A circumpolar current becomes possible
node
The opening of Drake Passage and the deepening of the Tasman gateway removed the last land barriers between the Atlantic, Pacific and Indian oceans at southern high latitudes, allowing an unbroken eastward current around Antarctica. When this happened is genuinely disputed: estimates cluster around the Eocene–Oligocene transition near 34 Ma, around 31 Ma from foraminiferal and neodymium evidence, near 30 Ma from gateway–westerly alignment arguments, and near 24 Ma from flow-speed and water-mass homogeneity records, while a 2023 study argues the modern ACC was not established until the late Miocene. The pack states the disagreement rather than choosing.
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Timeline
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Connections · 3
- Antarctic Circumpolar Current (ACC)concerns
- Drake Passageconcerns
- Southern Oceanconcerns
Assembled narrative · 1
Assembled from 50 blocks · 1 evidence · 83 related
- Story
- The opening of Drake Passage and the deepening of the Tasman gateway removed the last land barriers between the Atlantic, Pacific and Indian oceans at southern high latitudes, allowing an unbroken eastward current around Antarctica. When this happened is genuinely disputed: estimates cluster around the Eocene–Oligocene transition near 34 Ma, around 31 Ma from foraminiferal and neodymium evidence, near 30 Ma from gateway–westerly alignment arguments, and near 24 Ma from flow-speed and water-mass homogeneity records, while a 2023 study argues the modern ACC was not established until the late Miocene. The pack states the disagreement rather than choosing.
- Knowledge
- Antarctic Circumpolar Current (ACC)
- Southern Ocean
- Drake Passage
- A circumpolar current becomes possible
- Connections
- Antarctic Circumpolar Current (ACC)
- Drake Passage
- Southern Ocean
- 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
- 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
- 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
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/atlas?object=EVT_ACC_ONSET&experience=EVT_ACC_ONSET