Observatory Science, Industry and Society S. Martin Taylor President and CEO, Ocean Networks Canada (www.oceannetworks.ca) May 31st, 2012 Global challenges of ocean events, processes

More information

Organisms in the Ocean

Organisms in the Ocean Oceans Objective 8.E.1.2 Summarize evidence that Earth's oceans are a reservoir of nutrients, minerals, dissolved gases, and life forms: estuaries, marine ecosystems, upwelling, and behavior of gases in

More information

A brief history of scientific ocean drilling from the Australian and New Zealand points of view

A brief history of scientific ocean drilling from the Australian and New Zealand points of view 3 A brief history of scientific ocean drilling from the Australian and New Zealand points of view Neville Exon A full review of Australia s involvement in ocean drilling since its onset in 1968 through

More information

DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory

DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory DESIGN & IMPLEMENATION WORKSHOP Conceptual Network Design For The Regional Cabled Observatory 50 N N4 N10 N11 N7 N8 N5 N9 N6 AN INTEGRATED RCO Maintain Integrity of a Plate-Scale Experiment & Future Expandability

More information

Chapter Two. Figure 02_02. Geography of the Ocean Basins. The Sea Floor

Chapter Two. Figure 02_02. Geography of the Ocean Basins. The Sea Floor Chapter Two The Sea Floor Geography of the Ocean Basins Figure 02_02 The world ocean is the predominant feature on the Earth in total area. In the Northern Hemisphere, 61% of the total area is ocean. In

More information

Meeting July 2018 Agenda Item 7.1. Tsunami Service Provider Messages for the Maritime Community. Submitted by IOC Secretariat SUMMARY

Meeting July 2018 Agenda Item 7.1. Tsunami Service Provider Messages for the Maritime Community. Submitted by IOC Secretariat SUMMARY WWNWS WWNWS10/7/1 Meeting 10 19 July 2018 Agenda Item 7.1 Tsunami Service Provider Messages for the Maritime Community Submitted by IOC Secretariat SUMMARY Executive Summary: This document provides details

More information

OCN 201 Physiography of the Seafloor

OCN 201 Physiography of the Seafloor OCN 201 Physiography of the Seafloor 1 Ocean Depth versus Continental Height Why do we have dry land? Solid surface of Earth is dominated by two levels: Land with a mean elevation of +840 m (29% of Earth

More information

OCEANOGRAPHY CURRICULUM. Unit 1: Introduction to Oceanography

OCEANOGRAPHY CURRICULUM. Unit 1: Introduction to Oceanography Chariho Regional School District - Science Curriculum September, 2016 OCEANOGRAPHY CURRICULUM Unit 1: Introduction to Oceanography OVERVIEW Summary In this unit students will be introduced to the field

More information

The giant Gas planets of the outer solar system. Rocky inner planets. Silicates with Iron/Nickel cores. Hydrogen, Helium, methane, water, ammonia

The giant Gas planets of the outer solar system. Rocky inner planets. Silicates with Iron/Nickel cores. Hydrogen, Helium, methane, water, ammonia SUN Hydrogen (74%), some helium (24%) Rocky inner planets Silicates with Iron/Nickel cores The giant Gas planets of the outer solar system Hydrogen, Helium, methane, water, ammonia Where did the water

More information

OCN 201 Physiography of the Seafloor

OCN 201 Physiography of the Seafloor OCN 201 Physiography of the Seafloor Hypsometric Curve for Earth s solid surface Note histogram Hypsometric curve of Earth shows two modes. Hypsometric curve of Venus shows only one! Why? Ocean Depth vs.

More information

Development of EIA protocol for deep-sea ecosystems and seabed mining

Development of EIA protocol for deep-sea ecosystems and seabed mining Development of EIA protocol for deep-sea ecosystems and seabed mining Hiroyuki Yamamoto, Ryota Nakajima, Takehisa Yamakita, Dhugal Lindsay, Tomohiko Fukushima Environmental Impact Assessment Research Group,

More information

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones Name: Date: Period: Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonics - s - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones The plates are

