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Research Methods

The Bremen-Cog: reconstructed one more time

Pat Tanner et Mike Belasus
p. 315-324

Résumés

Dans le cadre du projet triennal « Entre la mer du Nord et la mer de Norvège : recherche interdisciplinaire sur la Hanse » (2015-2018), mis en place par l’Association Leibniz au Musée maritime allemand, des questions ont été soulevées sur la navigabilité des cogues du type de celle de Brême. Notre attention s’est donc portée sur la cogue de Brême, datée de la fin du Moyen Âge, précisément de 1378 ou 1379, et trouvée en 1962 dans la Weser près de Brême et qui est aujourd’hui exposée au musée de Bremerhaven.
Le projet n’a pas commencé avec l’intention de proposer une nouvelle hypothèse de restitution d’un navire par ailleurs déjà restitué, mais plutôt d’examiner les caractéristiques hydrodynamiques et de tenue à la mer du navire. Ceci afin de voir si les navires de ce type ont pu participer à un commerce océanique en navigant sur ­l’Atlantique Nord jusqu’à l’Islande.
Afin d’évaluer la tenue à la mer et les capacités transocéaniques du navire, l’établissement d’une forme de coque fiable ainsi qu’un plan détaillé de la construction sont nécessaires. L’évaluation des caractéristiques hydrostatiques globales, de la stabilité statique et dynamique et des capacités générales de navigation du navire s’effectue grâce aux mesures complexes des centres de flottabilité, de flottaison et de gravité.

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Texte intégral

  • 1  “Bremen-type” refers to the shipbuilding method defined on the base of the Bremen-Cog. It is used (...)

1Earlier historical research determined the cog to be a predominant vessel for seaborne transport within the Hanseatic League (Heinsius 1956; Fliedner 1969; Thier 2017). The technical definition of this supposed ship type was later based on the Bremen-Cog (Crumlin-Pedersen 2000, p. 230-233; Hocker, Ward 2004, p. 75). The majority of the league’s trade ranged from Russia in the east, across the Baltic Sea, to Britain in the west, across the North Sea. Records also show trade with “outlying” regions, such as Iceland in the northwest Atlantic Ocean (Wubs-Mrozewicz 2009), as well as south into the Mediterranean. The term “cog” is mentioned in connection with trade in all these regions (Gardiner 2007, p. 405).1

2However, is the Bremen-Cog, an example of the Bremen-type shipbuilding method, a typical example of the vessels that traded across the open oceans with Iceland as documented in historical records? Is the Bremen-type ship of the archaeological record the oceangoing cog of 80-200 tonnes in the historical documents (Gardiner 2007) of the Hanseatic League?

3Ship technical calculations have in the past been employed in the analyses of the original qualities of an archaeological vessel, and hence its sphere of operation. While it is possible to determine various coefficients that can describe the form and the hydrostatic qualities for each individual vessel, only by quantifying these conditions can a basis be formed for a scientific analysis. When studying the hydrodynamic conditions, the problems are even greater. The results of these are dependent on several factors, and for new ships, a combination of experiments with scale models, tank tests and full-scale sea trials has made it possible to develop correlation factors that permit reasonably reliable predictions of performance to be made. However, such work on ancient ships has not been fully undertaken in order to corroborate the results (Crumlin-Pedersen, Trakadas 2003, p. 217–218).

1. Previous analyses of the Bremen-cog

4Previous analyses of the Bremen-Cog have included the rigging, which was designed by Hoheisel, a naval architect and technical director of the German Maritime Museum. Clausen, a student in ship engineering at Hamburg University, tested Hoheisel’s reconstructed rigging on a simplified model in a wind tunnel. Results indicated that the vessel could tack to windward, but tests were unable to include wave action or seaway. Redlin, a student at the Technical University of Berlin, tested the hull shape: he drew an idealised set of lines based on photogrammetry measurements, and calculated the stability for various cargo loads and resultant waterlines, concluding the vessel was stable while ballasted or loaded but unstable if unballasted with the rigging standing. Redlin calculated a minimum ballast of 26 tonnes, based on the Vejby cog in Denmark (Hoheisel 1994). Professor Postel at the Institute for Shipbuilding in Kiel undertook tank-towing tests, and his experiments indicated the model could not come above 90° to the true wind. Postel described the vessel as a “beam-wind sailor” provided it was ballasted and in calm waters (Hoffmann, Hoffmann 2009, p. 287-289).

