ࡱ>    #` 0HIbjbj\.\. |>D>DH@$*V8V8V8P8<8*[^z9z9L999:::ژܘܘܘܘܘܘ$h!H?::H?H?99DDDH?99ژDH?ژDDJv\"9n9 0XE|V8AґBF+0[7B7"7"$::;C<s=:::CX:::[H?H?H?H?*$NND%*NN%*** World Meteorological Organization Intergovernmental Oceanographic Commission    Joint WMO-IOC Technical Commission for Oceanography and Marine Meteorology Second Session of the JCOMM Observations Coordination Group Geneva, Switzerland, 23-25 April 2007 NWP, CBS EXPERT TEAM ON THE EVOLUTION OF THE GLOBAL OBSERVING SYSTEM (ET-EGOS) (Agenda Item 3.4) Submitted by the WMO Secretariat This document is also submitted to the SOT-IV meeting, Geneva, 16-21 April 2007. Action required: The OCG in invited to take the ET-EGOS and Management Committee recommendations into account. 1. The second session of the CBS Expert Team on the Evolution of the Global Observing System (ET-EGOS) was held in Geneva, 10-14 July 2006. Prior to the meeting, the JCOMM Statement of Guidance for JCOMM Program Areas was reviewed and updated by the WMO Secretariat, Eric Lindstrom and Jean-Louis Fellous. The revised version dated June 2006 was presented to the meeting (see Appendix). 2. Meeting outcome and actions relevant to JCOMM: JCOMM statement of guidance needs to be refined. The following approach was proposed by the meeting: JCOMM to designate a focal point for user requirements (i.e. ocean mesoscale forecast and coastal marine services) as well as a focal point for estimating in situ observing systems capabilities (e.g. JCOMMOPS). There is no need for a JCOMM satellite expert as ET-EGOS has already sufficient expertise in this regard. In order to update its SoG, JCOMM will have to (i) update the CEOS/WMO database with regard to new requirements such as for Tsunami Monitoring as part of Coastal services, and to instrument performances of in situ components, (ii) conduct Rolling Review of Requirements (RRR) process and make use of Critical Review Charts while taking existing JCOMM metrics into account, (iii) consider JCOMM/OCG phased in implementation plan, and (iv) stress on gap analysis, including the need to provide for long term sustainability of the observational networks. New SoG should be submitted prior to the next ET-EGOS meeting in mid-2007. Etienne Charpentier can act as a focal point regarding SoG future updates. ASAP programme is regarded as complementary to AMDAR as a source of in situ Aerological profiles (AMDAR provides for little ascents and descents over the oceans). Despite high cost of maintaining ASAP programme, EUMETNET continues to operate it and is even targeting 5000 ASAP profiles yearly within its E-ASAP programme (North Atlantic and Mediterranean Sea). Transmission of higher vertical resolution profiles remains a priority and has telecommunication costs as well as migration to table driven code forms impacts. JCOMM was asked to investigate development of ASAP programmes in ocean areas with poor radiosondes coverage and to propose solutions for increasing vertical resolution of the transmitted profiles. ET-EGOS is concerned with observing programmes sustainability, including Argo, and extension of tropical mooring arrays in the Atlantic and Indian Oceans. JCOMM was invited to communicate Argo demonstrated benefits to its Member Countries/States. OOPC is invited to to provide up to date information regarding complementarity of in situ upper ocean thermal networks. Real-time distribution of Essential Climate Variables (ECV) as defined in the GCOS implementation plan should be pursued. Statements of Guidance for NWP and Seasonal to Inter-Annual Forecasts should now reflect dramatic improvements with regard to in situ SST data thanks mainly to the completion of the surface drifting buoy networks. Impact studies of surface pressure drifter networks was proposed, e.g. impact of Northern Hemisphere data density versus Southern Hemisphere. The goal is to investigate whether it will be required to equip all SH drifters with barometers. For sea surface winds, guidance is required regarding the impact on applications of having 1 scatterometer plus one or two microwave imagers rather than two scatterometers on LEO. Eric Lindstrom will be invited to provide input. SHIP security issue following WMO EC-58 resolution: JCOMM was asked to work with members to overcome the generic SHIP call sign issued to ensure that quality monitoring and feedback activities can continue to be undertaken. DBCP asked to pursue improvement of data timeliness of drifter data especially in the South Atlantic and SouthEast Pacific Oceans. Higher satellite data rate transmissions remains a topic of interest and JCOMM is asked to pursue pro-active action in this regard. IABP, IPAB, IPY: Impact of expected increased ice buoy deployment should be reviewed at the next OSE/OSSE workshop. 3. At its fifth Session, the JCOMM Management Committee, Geneva, October 2006, noted the outcome from the Second Session of the CBS Expert Team on the Evolution of the Global Observing System. The Committee agreed that the SoG should be regularly reviewed by the JCOMM, thanks primarily to the designation of: (i.) a focal point for user requirements (i.e., ocean mesoscale forecasts and coastal marine services, including tsunami monitoring), and (ii.) a focal point for estimating in situ observing system capabilities. The Committee designated Dr Craig Donlon and Ms Hester Viola as the respective focal points. The Committee agreed that a specific section for marine services should be developed in the WMO CEOS database (action: SPA). 