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Squat effect
Squat effect
from Wikipedia

The squat effect is the hydrodynamic phenomenon by which a vessel moving through shallow water creates an area of reduced pressure that causes the ship to increase its draft (alternatively decrease the underkeel clearance of the vessel in marine terms) and thereby be closer to the seabed than would otherwise be expected. This phenomenon is caused by the water flow which accelerates as it passes between the hull and the seabed in confined waters, the increase in water velocity causing a resultant reduction in pressure. Squat effect from a combination of vertical sinkage and a change of trim may cause the vessel to dip towards the stern or towards the bow. This is understood to be a function of the Block coefficient of the vessel concerned, finer lined vessels Cb <0.7 squatting by the stern and vessels with a Cb >0.7 squatting by the head or bow. [1]

Squat effect is approximately proportional to the square of the speed of the ship. Thus, by reducing speed by half, the squat effect is reduced by a factor of four.[2] Squat effect is usually felt more when the depth/draft ratio is less than four[2] or when sailing close to a bank. It can lead to unexpected groundings and handling difficulties. There are indications of squat which mariners and ship pilots should be aware of such as vibration, poor helm response, shearing off course, change of trim and a change in wash.

Squat effect is included by navigators in under keel clearance calculations.[3]

Marine incidents

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It was a cause of the 7 August 1992 grounding of the Queen Elizabeth 2 (QE2) off Cuttyhunk Island, near Martha's Vineyard. The liner's speed at the time was 24 knots (12 m/s) and the draft was 32 feet (9.8 m). The rock upon which the vessel grounded was an uncharted shoal later determined to be 34.5 feet (10.5 m), which should have given her room to spare, were it not for the "squat effect."[4] U.S. National Transportation Safety Board investigators found that the QE2's officers significantly underestimated the amount the increase in speed would increase the ship's squat. The officers allowed for 2 feet (0.61 m) of squat in their calculations, but the NTSB concluded that squat at that speed and depth would have been between 4.5 and 8 feet (1.4 and 2.4 m).[5]

Squat is also mentioned as a factor in the collision of the bulk carriers Tecam Sea and Federal Fuji in the port of Sorel, Quebec, in April 2000.[1]

The third largest cruise ship in the world, MS Oasis of the Seas, used this effect to obtain an extra margin of clearance between the vessel and the Great Belt bridge, Denmark, 1 November 2009, on a voyage from the shipyard in Turku, Finland to Florida, USA.[6] The new cruise liner passed under the bridge at 20 knots (37 km/h) in the shallow channel, giving the ship extra clearance due to a 30 cm squat.

References

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Further reading

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from Grokipedia
The squat effect, also known as ship squat, is a hydrodynamic phenomenon in wherein a vessel experiences vertical sinkage and a reduction in under-keel clearance when moving through shallow waters, primarily due to accelerated water flow beneath the hull that decreases hydrostatic pressure according to . This effect causes the ship to settle deeper into the water, potentially leading to grounding if not properly managed, and is most pronounced when water depth is less than 1.5 times the vessel's draft. It arises from the interaction between the ship's hull and the confined , where the continuity principle results in increased flow velocity under the , exacerbating the . Key factors influencing the magnitude of squat include the vessel's speed, block coefficient (a measure of hull fullness), and the blockage ratio (the proportion of the channel cross-section occupied by the ship). Squat is proportional to the square of the ship's speed, meaning higher velocities amplify the effect significantly—for instance, doubling speed quadruples the squat—and it tends to be greater in confined channels like rivers or canals due to additional banking suction. Full-form ships with a block coefficient greater than 0.7 (e.g., tankers) typically experience forward trim (bow sinkage), while fine-form vessels with coefficients below 0.7 (e.g., container ships) trim aft. Other contributors include the seabed topology, initial trim or heel, and proximity to banks or other vessels, all of which can intensify the hydrodynamic forces. Predicting and mitigating squat is crucial for maritime safety, as it can reduce maneuverability by 20-30%, increase turning radii, and heighten collision risks with the , particularly in restricted waters. Empirical formulas are commonly used for estimation, such as the open-water approximation Squat = (C_b × V^2) / 100, where C_b is the block and V is speed in knots (with a confinement factor of 50 instead of 100 for restricted waters), though advanced hydrodynamic models and software are preferred for precision. Mariners counteract squat by reducing speed (halving it quarters the effect), adjusting trim, or using real-time monitoring tools like echo sounders to maintain adequate under-keel clearance, ensuring safe passage in shallow drafts.

