Adding Oxygen to Argo: Developing a Global in-situ Observatory for Ocean Deoxygenation and Biogeochemistry

We propose to add dissolved oxygen sensors to the Argo float program in order to determine, on a global-scale, seasonal to decadal time-scale variations in dissolved oxygen concentrations throughout the upper ocean. Such observations are especially important to document the ocean’s expected loss of oxygen as a result of ocean warming, but there are many other benefits including the opportunity to estimate net community and export production, the assessment of changes in low oxygen regions, and improved estimates of the oceanic uptake of anthropogenic CO2. The proposed joint Argo-Oxygen program is made possible by the recent development of dissolved oxygen sensors that are both precise and stable over extended periods and can be easily integrated with the currently used Argo floats. Results from the more than 200 oxygen equipped Argo float have not only demonstrated the feasibility of the program, but also produced already many insights and discoveries. Achieving the main goal of the Argo-Oxygen program does not require any appreciable changes in the deployment and operating strategies of the current Argo program and can therefore be implemented without a significant impact on Argo’s core mission. A two-phase implementation is proposed, consisting of a small set of regional pilot-studies, followed by a build-up toward a global implementation. The cost of adding oxygen sensors to all floats of the Argo program is estimated to be about USD 4.2 million per year. The proposed Argo-Oxygen program will add substantial value to Argo by expanding the number of Argo data users, as well as by creating new synergies between the physical and the biogeochemical ocean research communities. The new observations will also contribute to the activities of various international networks and partnerships for Earth Observing Systems.

[1]  Johannes Karstensen,et al.  Age determination of mixed water masses using CFC and oxygen data , 1998 .

[2]  O. Ulloa,et al.  Warming and circulation change in the eastern South Pacific Ocean , 2000 .

[3]  C. Deutsch,et al.  Physical-biological interactions in North Pacific oxygen variability , 2006 .

[4]  C. D. Keeling,et al.  Seasonal and long‐term dynamics of the upper ocean carbon cycle at Station ALOHA near Hawaii , 2004 .

[5]  David S. Fox,et al.  Upwelling-driven nearshore hypoxia signals ecosystem and oceanographic changes in the northeast Pacific , 2004, Nature.

[6]  Y. Watanabe,et al.  Probability of a reduction in the formation rate of the subsurface water in the North Pacific during the 1980s and 1990s , 2001 .

[7]  Patrick F. Cummins,et al.  Argo : A new tool for environmental monitoring and assessment of the world's oceans, an example from the N. E. Pacific , 2005 .

[8]  H. Garcia,et al.  Decadal-scale chemical variability in the subtropical North Atlantic deduced from nutrient and oxygen data , 1998 .

[9]  Stephen C. Riser,et al.  Chemical Sensor Networks for the Aquatic Environment , 2007 .

[10]  Hervé Claustre,et al.  Bio-optical profiling floats as new observational tools for biogeochemical and ecosystem studies: Potential synergies with ocean color remote sensing , 2010 .

[11]  H. Bryden,et al.  Decadal Changes in the South Indian Ocean Thermocline , 2005 .

[12]  Nicolas Gruber,et al.  Ocean deoxygenation in a warming world. , 2010, Annual review of marine science.

[13]  F. Joos,et al.  Revision of the global carbon budget due to changing air‐sea oxygen fluxes , 2002 .

[14]  S. Doney,et al.  A modeling study of the seasonal oxygen budget of the global ocean , 2007 .

[15]  K. Koltermann,et al.  How much is the ocean really warming? , 2007 .

[16]  D. Wallace Storage and Transport of Excess CO 2 in the Oceans: the JGOFS/WOCE Global CO 2 Survey , 2001 .

[17]  F. Nansen,et al.  The Norwegian Sea : its physical oceanography based upon the Norwegian researches 1900-1904 , 1910 .

[18]  C. Wunsch,et al.  Oceanic nutrient and oxygen transports and bounds on export production during the World Ocean Circulation Experiment , 2002 .

