Conservation Constraints and Distributed Advective Memory in a Reduced Model of Atlantic Overturning Hysteresis

@misc{herho2026conservation,
  title = {{Conservation Constraints and Distributed Advective Memory in a Reduced Model of Atlantic Overturning Hysteresis}},
  author = {Sandy Hardian Susanto Herho and Iwan Pramesti Anwar and Mutiara Rachmat Putri and Rusmawan Suwarman and Deny Juanda Puradimaja and Dasapta Erwin Irawan},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.24000},
  eprint = {2609.24000},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.24000},
}

TY  - UNPB
TI  - Conservation Constraints and Distributed Advective Memory in a Reduced Model of Atlantic Overturning Hysteresis
AU  - Sandy Hardian Susanto Herho
AU  - Iwan Pramesti Anwar
AU  - Mutiara Rachmat Putri
AU  - Rusmawan Suwarman
AU  - Deny Juanda Puradimaja
AU  - Dasapta Erwin Irawan
PY  - 2026
DA  - 2026/09/21
PB  - arXiv
DO  - 10.48550/arxiv.2609.24000
UR  - https://arxiv.org/abs/2609.24000
AB  - Interbasin exchange through the Indo-Pacific gateway supplies salt to the Atlantic and is widely invoked as a control on the stability of the Atlantic overturning circulation. We ask whether that control can act on the equilibrium structure of a conceptual thermohaline model. A closed five-box model with an exact salt invariant is constructed, comprising North Atlantic, upper-limb, Indian, Pacific, and deep reservoirs, with the return flow split between a warm route through the Indian reservoir and a cold route, together with an Indonesian Throughflow branch and an Agulhas retroflection. Adding the steady-state budgets of the gateway reservoirs shows that every internal exchange cancels, so the salt they export to the Atlantic is fixed by the net Atlantic freshwater export alone. This holds independently of the warm-route fraction, the throughflow, the retroflection, and how the export is apportioned among gateway reservoirs; across a parameter sweep the largest departure is of order ten to the minus eleven. The gateway therefore enters as a purely additive forcing and cannot renormalize the salt-advection feedback. Replacing the discrete transit lag by a gamma memory kernel leaves the equilibria unchanged but yields a closed-form threshold for oscillatory instability depending only on kernel shape. Broad memory is strongly stabilizing, and a discrete lag is the least stable member of the family. Because the instantaneous feedback vanishes at the fold, oscillatory instability always precedes the saddle-node, over an interval widening more than tenfold as memory sharpens. Gateways therefore appear to act on transient rather than equilibrium dynamics
ER  -