EIOURI Workshop No 1, 25-26 April 2013, JAMSTEC, Yokahama, Japan Notes taken by Nick D’Adamo during the Physical Oceanography Breakout Session on 26 April 2013 Session led by Weidong Yu The session aimed to condense the broad range of issues, items, ideas raised during the workshop into a more manageable smaller set of consolidated specific research objectives. There will be a position paper developed throughout the three workshops (Japan ~Apr 2013, Qingdao ~ Nov 2013 and Bergen ~June 2014). The position paper will include a ‘gap analysis’ based on the review of the progress of major historical research projects in the Indian Ocean and proposals to address the gaps. The paper itself, or a subsequent associated document, will constitute the EIOURI ‘Science and Implementation Plan’, which will be submitted to CLIVAR and IMBER for endorsement. The scientific motivation behind the Eastern Indian Ocean Upwelling Research Initiative is to look into the Eastern Indian Ocean coastal from the point of view of basin and/or global prospects. The key consolidated research objectives include the dynamic linkage between the Eastern Indian Ocean upwelling variations and the basin scale processes in the Indian Ocean and beyond, and the ecological and ecosystem impacts of the Eastern Indian Ocean Upwelling. o In this context a few sub-points were made: 1. The linkage, over various time scales (e.g. intra-seasonal to inter-annual), between the equatorial processes and the upwelling variations, where the Kelvin wave plays the central role. 2. Linkages between the open and coastal/marginal seas, with emphasis on the circulation transport of the mass and ecosystem characters from the Java-Sumatra upwelling region out to the open ocean. 3. Assessment of the Eastern Indian Ocean upwelling in CGCMs (e.g. CMIP-3 and CMIP-5). If bias, what is the consequence on climate modelling, prediction and projection? 4. What is the role of meso-scale eddy in transporting nutrient upward and offshore? Targeted field work will have to be a key aspect of EIOURI. Atmospheric processes will need to be incorporated in the research in terms of the two-way coupling between upwelling and atmospheric processes. ‘Feedback’ between Atmospheric forcings and SST is an issue. Multi-scale variations of upwelling off Java Sumatra, respectively, needs to be examined. Importance of the relationship between IOD and upwelling should be noted. Barrier Layer Dynamics is important. Need field observations to examine this issue. Microstructure measurements may be useful. Need to encourage tide data being recorded in the regions of interest to EIOURI to be made available by relevant Governments. The current EIOURI group requires a more balanced technical representation (noted in respect to the need to invite a wider spectrum of relevant scientists at forthcoming workshops), eg: o Modelling specialists. Noted that Western Australian / Australian modelling community has been active in modelling upwelling related dynamics. o (added note post workshop by Nick ... Dr Ming Feng (IOP) and Prof Chari Pattiaratchi Uni of Western Australia useful references in this context). o Vertical mixing specialists. Need to reconcile dynamics of vertical advection and vertical diffusion – potentially with complementary micro-structure measurements/analytical techniques – both to respectively support characterisation and modelling. o Noted that the Mirai has done this type of work. o Noted that vessels undertaking observations for moorings (eg RAMA) could easily accommodate vertical mixing specialists. Vertical dynamics (physical and bio-geochemical) in meso-scale eddies a key issue. o In this context, noted that Leeuwin Current eddies have received active attention (field an analytical, physical and biological) in research over the past decade. Special Volume of Deep Sea Research mentioned in this context. (added note post workshop by Nick - Deep Sea Research Part II: Topical Studies in Oceanography · Volume 54, Issues 8–10, April–May 2007...) o Also noted that IOP and SIBER both have specialists as members in this context. Internal Waves contribute to upwelling at the shelf – an issue for EIOURI. (added note post workshop by Nick – detailed IW research underway at University of Western Australia ... ref Prof Greg Ivey – laboratory, field and analytical research of IWs off NW Shelf of Australia). Noted that in respect to characterising the flux in the ITF, Australia (through IMOS Australia) has in place a line of six moorings between NW Australia and Timor Leste. To