[19]  Jon Turton,et al.  Argo –Sounding the oceans , 2006 .

[20]  Scott C. Doney,et al.  The ARGO-Oxygen Program - A white paper to promote the addition of oxygen sensors to the international Argo float program , 2007 .

[21]  C. Benitez‐Nelson,et al.  A time-series study of particulate matter export in the North Pacific Subtropical Gyre based on 234Th : 238U disequilibrium , 2001 .

[22]  A. Hirst,et al.  Long‐term changes in dissolved oxygen concentrations in the ocean caused by protracted global warming , 2003 .

[23]  Stephen C. Riser,et al.  Net production of oxygen in the subtropical ocean , 2008, Nature.

[24]  Ralph F. Keeling,et al.  Seasonal and interannual variations in atmospheric oxygen and implications for the global carbon cycle , 1992, Nature.

[25]  J. Sprintall,et al.  Expanding Oxygen-Minimum Zones in the Tropical Oceans , 2008, Science.

[26]  A. Kasai,et al.  Flow structure and hypoxia in Hiuchi-nada, Seto Inland Sea, Japan , 2007 .

[27]  R. Slater,et al.  Possible biological or physical explanations for decadal scale trends in North Pacific nutrient concentrations and oxygen utilization , 2001 .

[28]  L. A. Anderson,et al.  Global ocean phosphate and oxygen simulations , 1995 .

[29]  Stefan Sommer,et al.  Evaluation of a lifetime‐based optode to measure oxygen in aquatic systems , 2006 .

[30]  N. Bindoff,et al.  Decadal Changes along an Indian Ocean Section at 32°S and Their Interpretation , 2000 .

[31]  Scott C. Doney,et al.  Seasonal variations in the atmospheric O2/N2 ratio in relation to the kinetics of air‐sea gas exchange , 1998 .

[32]  Ralph F. Keeling,et al.  THE CHANGE IN OCEANIC 02 INVENTORY ASSOCIATED WITH RECENT GLOBAL WARMING , 2022 .

[33]  A. Manning,et al.  Atmospheric potential oxygen: New observations and their implications for some atmospheric and oceanic models , 2006 .

[34]  A. Hirst,et al.  Changes in dissolved oxygen in the Southern Ocean with climate change , 2000 .

[35]  R. Keeling,et al.  TRANSPORT OF HEAT, CO2 AND O2 BY THE ATLANTIC'S THERMOHALINE CIRCULATION , 1995 .

[36]  F. A. Richards,et al.  The influence of organisms on the composition of sea-water , 1963 .

[37]  M. Tomczak Some historical, theoretical and applied aspects of quantitative water mass analysis , 1999 .

[38]  M. Tomczak,et al.  Detecting changes in Labrador Sea Water through a water mass analysis of BATS data , 2005 .

[39]  J. Holfort,et al.  Meridional transport of dissolved inorganic carbon in the South Atlantic Ocean , 1998 .

[40]  T. Saino,et al.  Temporal increases of phosphate and apparent oxygen utilization in the subsurface waters of western subarctic Pacific from 1968 to 1998 , 2001 .

[41]  J. Lubchenco,et al.  Emergence of Anoxia in the California Current Large Marine Ecosystem , 2008, Science.

[42]  C. D. Keeling,et al.  Carbon-13 constraints on the seasonal inorganic carbon budget at the BATS site in the northwestern Sargasso Sea , 1998 .

[43]  Walker O. Smith,et al.  Temperature effects on export production in the open ocean , 2000 .

[44]  Martin Heimann,et al.  Global and hemispheric CO2 sinks deduced from changes in atmospheric O2 concentration , 1996, Nature.

[45]  A. Körtzinger Oceanic oxygen - the oceanographer's canary bird of climate change , 2006 .

[46]  R. Keeling,et al.  Mean annual cycle of the air‐sea oxygen flux: A global view , 2000 .

[47]  E. Maier‐Reimer,et al.  Impact of circulation on export production, dissolved organic matter and dissolved oxygen in the ocean: Results from OCMIP-2 , 2007 .

