I will try to explain the altitude issue a different way. The key is this: it is not the pressure at any given depth that matters; it is the change in pressure as the diver ascends. In basic deco theory, you understand that a diver has to keep tissue pressure at a safe gradient relative to ambient pressure. As the diver ascends and ambient pressure decreases, the diver's tissue pressure must decrease enough to stay within that safe gradient range. At altitude, the decrease in ambient pressure as the diver ascends occurs at a different rate from sea level, with the biggest differences occurring in the shallowest depths.
Water weighs the same at any altitude, so the deeper the diver is on a dive, the greater the percentage of that water weight in determining ambient pressure. As the diver ascends and encounters less water weight, the atmospheric weight becomes more and more a factor.
To illustrate, let's compare the change in ambient pressure at an altitude of 6,000 feet as the diver ascends from what would be 6 ATA at sea level. At that altitude, the atmospheric pressure is about 0.8 ATA, so at the same starting depth (170 FFW), the diver is at 5.8 ATA. That 0.2 difference will be maintained throughout the ascent, but it becomes a greater and greater factor as you ascend,
You can see that reflected in the summaries of the two Buhlmann profiles in my last post. There is no real difference between the Buhlmann sea level profile and the altitude profile until you get to the last two deco stops, at which point the difference becomes very significant as the profile strives to keep the diver's tissue pressure at a safe gradient compared to the ambient pressure.
Water weighs the same at any altitude, so the deeper the diver is on a dive, the greater the percentage of that water weight in determining ambient pressure. As the diver ascends and encounters less water weight, the atmospheric weight becomes more and more a factor.
To illustrate, let's compare the change in ambient pressure at an altitude of 6,000 feet as the diver ascends from what would be 6 ATA at sea level. At that altitude, the atmospheric pressure is about 0.8 ATA, so at the same starting depth (170 FFW), the diver is at 5.8 ATA. That 0.2 difference will be maintained throughout the ascent, but it becomes a greater and greater factor as you ascend,
- At 170 FFW, the pressure is only 3% less than at sea level--barely worth considering.
- At 136 FFW, the diver is now at 4.8 ATA, still only 4% less than sea level
- At 102 FFW, the altitude diver is still only at 5% less pressure than at sea level.
- At 68 FFWW, the altitude diver is at 6.7% less pressure than at sea level.
- At 34 FFW, the diver is at 10% less pressure than at sea level.
- At 20 FFW, diver is at 12% less pressure than at sea level
- At 10 FFW, the diver is at nearly 16% less pressure than at sea level.
- At the surface, the diver is at 20% less pressure than at sea level.
You can see that reflected in the summaries of the two Buhlmann profiles in my last post. There is no real difference between the Buhlmann sea level profile and the altitude profile until you get to the last two deco stops, at which point the difference becomes very significant as the profile strives to keep the diver's tissue pressure at a safe gradient compared to the ambient pressure.
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