Antarctic Circumpolar Current (ACC)
node · earth · Southern Ocean — circumpolar
The largest current on Earth and the only one that circles the globe without meeting a coastline. Driven by the strongest sustained westerlies on the planet and unblocked by land, it runs eastward around Antarctica and connects the Atlantic, Pacific and Indian basins into one system — which is what makes a global overturning circuit possible at all. Continuous measurements in Drake Passage from 2007 to 2011 gave a mean transport of 173.3 Sv, the sum of a mean barotropic component of 45.6 ± 8.9 Sv and a baroclinic component of 127.7 Sv relative to zero at the seafloor. That total is about 30 per cent larger than the 134 Sv figure that had served as the benchmark for climate models for decades.
Read in · 1
Evidence · 2
Timeline
No dated observations are stored for this object. Atlas shows what was observed and when — it does not infer a history.
Connections · 4
- Atlantic Meridional Overturning Circulation (AMOC)comparable_to
- Drake Passageconstrained_by
- Southern Oceanlocated_in
- Drake Passagepasses_through
Assembled narrative · 1
Assembled from 61 blocks · 2 evidence · 88 related
- Story
- The largest current on Earth and the only one that circles the globe without meeting a coastline. Driven by the strongest sustained westerlies on the planet and unblocked by land, it runs eastward around Antarctica and connects the Atlantic, Pacific and Indian basins into one system — which is what makes a global overturning circuit possible at all. Continuous measurements in Drake Passage from 2007 to 2011 gave a mean transport of 173.3 Sv, the sum of a mean barotropic component of 45.6 ± 8.9 Sv and a baroclinic component of 127.7 Sv relative to zero at the seafloor. That total is about 30 per cent larger than the 134 Sv figure that had served as the benchmark for climate models for decades.
- Knowledge
- Atlantic Meridional Overturning Circulation (AMOC)
- Antarctic Circumpolar Current (ACC)
- Southern Ocean
- Drake Passage
- Connections
- Antarctica
- Antarctic Polar Front (Antarctic Convergence)
- Atlantic Meridional Overturning Circulation (AMOC)
- Drake Passage
- Southern Ocean
- Drake Passage
- A circumpolar current becomes possible
- Drake Passage is measured and the ACC turns out to be larger
- Gulf Stream
- Thermohaline Circulation
- Antarctic Circumpolar Current (ACC)
- North Atlantic Deep Water (NADW)
- RAPID-MOCHA-WBTS Array at 26.5°N
- Overturning in the Subpolar North Atlantic Program (OSNAP)
- Meridional Ocean Heat Transport
- The RAPID array begins continuous AMOC measurement at 26.5°N
- OSNAP moves the engine room out of the Labrador Sea
- IPCC AR6 assesses AMOC decline as very likely and collapse as unlikely this century
- A statistical early-warning analysis puts an AMOC collapse mid-century
- A physics-based early warning signal is proposed
- Twenty-two years of continuous AMOC observation
- Antarctic Circumpolar Current (ACC)
- Antarctic Circumpolar Current (ACC)
- A circumpolar current becomes possible
- Drake Passage is measured and the ACC turns out to be larger
- Antarctic Blue Whale (B. m. intermedia)
- Antarctic Summer Feeding Migration
- South Georgia
- Southern Ocean Whale Sanctuary
- Seasonal Krill Aggregation
- The factory ship Lancing takes a stern slipway south
- The Antarctic blue whale catch reaches its all-time peak
- The Southern Ocean Whale Sanctuary is adopted
- Dedicated Antarctic Blue Whale Project voyages
- Baleen whale consumption is re-measured, and the krill paradox sharpens
- The only published Antarctic blue whale satellite tracks are released as data
- Antarctic Krill (Euphausia superba)
- Arctic Tern (Sterna paradisaea)
- CCAMLR is agreed at Canberra
- A long-term decline in krill density is linked to winter sea ice
- CCAMLR adopts the Ross Sea marine protected area
- Antarctic sea ice reaches a record low, a year after the previous one
- Antarctic Circumpolar Current (ACC)
- Antarctica
- Thermohaline Circulation
- North Atlantic — Grand Banks approaches
- Weddell Sea
- A circumpolar current becomes possible
- Antarctic meltwater is projected to slow the abyssal cell
- A physics-based early warning signal is proposed
- Evidence
- Continuous Drake Passage observations from 2007 to 2011 give a mean ACC transport of 173.3 Sv — barotropic 45.6 ± 8.9 Sv plus baroclinic 127.7 Sv relative to zero at the seafloor — about 30 per cent above the canonical benchmark value. Figures taken from search summaries of the abstract; the article is on a blocked publisher domain.
- The timing of ACC onset is contested: this paper places the modern ACC in the late Miocene, while other studies place onset near the Eocene–Oligocene transition (~34 Ma), at ~31 Ma from foraminiferal and neodymium evidence, at ~30 Ma from Tasmanian gateway–westerly alignment, and at ~24 Ma from flow-speed and water-mass homogeneity records. The disagreement is stated, not resolved; none of the papers was fetched.
Observed changes · 0
No public Signals are attached to this object. Signals show what changed and when it was observed — never a direction or a rank.
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