[48]  A. Manning,et al.  Global oceanic and land biotic carbon sinks from the Scripps atmospheric oxygen flask sampling network , 2006 .

[49]  G. Johnson,et al.  Decadal water mass variations along 20°W in the Northeastern Atlantic Ocean , 2007 .

[50]  A. Defant,et al.  Schichtung und Zirkulation des Atlantischen Ozeans , 1936 .

[51]  A. Körtzinger,et al.  The Ocean Takes a Deep Breath , 2004, Science.

[52]  Timothy P. Boyer,et al.  Warming of the world ocean, 1955–2003 , 2005 .

[53]  F. Joos,et al.  Trends in marine dissolved oxygen: Implications for ocean circulation changes and the carbon budget , 2003 .

[54]  M. Heimann,et al.  Testing global ocean carbon cycle models using measurements of atmospheric O2 and CO2 concentration , 1998 .

[55]  D. Wilbur,et al.  O2, Ar, N2, and 222Rn in surface waters of the subarctic Ocean: Net biological O2 production , 1991 .

[56]  T. Stocker,et al.  An improved method for detecting anthropogenic CO2 in the oceans , 1996 .

[57]  Two decades of ocean CO2 sink and variability , 2003 .

[58]  R. Keeling,et al.  Analysis of the mean annual cycle of the dissolved oxygen anomaly in the World Ocean , 1997 .

[59]  S. Levitus,et al.  Warming of the World Ocean , 2000 .

[60]  R WOLF,et al.  Continuous recording of blood oxygen tensions by polarography. , 1953, Journal of applied physiology.

[61]  Arne Körtzinger,et al.  High Quality Oxygen Measurements from Profiling Floats: A Promising New Technique , 2005 .

[62]  M. Gloor,et al.  Air‐sea flux of oxygen estimated from bulk data: Implications For the marine and atmospheric oxygen cycles , 2001 .

[63]  L. W. Winkler,et al.  Die Bestimmung des im Wasser gelösten Sauerstoffes , 1888 .

[64]  Reiner Schlitzer,et al.  Applying the Adjoint Method for Biogeochemical Modeling: Export of Participate Organic Matter in the World Ocean , 2013 .

[65]  M. V. Hood,et al.  Ship-based Repeat Hydrography: A strategy for a sustained global programme: A Community White Paper , 2010 .

[66]  H. Ducklow,et al.  Annual flux of dissolved organic carbon from the euphotic zone in the northwestern Sargasso Sea , 1994, Nature.

[67]  R. Eugene Turner,et al.  Coastal Hypoxia: consequences for living resources and ecosystems , 2001 .

[68]  W. J. Jenkins,et al.  The subtropical nutrient spiral , 2003 .

[69]  D. Gilbert,et al.  A seventy‐two‐year record of diminishing deep‐water oxygen in the St. Lawrence estuary: The northwest Atlantic connection , 2005 .

[70]  S. Emerson,et al.  Constraining bubble dynamics and mixing with dissolved gases: Implications for productivity measurements by oxygen mass balance , 2006 .

[71]  Patrick Lehodey,et al.  Integrating biogeochemistry and ecology into ocean data assimilation systems , 2009 .

[72]  C. Deutsch,et al.  Fingerprints of climate change in North Pacific oxygen , 2005 .

[73]  D. Stephenson,et al.  Granger Causality of Coupled Climate Processes: Ocean Feedback on the North Atlantic Oscillation , 2006 .

[74]  John Gould,et al.  Argo profiling floats bring new era of in situ ocean observations , 2004 .

[75]  R. Service New Dead Zone Off Oregon Coast Hints at Sea Change in Currents , 2004, Science.

[76]  T. Ono,et al.  Temporal Trends in Apparent Oxygen Utilization in the Upper Pycnocline of the North Pacific: 1980–2000 , 2004 .

[77]  W. Spitzer Rates of vertical mixing, gas exchange, and new production : estimates from seasonal gas cycles in the upper ocean near Bermuda , 1989 .