Argo world 

News Archive
June 26, 2020 Register now for the Arctic and Baltic Users Workshop
hosted by the Institute of Oceanology Polish Academy of Sciences in Sopot, Poland on 23 - 25 September 2020
June 5, 2020 Working session on how to import data from Argovis into your programming environment of choice: Friday 26 June at 1 pm MT. The session is free, yet please register here
May 11, 2020 Argo releases an environmental impact statement
April 15, 2020 A series of papers has recently been published on the dynamic corrections to the SBE CTD.
April 14, 2020 Paper from RBR describing dynamic corrections for RBRArgo 2000dbar combined conductivity cell
March 26, 2020 AST-21 meeting in Southampton canceled
A series of three virtual meetings will occur during the week of April 13 - 20, 2020 to address some of the topics from the AST-21 draft agenda. Check the AST-21 meeting page for more information and updates.
March 25, 2020 Argo bibliography, Argo in press updated. Argo thesis list to be updated soon.
Inform of changes.
March 25, 2020 Register now for the ADMT-21 meeting in Miami, FL: 29 November - 4 December, 2020
Hotel information coming soon
March 11, 2020 7th DMQC Core and Deep Workshop postponed
Originally planned for the week of May 11- 15, 2020 in Liverpool. No new dates set. Please stay tuned for more information.
February 18, 2020 Save the date for the Baltic and Arctic Argo Workshop in Sopot, Poland, 23 - 25 September, 2020.
February 7, 2020 Arvor/Provor float technical workshop outcomes posted
December 17, 2019 Argo is in 55+ OceanObs19 papers published in Frontiers in Marine Science, volume 6!
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
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 animationargo.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).