More information

Fukushima nuclear power plant damaged by M9 Earthquake with some focus on ocean

Fukushima nuclear power plant damaged by M9 Earthquake with some focus on ocean Fukushima nuclear power plant damaged by M9 Earthquake with some focus on ocean Moto Ikeda (Hokkaido Univ. & JAMSTEC) Oceanographic Society of Japan, Earthquake Disaster Working Group Magnitude-9 earthquake

More information

Crater, fault, volcanic cone, lava flow

Crater, fault, volcanic cone, lava flow 2-1 INTERNATIONAL HYDROGRAPHIC ORGANIZATION INTERGOVERNMENTAL OCEANOGRAPHIC COMMISSION (of UNESCO) Note: The boxes will expand as you fill the form. UNDERSEA FEATURE NAME PROPOSAL (Sea NOTE overleaf) Name

More information

DOOS platform considerations

DOOS platform considerations DOOS platform considerations Focus on platforms that can be deployed below 1000m and in a globally distributed fashion (or at hotspots, choke points, places of societal interest) Uwe Send Scripps Institution

More information

S/V Yokosuka Cruise Report YK14-E02

S/V Yokosuka Cruise Report YK14-E02 S/V Yokosuka Cruise Report YK14-E02 2014FY Marine geological and geophysical surveys to unravel the subduction zone great earthquakes and tsunamis : Seismic refraction and reflection survey in the outer

More information

Earthquakes Physical Geology 2017 Part 1: Exploring Earthquake distributions. Home butto California Earthquakes: 1) 2) 3) above

Earthquakes Physical Geology 2017 Part 1: Exploring Earthquake distributions. Home butto California Earthquakes: 1) 2) 3) above Earthquakes Physical Geology 2017 Adapted from a lab by Jennifer Wenner This lab is designed to give you experience exploring seismicity associated with different plate boundaries. You will examine seismograms

More information

Physical Oceanography OEAS 405/505 Fall 2013

Physical Oceanography OEAS 405/505 Fall 2013 Physical Oceanography OEAS 405/505 Fall 2013 Instructor: Prof. Tal Ezer http://www.ccpo.odu.edu/facstaff/faculty/tezer/ezer.html Office: CCPO, Innovation Research Park Bldg. #1 4111 Monarch Way, Room 3217

More information

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past. 1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments

More information

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features

More information

Lawrence A. Lawver Ian W.D. Dalziel Robert Larter University of Texas at Austin, Institute for Geophysics British Antarctic Survey

Lawrence A. Lawver Ian W.D. Dalziel Robert Larter University of Texas at Austin, Institute for Geophysics British Antarctic Survey 20 August 2012 Prof. Hans-Werner Schenke, Chairman GEBCO Sub-Committee on Undersea Feature Names (SCUFN) International Hydrographic Bureau (IHB) 4, Quai Antoine 1er B.P. 445 MC 98011 MONACO CEDEX Principality

More information

Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p.

Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p. Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p. 2 Mid-Ocean Ridge Province p. 3 Benthic and Pelagic Provinces

More information

Map shows 3 main features of ocean floor

Map shows 3 main features of ocean floor Map shows 3 main features of ocean floor 2017 Pearson Education, Inc. Chapter 3 Marine Provinces 2017 Pearson Education, Inc. 1 Chapter 3 Overview The study of bathymetry determines ocean depths and ocean

More information

Chapter 20. Plate Tectonics

Chapter 20. Plate Tectonics Chapter 20 Plate Tectonics Early Evidence (Wegener) The geometric fit of the continents. The similarity in rock age groups between adjoining regions. The similarity in Paleozoic fossils between adjoining

More information

Preparation for Future Earthquake and Tsunami Hazards: Lessons Learned from the 2004 Sumatra-Andaman Earthquake and the Asian Tsunami

Preparation for Future Earthquake and Tsunami Hazards: Lessons Learned from the 2004 Sumatra-Andaman Earthquake and the Asian Tsunami First International Conference of Aceh and Indian Ocean Studies Organized by Asia Research Institute, National University of Singapore & Rehabilitation and Construction Executing Agency for Aceh and Nias

More information

Question: What is the primary reason for the great abundance of fish along the Peruvian coast?

