4.7 Article

Deep Argo Reveals Bottom Water Properties and Pathways in the Australian-Antarctic Basin

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 126, Issue 12, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021JC017935

Keywords

abyssal ocean circulation; Antarctic Bottom Water; Deep Argo; water mass properties and variability

Categories

Funding

  1. Centre for Southern Hemisphere Oceans Research
  2. Australian Antarctic Program Partnership (AAPP) through Australian Government as part of the Antarctic Science Collaboration Initiative program
  3. Australian Government as part of the Antarctic Science Collaboration Initiative program
  4. Australian Government's National Environmental Science Program
  5. NOAA [NA15OAR4320071]
  6. MEXT of the Japanese Government [19K03981]
  7. European Union [821001]
  8. EQUIPEX NAOS project by French National Research Agency (ANR) [ANR-10-EQPX-40]
  9. Grants-in-Aid for Scientific Research [19K03981] Funding Source: KAKEN

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This study highlights the significance of Antarctic Bottom Water (AABW) in the climate system and the new perspective provided by the Deep Argo floats array for observing and studying this water mass. The research reveals the significant spatiotemporal variability in the properties of AABW, which plays a crucial role in climate change.
Changes in properties and quantity of Antarctic Bottom Water (AABW) have major implications for the climate system, through sequestration of heat and carbon into, and ventilation of, the abyssal ocean. Yet, it remains one of the most difficult water masses to observe. An array of 12 Deep Argo floats, capable of profiling from the surface to the seafloor and under sea ice, provides a new perspective on AABW in the Australian-Antarctic Basin. Over 2 years of data from the floats illuminate AABW properties with unprecedented detail, simultaneously sampling AABW at multiple locations, year-round, throughout the basin. Calibrating each float individually with nearby, quasi-simultaneous shipboard profiles ensures the highest quality salinity data, with estimated accuracy of +/- 0.005 or better. Pathways of Ross Sea and Adelie Land Bottom Water (RSBW and ALBW), defined by their unique temperature and salinity characteristics, are mapped along the continental slope from their respective sources. The main pathway of RSBW, identified by its characteristic deep salinity maximum, is inferred to be inshore of the 3,700 m isobath, where it cools and freshens westward along the slope before interacting with ALBW near 140 degrees E. A pulse of very cold and very fresh (nearly -0.6 degrees C, 34.82 g kg(-1)) ALBW appears in February 2019, highlighting temporal variability on daily scales near its source. Deep Argo has greatly enhanced our view of AABW in the Australian-Antarctic Basin and will prove to be an essential tool for monitoring future changes in the deep ocean by drastically increasing observations in a cost-effective way.

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