Air Pressure at Altitude Calculator
Calculate atmospheric pressure, temperature, and air density at any altitude using the International Standard Atmosphere (ISA) model. Supports humidity correction.
Calculate pressure at depth P = P₀ + ρgh for any liquid. Converts to kPa, atm, psi, bar, and mmHg with force on surfaces.
| Depth (m) | Gauge (kPa) | Absolute (kPa) | Absolute (atm) |
|---|---|---|---|
| 1 | 9.8 | 111.1 | 1.10 |
| 2 | 19.6 | 120.9 | 1.19 |
| 5 | 49.0 | 150.3 | 1.48 |
| 10 | 97.9 | 199.2 | 1.97 |
| 20 | 195.8 | 297.1 | 2.93 |
| 50 | 489.5 | 590.8 | 5.83 |
| 100 | 979.0 | 1,080.4 | 10.66 |
| 200 | 1,958.1 | 2,059.4 | 20.32 |
| 500 | 4,895.2 | 4,996.5 | 49.31 |
| 1,000 | 9,790.4 | 9,891.7 | 97.62 |
| 3,000 | 29,371.1 | 29,472.5 | 290.87 |
| 10,000 | 97,903.8 | 98,005.1 | 967.24 |
Hydrostatic pressure is the pressure exerted by a fluid at rest due to gravity. At any point within a static fluid, the pressure increases linearly with depth according to the fundamental equation P = P₀ + ρgh. This principle, rooted in Pascal's law, is essential for diving safety, dam design, submarine engineering, and water-supply systems.
The gauge pressure ρgh tells you how much pressure the fluid column itself adds above the surface pressure P₀. At 10 meters of freshwater depth, gauge pressure is about one atmosphere (≈ 101 kPa), which is why scuba divers double the absolute pressure on their bodies with every 10 m descent. At the bottom of the Mariana Trench (≈ 11 000 m), the pressure exceeds 1 100 atm.
This calculator handles any liquid — from freshwater and seawater to mercury, oil, blood, and custom fluids. It outputs pressure in six unit systems and computes the total force on a submerged flat surface, useful for tank wall and bulkhead design.
Whether you are sizing a water tank, planning a dive, or designing a submarine hull, knowing the pressure at depth is critical. This calculator gives the result in all common pressure units and includes force calculations for structural design.
Hydrostatic Pressure: P = P₀ + ρgh
Where:
• P = absolute pressure at depth (Pa)
• P₀ = surface or atmospheric pressure (Pa)
• ρ = fluid density (kg/m³)
• g = gravitational acceleration (m/s²)
• h = depth below surface (m)
Gauge Pressure: P_gauge = ρgh
Force on flat surface: F = P × AResult: 3 115 kPa (≈ 30.7 atm)
P = 101 325 + 1025 × 9.81 × 300 = 101 325 + 3 016 575 = 3 117 900 Pa ≈ 3 118 kPa ≈ 30.8 atm. A submarine at 300 m depth experiences roughly 31 times atmospheric pressure.
Calculate pressure at depth P = P₀ + ρgh for any liquid. Converts to kPa, atm, psi, bar, and mmHg with force on surfaces. Use it when you need a repeatable calculation in the physics / fluid category and want the setup, result, and supporting values kept together. This is especially helpful when small input changes, unit choices, or rounding decisions can change the final number.
Start by confirming that the inputs match the formula shown on the page. Then compare the main output with the worked example and any secondary values shown by the calculator. If the result will be used in another calculation, keep extra precision until the final step and record the assumptions beside the number.
Treat the result as a calculation aid rather than a substitute for context. For schoolwork, include the formula and substitution steps. For planning, technical, financial, or health-related decisions, verify important numbers against primary records, current rules, or a qualified professional before acting on them.
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In the deepest part of the Mariana Trench (≈ 10 994 m), the absolute pressure is about 1 100 atm or 110 MPa. Only specially engineered vessels can survive such forces.
No. Hydrostatic pressure depends only on depth, fluid density, and gravity — not on container shape. This is the "hydrostatic paradox": a narrow tube and a wide tank at the same depth have the same pressure.
Gauge pressure tells the diver how much more pressure they experience compared to the surface. Each 10 m of seawater adds roughly 1 atm of gauge pressure, affecting gas absorption and decompression requirements.
Engineers calculate the force on the dam face by integrating ρgh over the submerged area. Because pressure increases with depth, the resultant force acts at ⅓ of the depth from the bottom, not at the centre.
For most liquids over moderate depth ranges, incompressibility is an excellent approximation. In very deep ocean scenarios, seawater compressibility slightly increases density and pressure beyond the linear model.
The hydrostatic equation applies to fluids at rest. For moving fluids, Bernoulli's equation accounts for both static and dynamic pressure components.
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