  • 2  The weight for Roland von Bremen has been attributed to the extra thick hull planking and thicker (...)

5Further details of the Bremen-Cog include Lahn’s estimate of the ship’s weight at 60 tonnes empty, giving a draught of 1.25 m and a cargo weight of 76-84 tonnes, giving a displacement of 136-144 tonnes at a draught of 2.25 m (Lahn 1992, p. 250). Hoheisel estimated the ship to weigh 55 tonnes without ballast, to have a draught of 1.53 m when ballasted, and a draught of 2.25 m with a maximum cargo of 87 tonnes. Based on Lahn’s drawings, Kenn Jensen calculated the displacement to be 139.23 tonnes at 2.25 m draught (Jensen 1999, p. B-50). Of the three replicas: the Ubena von Bremen, built in 1991, is listed as 75 tonnes displacement, including 35 tonnes of ballast at 2.25 m draught; the Kieler Hansekogge, also built in 1991, is listed as 60 tonnes displacement including 22 tonnes of ballast at 1.6 m draught; and the Roland von Bremen, built in 2000, is listed as 120 tonnes displacement including 20 tonnes of ballast at 2.25 m draught (Hoffmann, Hoffmann 2009, p. 291). The displacement weights for the three replicas equate to unballasted weights of 40, 38 and 100 tonnes respectively2, even though all three were built based on the same drawings, and should be the same shape, yet Roland von Bremen displaces 45 tonnes more than Ubena at the same draught. Either the quoted figures are inaccurate, or the Roland von Bremen has an additional 43.9 m³ volume in her underwater hull form. A comparison of the various versions is set out in table 1. As Crumlin-Pedersen stated, the relevance of these calculations is impaired by the fundamental uncertainty that is attached to the reconstruction solution (Crumlin-Pedersen, Trakadas 2003, p. 217-218).

Table 1: Comparison of the published versions of the Bremen-Cog

Version Empty weight Ballast tonnes Cargo tonnes Displacement tonnes Draught
Lahn 60 tonnes –  76 – 84 136 – 144 2.25 m
Hoheisel 55 tonnes 26 –  81 1.53 m
Hoheisel 55 tonnes –  87 142 2.25 m
Jensen –  –  –  139.23 2.25 m
Ubena von Bremen 40 tonnes 35 –  75 2.25 m
Kieler Hansekogge 38 tonnes 22 –  60 1.6 m
Roland von Bremen 100 tonnes 20 –  120 2.25 m

2. Available data sets

  • 3  The still ongoing deformation processes are a subject of current research on monitoring of large-s (...)
  • 4  The vessel remains were 3D-laser scanned in 2011 and 2014, and recorded using photogrammetry in 20 (...)

6The shape of the Bremen-Cog, as it currently stands on display in the museum’s ship hall, is not a true representation of the hull shape: it has suffered several periods of distortion3. Consequently, a decision was made to attempt to examine the current overall hull shape and compare that to the available data sets. The available data sets included two-dimensional paper drawings by Lahn in 1981-90, which also included a photogrammetry survey of the reconstructed vessel carried out by the University of Hanover in 1980, as well as published material on the vessel (Kiedel, Schnall 1989; Lahn, 1992). In addition, the data from three separate occasions of three-dimensional digital documentation4 carried out by the museum in 2011 and 2014 was included.

7The goal of the project changed from simply analysing the seafaring capabilities of the vessel to also examining the current form of the vessel on display, as well as attempting to distil several conflicting data sets into a valid hypothetical recons­truction to be used as the basis for detailed hydrodynamic and seakeeping analysis.

3. Methodology

8All of the available data sets were imported into Rhinoceros, a 3D CAD modelling software, and the original published Lahn drawings were converted into three-dimensional CAD models in order to compare with the various three-­dimensional digital documentation sets (fig. 1). This clearly illustrated the changing form of the hull shape over the 30 year period from the initial reconstruction to its shape when documented in 2014 (Tanner 2017a, p. 5-24). A series of cross sections (A-H) were taken at 2 m intervals along the keel, and the changing height of the sheer at each point is documented in table 2. This deformation and change in hull shape could possibly be explained by the steel structure, which is currently supporting the vessel in the museum, or by shrinkage of the exhibited timbers

Fig. 1: Comparison of the digital data sets

Fig. 1: Comparison of the digital data sets

The colour coding is as follows: blue is the hull shape from Lahn’s section drawings; green is the hull shape from Lahn’s lines plan drawings; and red is the hull shape during 3D laser scanning in 2014.