4. MAN-V agreed that the JCOMM must participate more actively in the ET-EGOS Rolling Review of Requirements (RRR) process, and to make use of its Critical Review Charts while taking existing JCOMM metrics and other tools into account, and stressing observing system deficiencies. The Committee tasked the SPA to designate a focal point to liaise with the WMO Secretariat and provide input on the issue (action: SPA). The new SoG should be submitted by mid-2007 prior to the next ET-EGOS meeting. 5. MAN-V agreed that the ASAP Programme should be regarded as complementary to the AMDAR Programme, as a source of in situ aerological profiles (AMDAR provides for few ascents and descents over the oceans). The Committee asked the OPA and its SOT to address this issue (action: OPA and its SOT). 6. MAN-V noted the request by the ET-EGOS to provide the JCOMM with input on requirements for satellite sea surface winds, as well as guidance regarding the impact on applications of scatterometers and microwave imagers. It asked the Cross-cutting Team on Satellite Data Requirements to provide input (action: Cross-cutting Team on Satellite Data Requirements). 7. The OCG in invited to take the ET-EGOS and Management Committee recommendations into account. APPENDIX 3.8 Statement of Guidance for JCOMM Program Areas (June 2006) 3.8.1 Background The joint WMO-IOC Technical Commission for Oceanography and Marine Meteorology (JCOMM), at its second session in Halifax, 19-27 September 2005, noted the participation of its satellite rapporteur and JCOMMOPS in the work of the ET-ODRRGOS and contribution to that process. The Commission requested that this work be pursued with ET on Evolution of the GOS (ET-EGOS), through one or more experts designated by the co-Presidents, and that the existing statement of guidance relating to marine user requirements be updated, published as a JCOMM technical report and widely distributed. The Commission also requested the Services Programme Area Coordinator to ensure that eventually a clear set of observational data requirements to support marine meteorological and operational oceanographic products and services be finalized and included in the CEOS/WMO database. This document describes application areas relating to the JCOMM activities. Observation variables used for the application areas are listed as well as their observing systems. 3.8.2 JCOMM Applications Areas One of the important roles of JCOMM is to be an efficient mechanism for coordinating and integrating marine observation systems. JCOMM will provide a consistent framework for the collection, archival, distribution, and utilization of data collected at sea for oceanographic and meteorological applications. There are four major application areas relevant to JCOMM: (a) Numerical Weather Prediction, NWP, (b) Ocean Mesoscale Forecast, OMF, (c) Seasonal to Inter-annual Forecast, SIA, and (d) Coastal Marine Services. NWP uses the marine meteorological parameters to initialise the numerical models, and the SST distribution becomes one of the most important boundary condition. OWF and SIA predict future ocean status using numerical models, but the former target is higher frequency components (a week to a month) of ocean variability and the latter the lower frequency components (seasonal and inter-annual). Two of the four application areas are described in the other documents (ET-EGOS) and specific JCOMM requirements in this regard were taken into account. NWP has been discussed in the previous Statement of Guidance (sections 3.1 and 3.2). Seasonal and Inter-annual Forecasts consider both the atmospheric and oceanic lower-frequency variation using coupled numerical models, which is described in the SIA SoG found in section 3.5. The ocean community has produced a widely-agreed and endorsed plan for the next five to ten years, incorporated into the Implementation Plan for the Global Observing System for Climate in support of the UNFCCC (GCOS-92). Therefore, the statement of guidance presented below refers to the following application areas, Ocean Mesoscale Forecast and Coastal Marine Services. OMF is now designed and implemented by a GOOS/GCOS OOPC pilot project, Global Ocean Data Assimilation Experiment (GODAE). Integrating existing and near future ocean observation systems, near-operational ocean mesoscale forecast is or will be conducted in the GODAE project. Demonstration phase of GODAE started in 2003. Coastal Marine Services include the traditional tasks of the JCOMM community. However, the social needs have increased and become diversified, which forces JCOMM community to redesign the observing systems including backbone GOSs (e.g.,GOOS/Coastal Ocean Observing Panel). 3.8.3 Ocean Mesoscale Forecasts Increasing ocean information from the remote sensing methods enables us to predict high-frequency components of ocean variability, i.e., ocean mesoscale forecasts. On the basis of traditional ocean observation components for NWP and monitoring of the low frequency variability (e.g., in situ platform based observing system), new in situ and satellite observations will be integrated to realize operational ocean nowcasting and forecasting in the near future. The ocean observation data are now being assimilated into numerical forecast models. Important observation variables and their present global ocean observing systems are listed in the table below. Observation variablesObserving System Temperature/salinity profiles Tropical mooring buoy (TIP) XBTs (SOOP) Profiling floats (Argo) Sea Surface Height Satellite Altimeter Tide Gauges (GLOSS) High-resolution SST Infrared, Microwave radiometers combined with in situ drifter (DBCP) and ship (VOSP) data  In order to generate the forecasting products, the observed data must be delivered to forecasting centres in timely manner. The boundary conditions for deriving the ocean forecast model are provided by the NWP products, which are generated by the atmospheric numerical model using the marine meteorological observation data as mentioned above. 