IHE vs. Continuous Hypoxia: Maximizing EPO Response
There are two common ways athletes use hypoxia for adaptation:
Continuous hypoxia: living/sleeping for many days at altitude (or in an altitude tent).
IHE / HEPOX: short, controlled bouts of hypoxia, awake and at rest.
Both can work, but they behave differently in the body—especially for EPO (erythropoietin) and ventilation/CO₂ handling.
Continuous hypoxia: long exposure, strong early EPO rise, then acclimatization
With prolonged altitude exposure, EPO typically rises early and then declines toward baseline even while the hypoxic exposure continues.
Reviews describe EPO increasing within the first 1–3 days, peaking around ~1–2 days, then falling despite ongoing hypoxia as acclimatization progresses. (Liebert Publishing)
Classic high-altitude physiology also documents this “early rise then decline” pattern. (Cleveland Clinic)
Practical takeaway: continuous altitude delivers a very large total hypoxic dose (hours/day), but the EPO signal isn’t permanently elevated.
HEPOX (IHE): short at-rest sessions, repeatable “pulses” of hypoxia
HEPOX is intermittent hypoxic exposure at rest: you’re awake, seated, and monitored (SpO₂ + HR). The stimulus is standardized by physiologic response rather than a fixed “altitude number.”
Where HEPOX often differs from altitude living is severity per minute:
Many “live high” scenarios are moderate enough that SpO₂ doesn’t drop as aggressively.
HEPOX is commonly run at a lower SpO₂ target window (often ~80–85%), which can provide a stronger hypoxic signal per minute. (Physiology Journals)
EPO: why “short + more intense” can spike the signal
Controlled human studies show that even brief intermittent hypoxia can increase EPO:
Eight 4-minute cycles of intermittent hypoxia have been reported as the shortest protocol shown to increase serum EPO in healthy young adults. (Physiology Journals)
That same model found eight cycles of intermittent hypoxia increased EPO to a similar extent as 120 minutes of continuous hypoxia, with peak EPO observed around ~4.5 hours after the onset of hypoxia. (PubMed)
Practical takeaway: HEPOX aims for repeatable EPO pulses by using a more intense hypoxic level for short periods—without requiring overnight exposure.
Ventilatory adaptations: the “O₂/CO₂ coupling–decoupling” story (and why it matters)
This is the part many blogs skip—but it affects both how HEPOX feels and how the body adapts.
1) What “coupling” means in plain English
When you breathe more (hyperventilate), you typically do two things at once:
you increase oxygen uptake (helpful in hypoxia), and
you blow off more CO₂, lowering arterial CO₂ (PaCO₂) and raising blood pH (respiratory alkalosis). (NCBI)
That linkage is the basic O₂–CO₂ coupling: pushing ventilation up tends to push CO₂ down.
2) Why CO₂ changes can change the “feel” of hypoxia
Dropping CO₂ (hypocapnia) is one reason people can feel lightheaded, “tingly,” or off during aggressive over-breathing—because low PaCO₂ is associated with respiratory alkalosis and downstream effects like cerebral vasoconstriction. (NCBI)
This is why HEPOX sessions should emphasize calm, controlled breathing—you want the hypoxic stimulus without “panic ventilation.”
3) “Decoupling”: how the body adapts over repeated exposure
With repeated hypoxic exposure (including altitude acclimatization), the control system for breathing can adapt—shifting chemoreflex behavior and CO₂ “set points.”
High-altitude exposure has been shown to modify ventilatory CO₂ sensitivity and the relationship between chemoreflex thresholds and acid–base status (e.g., bicarbonate). (PMC)
Intermittent hypoxia protocols in humans have also demonstrated changes in ventilatory control, including shifts in CO₂ thresholds and persistence of altered ventilatory responses after exposure blocks. (PubMed)
In practice, this is part of what people mean by “decoupling”: over time, the system can tolerate maintaining ventilation (supporting oxygenation) with different CO₂/pH dynamics than in the first exposures—because the body adjusts the control knobs.
4) A key nuance: “isocapnic” vs “poikilocapnic” hypoxia
Some research protocols clamp CO₂ (isocapnic hypoxia) so CO₂ stays stable while oxygen drops—this isolates the oxygen signal. Other protocols allow CO₂ to drift (poikilocapnic), which changes sensations and physiology.
This matters because two “equally low SpO₂” sessions can feel different depending on how CO₂ behaves—and that can affect comfort, perceived difficulty, and how repeatable the protocol is. (Physiological Society Journal)
Important nuance: EPO spikes are a signal, not a promise of RBC gains
EPO is the signal to build red blood cells. Whether you see measurable RBC changes depends on total dose over time, iron availability, and recovery. Reviews consistently note large variability in downstream hematologic outcomes. (Cdn Science Publishing)
Bottom line
Continuous altitude is a high-volume hypoxia strategy: lots of hours, strong early EPO response, then acclimatization.
HEPOX (IHE) is a high-signal strategy: short, at-rest sessions standardized by SpO₂, often at a more intense hypoxic level per minute—capable of producing repeatable EPO pulses while fitting into real life. (PubMed)