(P. Tanner)

Table 2: Changes in sheer heights over time

Position

A

B

C

D

E

F

G

H

Photogrammetry 1980

0

0

0

0

0

0

0

0

Lahn Drawing 1985

+32 mm

+15 mm

+23 mm

+86 mm

+82 mm

+66 mm

+19 mm

0 mm

3D scan 2011

No Data

– 46 mm

– 47 mm

– 117 mm

– 71 mm

– 104 mm

– 113 mm

– 79 mm

SFM Oct 2014

– 66 mm

– 58 mm

– 58 mm

– 141 mm

– 118 mm

– 135 mm

– 143 mm

– 92 mm

3D scan 2014

– 105 mm

– 103 mm

– 102 mm

– 169 mm

– 138 mm

– 156 mm

– 185 mm

– 99 mm

9While generating 3D models from Lahn’s drawings, it was realised that all of these drawings could not be reconciled into a single coherent three-dimensional model, as can be seen from the blue and green surfaces in figure 1. Additional discrepancies noted (fig. 2) include strake runs which appear very distorted when modelled three dimensionally, the transverse beam bolted 80 mm lower than the archaeological evidence suggests, the reverse camber to the castle deck, as well as the angled stern castle deck.

Fig. 2: Top left, unfair strake runs; top right, strake runs not matching archaeological evidence; bottom left, reverse camber in castle deck; bottom right, transom beam bolted (yellow) 80 mm below existing hole (circled red)

Fig. 2: Top left, unfair strake runs; top right, strake runs not matching archaeological evidence; bottom left, reverse camber in castle deck; bottom right, transom beam bolted (yellow) 80 mm below existing hole (circled red)

(P. Tanner)

  • 5  This process is explained in detail in the reconstruction report on file at the German Maritime Mu (...)

10It was therefore decided to undertake a completely revised digital reconstruction of the vessel5 in order to reconcile the various Lahn drawings, not only with each other, but also with the archaeological evidence. The methodology used in this approach has been demonstrated using a known test subject, and the results have been shown to be better than 99% accurate for dimensional variations in the 3D modelling process, and better than 98% accurate when calculating displacement values using average wood densities (Tanner 2017b).

4. A new hypothetical reconstruction

11In a process similar to that used on the Drogheda boat, the Newport ship and the Poole Iron Age logboat (Berry et al. 2019; Tanner 2013a, 2013b), a digital model of every constituent part of the vessel was created using Rhinoceros 3D, with Lahn’s drawings and the archaeological data as reference. A series of fair curves were created to represent each strake. The length of each curve was fixed to match the archaeological evidence taken from the 3D scan data, and the curvature adjusted until fair, using Lahn’s drawings and the 3D scan data as a reference (fig. 3, top). Then, digital 3D models of the surviving hull elements were created and fitted to the evolving hull form (fig. 3, middle left). Next, the missing elements were extrapolated and modelled (fig. 3, bottom left) to create a more definitive hypothetical reconstruction combining all of the available data sets (fig. 3, bottom right). The revised hypothetical reconstruction based on the evidence resulted in a less full-bodied hull form, compared to Lahn’s reconstruction, particularly in the lower extremities, such as at Frame 10 (fig. 3, top left) where the revised shape was up to 20 cm narrower at the height of the fourth strake.

Fig. 3: Top left, difference between Lahn and reconstructed hull at Frame 10; top right, difference between two hull forms; middle left, archaeological remains 3D modelled; bottom left, missing elements extrapolated; bottom right, fully reconstructed hypothetical reconstruction of the Bremen cog

Fig. 3: Top left, difference between Lahn and reconstructed hull at Frame 10; top right, difference between two hull forms; middle left, archaeological remains 3D modelled; bottom left, missing elements extrapolated; bottom right, fully reconstructed hypothetical reconstruction of the Bremen cog

(P. Tanner)

  • 6  This weight is based on using an average density for the oak, in this case 800 kg per m³ being typ (...)

