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 Home About Argo Argo in brief How Argo floats work Framework for entering Argo Guidelines for Argo floats The novel nature of Argo data Origins of Argo Future Argo International collaboration Argo Project Office Argo Regional Centers (ARC) Argo data Argo data and how to get it Argo data beginners guide Acknowledging Argo data Data products Data viewers Auxiliary directory Uses of Argo data Uses of Argo data Uses by operational centers Global research Research use Educational use Acknowledging Argo data Media Center Movies Photos Argo in Schools Float Deployment Stories Argo Story Map Documents Argo bibliography Argo research in press Thesis citation list Complete float bibliography Newsletter: Argonautics Argo user group reports Argo brochures Argo design papers News archive Argo Steering Team Argo Steering Team Members Meeting reports Meetings Links Google Earth layer FAQ Data FAQ Contact Site Map News Archive January 10, 2020 Annoucement of the 7th DMQC Core and Deep Workshop in Liverpool, the week of May 11- 15, 2020. December 19, 2019 Register now for the AST-21 meeting and OceanPredict Workshop hosted by UK Argo in Southampton the week of 16 - 20 March, 2020. December 17, 2019 Argo is in 55+ OceanObs19 papers published in Frontiers in Marine Science, volume 6! Argo bibliography , Argo in press and Argo thesis list updated. Inform argo@ucsd.edu of changes. November 13, 2019 Register until 31 Dec 2019 for the Arvor-Provor Float Technical Workshop hosted by Ifremer 28 - 30 January, 2020 in Brest, France November 8, 2019 Call for EGU abstracts for session on Sustained Ocean Observing and Paths Toward Improved Understanding and Modelling of Climate Abstract submission deadline: 15 January 2020 October 22, 2019 ADMT-20, BGC-ADMT-8 and Argo Visualization Workshop talks posted September 19, 2019 A new blob is spreading across the NW Pacific Ocean August 22, 2019 Garmin GPS problem on Teledyne/Webb and SeaBird floats July 22, 2019 BGC-Argo synthetic profiles are now being produced June 10, 2019 Mysterious holes in Antarctic sea ice explained by years of robotic data June 9, 2019 N2 and salinity anomaly plots from WHOI to help DMQC operators and DACs in identifying floats with high salinity drift. February 1, 2019 Revised notice of an error in pressure calibration of SBE Argo CTDs manufactured between September 2015 and June 2018 January 31, 2019 Statement from RBR on conductivity pressure correction for the 2000db conductivity cell. List of affected RBR cells by serial number December 10, 2018 Argo Story Map helps celebrate the 2 millionth Argo profile September 17, 2018 Message to Argo users about an increased occurrence of salinity erros in the real time Argo data stream What is Argo? Argo is a global array of 3,800 free-drifting profiling floats that measures thetemperature and salinity of the upper 2000 m of the ocean. This allows, for the first time, continuous monitoring of the temperature, salinity, and velocity of the upper ocean, with all data being relayed and made publicly available within hours after collection. Positions of the floats that have delivered data within the last 30 days : Maps displaying statistics about the Argo array, including its extensions into high latitudes and marginal seas, bio-geochemical sensors, communication systems, float type, etc., can be found in the map section on the Argo Information Centre website. Why do we need Argo? We are increasingly concerned about global change and its regional impacts. Sea level is rising at an accelerating rate of 3 mm/year, Arctic sea ice cover is shrinking and high latitude areas are warming rapidly. Extreme weather events cause loss of life and enormous burdens on the insurance industry. Globally, 8 of the 10 warmest years since 1860, when instrumental records began, were in the past decade. These effects are caused by a mixture of long-term climate change and natural variability. Their impacts are in some cases beneficial (lengthened growing seasons, opening of Arctic shipping routes) and in others adverse (increased coastal flooding, severe droughts, more extreme and frequent heat waves and weather events such as severe tropical cyclones). Understanding (and eventually predicting) changes in both the atmosphere and ocean are needed to guide international actions, to optimize governments' policies and to shape industrial strategies. To make those predictions we need improved models of climate and of the entire earth system (including socio-economic factors). Lack of sustained observations of the atmosphere, oceans and land have hindered the development and validation of climate models. An example comes from a recent analysis which concluded that the currents transporting heat northwards in the Atlantic and influencing western European climate had weakened by 30% in the past decade. This result had to be based on just five research measurements spread over 40 years. Was this change part of a trend that might lead to a major change in the Atlantic circulation, or due to natural variability that will reverse in the future, or is it an artifact of the limited observations? In 1999, to combat this lack of data, an innovative step was taken by scientists to greatly improve the collection of observations inside the ocean through increased sampling of old and new quantities and increased coverage in terms of time and area. That step was Argo. argo.avi is a float animation that explains the purpose and method of Argo. Where is Argo now? Argo deployments began in 2000, and by November 2007, the millionth profile was collected. Today, even with close to 4000 active floats, there are still some areas of the ocean that are over-populated while others have gaps that need to be filled with additional floats. Today's tally of floats is shown in the figure above and additional float statistics can be found here . To maintain the Argo array, national programs need to provide about 800 floats per year. The original global Argo array was designed for the open ocean excluding seasonal sea-ice zones and marginal seas. Thanks to both two-way communication and ice-sensing algorithms on floats, these technical limitations are largely mitigated. The concept of Argo has always been of a spatially complete global array. Therefore, including seasonal sea-ice zones and marginal seas moves the target number of Argo floats from 3000 to 3800. In addition to the globalization of core Argo described above, there are several Argo enhancements that are in various stages of development and implementation. These include extended coverage to the ocean bottom, additional floats equipped with bio-geochemical sesnors, and enhanced spatial coverage in boundary current regions and equatorial regions. Besides float deployment, Argo has worked hard to develop two separate data streams: real time and delayed mode. A real time data delivery and quality control system has been established that delivers 90% of profiles to users via two global data centers (GDACs) within 24 hours. A delayed mode quality control system (DMQC) has been established and 65% of all eligible profiles have had DMQC applied. Float reliability has improved almost every year and the float lifetime has been extended. Argo has developed a large user community in universities, government labs and meteorological/climate analysis/forecasting centers. The need for global Argo observations will continue indefinitely into the future, though the technologies and design of the array will evolve as better instruments are built, models are improved, and more is learned about ocean variability. -- Who Collaborates with Argo? Argo is a major contributor to the WCRP 's Climate Variability and Predictability Experiment ( CLIVAR ) project and to the Global Ocean Data Assimilation Experiment ( GODAE ). The Argo array is part of the Global Climate Observing System/Global Ocean Observing System OceanView GCOS / GOOS )....