Fundamentals

Definition and Overview

The squat effect is a hydrodynamic that occurs when a ship moves through shallow , characterized by an increase in the vessel's draft—known as sinkage—and potentially a change in trim due to reduced hydrostatic pressure beneath the hull. This effect manifests as the ship settling deeper into the , distinct from its stationary condition, and is particularly pronounced when the water depth is limited relative to the ship's dimensions. Sinkage represents the uniform vertical downward movement of the entire hull, reducing the overall under-keel clearance, while trim refers to a rotational adjustment in the ship's longitudinal attitude, which may result in the bow or dipping further. These changes arise dynamically only when the ship is , as opposed to static draft, which is fixed by the vessel's displacement and water density at rest. From a visual perspective, the squat effect causes the ship to appear "squatted" or lowered in the water, as if the is rising toward the , thereby diminishing the available margin and heightening the risk of grounding. This phenomenon is a critical consideration in restricted waterways, where even modest speeds can amplify the effect.

Physical Principles

The squat effect arises primarily from hydrodynamic interactions between a moving ship and the surrounding in restricted depths, governed by fundamental fluid dynamic principles. In shallow , the ship's hull displaces , constricting the flow beneath and around it. According to the , which ensures in , this constriction accelerates the water velocity in the narrowed channel under the hull compared to the undisturbed flow ahead. The increased velocity creates a low-pressure zone, as described by , where the sum of pressure energy and remains constant along a streamline. Specifically, the faster-moving water under the hull reduces , causing the ship to experience a net downward force or sinkage, as the reduced pressure fails to fully support the vessel's weight. This pressure reduction is not uniform along the hull, leading to a characteristic distribution that influences both sinkage and trim. At the bow and , where the flow converges and diverges, higher pressures develop due to stagnation and deceleration effects, while amidships, the accelerated parallel flow maintains lower pressures. This gradient typically results in greater sinkage amidships, leading to trim by the bow for full-form ships and trim by the for fine-form vessels. In addition to these inviscid pressure-driven mechanisms, and viscous effects contribute to squat. stems from the energy dissipated in generating surface waves, which in shallow water alters the elevation and amplifies the pressure imbalance beneath the hull, increasing overall sinkage. Viscous effects, including friction and in the constricted flow, further enhance resistance and squat by generating additional drag and eddy formations around the hull. The manifestation of squat differs between confined and unconfined waters due to varying flow constraints. In unconfined shallow water, such as open channels, squat is predominantly influenced by wave-making patterns modeled through potential flow theories, resulting in a more symmetric sinkage with moderate trim changes. In confined waters like canals, the proximity of sidewalls intensifies return currents and blockage, leading to greater velocity accelerations and pressure drops, often modeled via one-dimensional theories that emphasize longitudinal flow variations.

Influencing Factors

Ship Characteristics

The severity of the squat effect in ships is significantly influenced by the vessel's block coefficient (Cb), which measures the fullness of the hull form relative to a rectangular block of the same , beam, and draft. A higher Cb, typical of fuller hull forms such as those found in large tankers (often around 0.85), results in greater squat because these designs displace more water and create increased flow blockage under the hull, amplifying the low-pressure zone beneath the vessel. In contrast, ships with lower Cb values, such as bulk carriers (around 0.75) or finer forms below 0.7, experience less overall sinkage but may exhibit trim changes, with squat predominantly by the due to the distribution of and forces. The -to-beam ratio (L/B) also plays a key role in determining squat magnitude, with slender vessels (high L/B, often exceeding 7 for modern tankers) generally experiencing reduced squat compared to beamier designs (lower L/B). Slender hulls minimize hydrodynamic blockage and in shallow water, leading to less pronounced differentials along the hull . Beamier ships, by contrast, generate greater under-keel flow acceleration due to their wider cross-section, intensifying the squat effect for equivalent speeds and drafts. The draft-to-depth ratio (d/h) further modulates squat, where deeper-drafted ships relative to the available water depth (higher d/h) amplify the phenomenon by restricting vertical flow paths and increasing the relative blockage. This intrinsic ship property interacts with external water depth to heighten sinkage risks, particularly when h/d falls below 2.5. Specific hull shape features, such as bulbous bows and stern configurations, influence local distributions and thus the trim component of squat. Bulbous bows can alter bow sinkage by modifying inflow patterns, potentially reducing forward trim moments in some designs, while stern shapes—such as those with pronounced transoms or skegs—affect aft , contributing to squat in conventional forms. Service speed and type contribute variably to squat responses, with faster service speeds (e.g., above 15 knots for vessels) exacerbating the effect nonlinearly, as squat increases approximately with the square of the speed due to heightened flow velocities under the hull. Twin-screw systems, common in maneuverable vessels, often produce more uniform bodily sinkage compared to single-screw designs, which tend to induce greater squat from localized propeller-induced low at the aft end.