Question: What is the primary reason for the great abundance of fish along the Peruvian coast? Buzzer Question # 1 Question Type: toss-up Question Format: Multiple Choice Category: Biology What is the primary reason for the great abundance of fish along the Peruvian coast? Answer W: upwelling Answer

More information

GLG101: What-To-Know List

GLG101: What-To-Know List Exam 3, Page 1 GLG101: What-To-Know List (Derived from Before You Leave This Page Lists) This list is intended to guide your reading and to help you prepare for the online multiple-choice quizzes. Each

More information

Promoting Seafloor Observation in China -- A Meeting Report

Promoting Seafloor Observation in China -- A Meeting Report Promoting Seafloor Observation in -- A Meeting Report Introduction With its rapid development in economy, is now placing more emphasis on marine science and technology. Recently, construction of a sea-floor

More information

Announcements. Manganese nodule distribution

Announcements. Manganese nodule distribution Announcements Lithospheric plates not as brittle as previously thought ESCI 322 Meet in Env. Studies Bldg Rm 60 at 1 PM on Tuesday One week (Thursday): Quiz on Booth 1994 and discussion. (Lots of odd terms

More information

MARINE GEOLOGY & GEOGRAPHY

MARINE GEOLOGY & GEOGRAPHY MARINE GEOLOGY MARINE GEOLOGY & GEOGRAPHY Marine Geology 4 LAYERS OF THE EARTH CRUST THICKNESS: VARIES BETWEEN OCEAN & CONTINENTS 5-40 KM STATE: SOLID ELEMENTS: SILICON, ALUMINUM, CALCIUM, SODIUM, POTASSIUM

More information

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation) Science 10 Review Earth Science Vocabulary asthenosphere continental drift theory converging plates diverging plates earthquakes epicentre fault hot spot inner core lithosphere mantle mantle convection

More information

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features 1 2 3 4 5 6 7 8 9 10 11 CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools.

More information

News Release December 30, 2004 The Science behind the Aceh Earthquake

News Release December 30, 2004 The Science behind the Aceh Earthquake News Release December 30, 2004 The Science behind the Aceh Earthquake PASADENA, Calif. - Kerry Sieh, the Robert P. Sharp Professor of Geology at the California Institute of Technology and a member of Caltech's

More information

DEVASTATING DAMAGE DUE TO THE 2004 INDIAN OCEAN TSUNAMI AND ITS LESSONS

DEVASTATING DAMAGE DUE TO THE 2004 INDIAN OCEAN TSUNAMI AND ITS LESSONS DEVASTATING DAMAGE DUE TO THE 2004 INDIAN OCEAN TSUNAMI AND ITS LESSONS Fumihiko Imamura 1 1 Professor, Tsunami Engineering, Disaster Control Research Center, Tohoku University, Japan Email: imamura@tsunami2.civil.tohoku.ac.jp

More information

Update on Pacific Arctic Group (PAG) activities

Update on Pacific Arctic Group (PAG) activities Update on Pacific Arctic Group (PAG) activities Jacqueline Grebmeier 1 and Sung-Ho Kang 2 1 Member, PAG Executive Committee, Chesapeake Biological Laboratory, University of Maryland Center for Environmental

More information

Lessons from the 2004 Sumatra earthquake and the Asian tsunami

Lessons from the 2004 Sumatra earthquake and the Asian tsunami Lessons from the 2004 Sumatra earthquake and the Asian tsunami Kenji Satake National Institute of Advanced Industrial Science and Technology Outline 1. The largest earthquake in the last 40 years 2. Tsunami

More information

Unit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core.

Unit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core. Unit 4 - Water How did the oceans form? What special adaptations do saltwater organisms have? Where does our water come from? How do humans affect the Earth s water? Crust Rigid outer shell of Earth Oceanic

More information

Weather & Ocean Currents

Weather & Ocean Currents Weather & Ocean Currents Earth is heated unevenly Causes: Earth is round Earth is tilted on an axis Earth s orbit is eliptical Effects: Convection = vertical circular currents caused by temperature differences

More information

60% water. Big Bang: 14,000 millions years ago The Earth originated about 4,500 millions years ago its orbit allows water to exist in a liquid state!

60% water. Big Bang: 14,000 millions years ago The Earth originated about 4,500 millions years ago its orbit allows water to exist in a liquid state! Ch2. The Sea Floor #1 Why geology of the oceans? Marine habitats are directly shaped by geological processes The form of the coastlines The depth of the water Type of bottom (muddy, sandy, rocky) #2 Geological

More information

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates.