complement fully equipped vertical stations (moorings) in upwelling zones, mention was made of the potential use of cheap thermistor loggers on strings, with the potential to have greater coverage in cost-effective mode. Scoping would be required. Why does the MJO vary in intensity as it propagates past Indonesia?: noted that the MJO intensity has a local peak west of Sumatra, then locally reduces off Java, to increase again south of Bali – with the reasons for this unresolved. Related question – the mixed layer depth seems to vary along with this variability, with a question arising as to the role of the Barrier Layer in this context. Kelvin Waves and Rossby Waves and related equatorial / coastal linkages. Issues relating to reflection. Noted J McCreerey’s current investigations in this context. Need to resolve the differences between inter and intra-seasonal Kelvin Wave dynamics. Participants all emphasised the lack of coastal observation networks in the EIOURI context. o EIOURI should produce an aspirational observational plan (eg such as the IndOOS schematic from the IOP Implementation Plan) and this could/should also be submitted to IIOE-2 as a contribution. Important – critical that the physical considerations be developed and linked with those relating to the biology (ie from the complementary Biology breakout session of this workshop). Note importance of having a broad scope – to include social, economic, environmental considerations and/or relevancies of the EIOURI research. Source of nutrients...discern the flux pathways via the different types of nutrient transport (eg currents = advection; eddies = advection + upwelling) Temporal issues – time that upwellings keep nutrients in the photic zone Role of meso-scale eddies in larval dynamics. o Again – Deep Sea Research II a good reference. A key mystery and potential cross-cutting research focus for EIOURI is the issue of the S B F Tuna spawning area between Java / N W Australia. Why such a localised occurrence? What might the role of geographically idiosyncratic bio-physical processes be? Examine tagging data. This should/will be a major specific research focus for EIOURI. IIOE-2 and the role of EIOURI stakeholders to act as advocates for a high level coordination/imprimatur to be given to the IIOE-2. It was felt that this would be a positive development in that it would translate down as broad support for EIOURI in EIOURI participants’ respective countries.. o In this context, it was felt that a constructive option would be for such a proposition to be tabled at the IOC’s 27th Assembly meeting (25/6-5/7/13). o Specifically, this could well involve IOC taking on the principal driving/coordination role for IIOE-2 working in partnership with entities such as SCOR, IOGOOS etc. This would effectively equate to Intergovernmental endorsement. o The aspiration here would be that EIOURI members would then find it easier to advocate to other institutions in their own countries to become materially engaged in supporting EIOURI under the imprimatur that would be implied as part of the IOC endorsement of IIEO-2. o Workshop participants resolved to discuss this issue and advocate for the IOC endorsement model– they would speak to their own respective national IOC delegations on this issue. o Further discussion on this issue is planned for the IIOE-2 Reference Group meeting in Hyderabad 14-15 May 2013. The EIOURI context will be represented in those discussions (NB W Yu and Y Masumoto will be at the Hyderabad meeting). Securing dedicated shiptime for EIOURI was raised as a key issue. This would be a major discussion item at the Nov 2013 workshop (Qingdao). The form of the EIOURI report (as the major output from the three workshops) was discussed...its spectrum should be bio-physical. o A scientific paper was favoured. Weidong and Yukio will prepare a draft paper framework and distribute it for discussion after the Hyderabad IIOE-2 meeting. o Either it would constitute a Science and Implementation Plan for EIOURI or be the basis for one. o Discrete sections would have principal authors, with co-authorship. The next workshop and having a more balanced technical participant spread was discussed, including: o o o o Modellers Specialists in contemporary ocean observation techniques (eg gliders) Fisheries experts And others – as members advise or interest from new participants is received over the coming months Finally, it was emphasised that the EIOURI initiative should be open to all who are interested and that future workshops would be open. END