Waterway Conditions

The squat effect is profoundly influenced by the water depth relative to the ship's draft, denoted as the ratio , where h is the depth and d is the draft. As decreases below 1.2, squat increases non-linearly due to the acceleration of flow beneath the hull, leading to reduced and greater sinkage; critical thresholds occur around = 1.1 to 1.3, where even modest speeds can result in under-keel clearances dropping to dangerous levels. In such shallow conditions, the phenomenon becomes particularly pronounced, with experimental data showing squat magnitudes up to 30% of the draft in limiting scenarios. Channel width and overall confinement further amplify squat by inducing additional flow acceleration from bank effects. In narrow channels, where the blockage factor (the ratio of the ship's submerged cross-sectional area to the channel's) exceeds 0.1, squat can increase by 20-50% compared to open water, as the restricted flow creates a stronger differential around the hull. This confinement is especially severe in canals or straits with widths less than 2-3 times the ship's beam, exacerbating the risk of grounding during transit. Variations in , such as bends, slopes, or irregular depths, introduce asymmetric squat and induce trim changes that complicate . For instance, in curved channels or areas with sloping banks, the uneven flow distribution causes differential sinkage fore and aft, potentially leading to bow or trim by several degrees. Similarly, abrupt depth changes along the path can generate transverse currents, further distorting the squat pattern and increasing lateral drift. Currents in the modify squat by altering the ship's relative speed through the water. Following currents, which reduce , tend to lessen squat magnitude, while opposing currents increase it by effectively raising the speed-squared component of the hydrodynamic forces. This effect is particularly relevant in tidal channels, where current speeds of 1-2 knots can shift squat by up to 25% depending on direction. Bottom topography has a subtler influence on the hydrodynamics of squat but plays a key role in associated risks. Soft or deformable seabeds minimally alter the flow patterns compared to hard bottoms, yet they heighten grounding vulnerability once squat reduces under-keel clearance. Uneven topographies, such as ridges or depressions, can induce additional trim without significantly changing overall sinkage, underscoring the need for precise bathymetric data in confined areas.

Prediction Methods

Empirical Formulas

Empirical formulas provide practical tools for mariners and engineers to estimate ship squat quickly using basic ship and waterway parameters, derived from extensive model tests and field observations. These methods prioritize simplicity for onboard calculations, focusing on key variables like speed, hull form, and water depth. The Barrass , developed from analyses of merchant vessel data, estimates maximum squat in open waters as S=CbV2100S = \frac{C_b V^2}{100}, where SS is squat in , CbC_b is the block coefficient (dimensionless, typically 0.7–0.85 for full-form ships), and VV is speed in knots. For confined waters, a factor of 2 is applied: S=2CbV2100S = \frac{2 C_b V^2}{100}. This relation accounts for hydrodynamic sinkage in relatively shallow conditions (h/d ≈ 1.1–1.4) and is applicable for speeds below critical Froude numbers. Variants incorporate blockage factor Sb=AsAcS_b = \frac{A_s}{A_c}, such as S=2.08Cb2/3V2Sb2/3/30S = 2.08 C_b^{2/3} V^2 S_b^{2/3} / 30. The Huuska method (also referred to as Huuska/Guliev), offers a relation for squat and associated trim, incorporating the ship's length-to-beam (L/B) and a speed-squared term adjusted by depth . The core equation is S=2.4Fnh2KsS = 2.4 \nabla Fn_h^2 K_s, where \nabla is displacement volume in cubic meters, Fnh=V/ghFn_h = V / \sqrt{g h}
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