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. As you can see, some of the plates contain continents and others are mostly under the ocean.

More information

Chapter 2 Plate Tectonics and the Ocean Floor

Chapter 2 Plate Tectonics and the Ocean Floor Chapter 2 Plate Tectonics and the Ocean Floor Matching. Match the term or person with the appropriate phrase. You may use each answer once, more than once or not at all. 1. hydrothermal vents A. convergent

More information

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent Name: Date: Period: Plate Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonic plates are constantly moving and interacting As they move across the asthenosphere and form plate boundaries

More information

The Growth of Oceanography

The Growth of Oceanography The Growth of Oceanography Why study oceanography? Scientific Curiosity How do oceans operate and interact with entire earth system? Why study oceanography? Scientific Curiosity How do oceans operate and

More information

General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On

General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank

More information

Dynamic Crust Practice

Dynamic Crust Practice 1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides

More information

Coordinates : A - of midpoint or summit : Lat., Long. } to. Description (kind of feature) : seachannel

Coordinates : A - of midpoint or summit : Lat., Long. } to. Description (kind of feature) : seachannel INTERNATIONAL HYDROGRAPHIC ORGANIZATION INTERGOVERNMENTAL OCEANOGRAPHIC COMMISSION (of UNESCO) IHO/IOC Form No. 1 UNDERSEA FEATURE NAME PROPOSAL (See NOTE overleaf) Ocean or Sea Japan Sea Name proposed

More information

Captain s Tryouts 2017

Captain s Tryouts 2017 Captain s Tryouts 2017 Dynamic Planet Test Written by: Araneesh Pratap (Chattahoochee High School) Name: Date: Answer all questions on the answer sheet. Point values are given next to each question or

More information

Chapter 20. Plate Tectonics. Scientific Method. This is a repeatable measurement or experiment. One or more possible explanations to link observations

Chapter 20. Plate Tectonics. Scientific Method. This is a repeatable measurement or experiment. One or more possible explanations to link observations Chapter 20 Plate Tectonics Scientific Method 1. Observation (fact) This is a repeatable measurement or experiment 2. Hypothesis One or more possible explanations to link observations 3. Testing Further

More information

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic

More information

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA? The Ocean Basins How Deep is the Ocean? 1 2 Three Major Oceans Three Major Oceans Pacific Atlantic the shallowest ocean (3.3km average depth) Indian second shallowest ocean (3.8km average depth) Pacific

More information

ASEAN Trans-Boundary Marine Debris and Consortium for Indonesia Oceanic Research

ASEAN Trans-Boundary Marine Debris and Consortium for Indonesia Oceanic Research ASEAN Trans-Boundary Marine Debris and Consortium for Indonesia Oceanic Research Dr. Mutiara Rachmat Putri Research Group of Oceanography Institut Teknologi Bandung, INDONESIA Regional Workshop in support

More information

PLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence

PLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence Continental Drift PLATE TECTONICS E.B. Taylor (1910) and Alfred Wegener (1915) published on Continental Drift. Continental Drift Wegener s evidence 1. Fit of the Continents 2. Fossil Evidence 3. Rock Type

More information

Laboratory #7: Plate Tectonics

Laboratory #7: Plate Tectonics Materials Needed: 1. Pencil 2. Colored Pencils 3. Metric/Standard Ruler 4. Calculator 5. Tracing Paper Laboratory #7: Plate Tectonics Plate Tectonics The Earth is composed of layers. At the center is a

More information

Geologic Evolution of Latin America. Plate Tectonics: General Concepts & Applications to Latin America

Geologic Evolution of Latin America. Plate Tectonics: General Concepts & Applications to Latin America Geologic Evolution of Latin America Plate Tectonics: General Concepts & Applications to Latin America Structure of Earth: 3 major divisions of Core, Mantle, and Crust Upper mantle differs in the way that

More information

OSU Ocean Observing Center

OSU Ocean Observing Center OSU Ocean Observing Center and The Ocean Observatories Initiative OSU Retirement Association March 10,19 2016 2 Early Ocean Observations OSU Retirement Association March 10,19 2016 3 No information off

More information