3.8.4 Coastal Marine Services With respect to Marine Meteorology, nowcasts and forecasts of sea state (wave environment), ocean surface topography, fog, sea ice and coastal circulation are of critical importance to safe and efficient marine operations including shipping, port operations, search and rescue operations, fishing, recreational boating, swimming, and the extraction of natural resources, etc. Coastline Changes are constantly occurring due to eroding and accreting from routine and episodic events associated with tides, winds, waves, storm surges, sediment re-suspension and transport by rivers, tectonic processes and human modifications of the coastal zone. Marine Pollution involves monitoring polluted sea areas (i.e., oil spill, red tide, high sediment concentration, etc.) that are drifted by surface, near sub-surface and wind-driven currents. Detections of the polluted area and fields involved in fate and weathering processes are required for mitigation of their influence on the coastal environment. In order to provide useful information (products) for the society living in/relating to the coastal region, we need various observational data not only the marine meteorological (physical) variables but also geological/biological variables. The following lists some (but not all) of the important marine meteorological parameters: SST, air temperature, air pressure, surface wind, air humidity, surface wave, temperature/salinity profiles, currents, sea ice, river discharge, coast lines, bathymetry, etc. The coastal variables are traditionally observed by the in situ observing systems. The variables and their observing systems are described in the table below. Observation variables Observing System Wind, Wave height/direction/spectrum Surface meteorological data Subsurface oceanographic data (Temperature, salinity currents) Wind/Wave Moored Buoy Ships and/or marine platforms Small moored buoy, Ships (XBTs), drifters with thermistor strings, ADCP  Satellite observations are also useful for MS as well as the other ocean application areas. Satellite observations with higher temporal and spatial resolutions are required for MS because its major activities are carried out in the coastal seas. Concerning the requirements for the coastal phenomena, potential satellite products for MS are high-resolution coastal wind, high-resolution SST, and high-resolution ocean colour. Potential of very high-spatial resolution sensors for JCOMM programme areas is pointed out. High-resolution coastal wind: The surface wind is a key parameter to nowcast and forecast of the coastal marine meteorological and oceanic conditions. It is strongly influenced by the coastal topography and land-sea surface conditions. Traditional global/regional NWP products do not have enough spatial resolution for MS. The microwave scatterometer has limited spatial resolution (25km), and the wide swath SAR measurement has limited temporal resolution (one measurement every few days) and provides no wind direction. High-resolution sea surface temperature: SST in the coastal region has a large variability due to the diurnal cycle of solar radiation, which enhances surface characteristics of the land and sea and forces land-air-sea interactions, i.e., land-sea breezes. High-resolution SSTs (1 km) can be retrieved by the LEO infrared radiometer and rather degraded resolution SSTs (5 km) from the GEO IR radiometer. However, quantitative detection of the SST diurnal cycle is still challenging subject but drifters can provide high temporal resolution SST data. In contrast, microwave radiometers cannot be used for the coastal applications because of (a) rather coarse spatial resolution and (b) contamination of land signals in the measurement in the coastal sea. High-resolution ocean colour: The ocean colour remote sensing provides images of biological/non-biological parameters with high-spatial resolution of 250m to 1 km. The ocean colour can detect several types of marine pollutions and harmful biological activities. Parameter retrieval algorithm in turbid waters is not established yet, but developments of an observation system based on the OC remote sensing have presented promising results for a future operational observing system. Very high-resolution visible/infrared imagers (i.e., Landsat, Spot) and synthetic aperture radar (SAR): These provide information on the coastline, which gradually changes through erosion and accretion processes relating to coastal meteorological/oceanic phenomena. However, their images are rather expensive and not freely available to the community. In order to design efficient observing system for MS in the near-coast sea region, a mechanism to incorporate these high-resolution images needs to be discussed.     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