12With the entire vessel modelled using Rhinoceros 3D, it was then possible to analyse the vessel in greater detail. One of the added benefits of the project was that 3D modelling the surviving archaeological elements allowed for a better understanding of the material remains. The surviving elements of the Bremen-Cog weigh a total of 25.02 tonnes6. In addition, during the recording and digital reconstruction phase of this project, it was possible to accurately measure the timbers, allowing the shrinkage of the conserved timbers to be analysed. A sample of the results is set out in table 3. The amount of shrinkage proved comparable with that documented in the Newport medieval ship where tangential shrinkage (width in the case of radially split planks) ranged between 4.4 and as much as 15.1% with an 8% average (Jones, Panter 2016).

Table 3: Shrinkage measured between 1980 and 2014 scan dimensions

Location Lahn measurement 1980 2014 laser scan dims. Difference
Weather board @ F19 580 mm 527 mm 53 mm 9.1%
Strake 12 @ Frame 19 642 mm 604 mm 38 mm 5.9%
Strake 11 @ Frame 19 648 mm 609 mm 39 mm 6.0%
Strake 10 @ Frame 19 494 mm 457 mm 37 mm 7.5%
Strake 9 @ Frame 19 509 mm 465 mm 44 mm 8.6%
Weather board @ F23 574 mm 537 mm 37 mm 6.4%
Strake 12 @ Frame 23 635 mm 577 mm 58 mm 9.1%
Strake 11 @ Frame 23 649 mm 581 mm 68 mm 10.5%
Strake 10 @ Frame 23 505 mm 457 mm 48 mm 9.5%
Strake 9 @ Frame 23 515 mm 474 mm 41 mm 8.0%

5. Analysis of the hypothetical reconstruction

13The determination of a vessel’s capabilities is a complicated interaction between hydrodynamic and aerodynamic forces, dependant on many factors including flotation characteristics, static stability, dynamic stability, performance, environmental conditions, and seamanship. Past approaches to examining the Bremen-Cog’s seafaring or hydrodynamic capabilities have included tank and wind tunnel testing, which are limited (Crumlin-Pedersen, Trakadas 2003, p. 217-218), as well as full-scale replicas used for sea trials. However, the tests have produced conflicting results such as wind tunnel results indicating the vessel could tack to windward, while tank-towing tests indicated the model could not come above 90° to the true wind. The replicas all include modern additions, such as mechanical propulsion systems, watertight decks and other safety requirements. Hoheisel states the replica Kieler Hansekogge could sail at about 70° to the wind but would drift about 15 to 20° (Hoheisel 1994, p. 259), this would result in the vessel making little or no progress to weather as the resultant course to windward would be 90° or more.

  • 7  The use of coefficients such as block, prismatic, midship, volumetric and slenderness coefficient (...)

14A more traditional approach has typically been to use various coefficients that can describe the form and the hydrostatic qualities. McGrail (1987) gives a brief introduction to using weight calculations and hydrostatic curves to determine the stability, displacement and draught calculations on ancient boats in Chapter 3 of Ancient Boats in North-West Europe (McGrail 1987, p. 12–22), and discusses methods of assessing the performance of a vessel in Chapter 11 (McGrail 1987, p. 192-203). The use of simple form coefficients is suggested by McGrail as a method of determining relative assessments of a boat’s capabilities, such as length to beam ratio or beam to depth ratio. Hydrostatic curves defining the underwater form of a vessel are used to generate coefficients of form which give forecasts of performance. However, coefficients7 are a multiplier or factor that measures a particular property and are based on the underwater form of the vessel. Standard naval architectural convention divides the underwater volume into ten equal stations and using Simpson’s Rule an approximation of the underwater volume is calculated. This generates a snapshot of the underwater form of a vessel in a given flotation condition, which needs to be recalculated whenever external factors, such as additional cargo, or a change in heel angle due to wind load causes a change in the equilibrium condition, resulting in a changed underwater profile or volume.

  • 8  For the timber elements, a density of 800 kg per m³ being typical for oak at 27% moisture content

15Using Orca3D, a naval architecture plugin for Rhinoceros 3D allows for the rapid and real-time calculations of the hydrostatic forces in effect on a ship’s hull. By calculating the exact geometric form of the selected elements, and if material densities are applied to each element, the computer calculates the exact shape, weight and centre of gravity of the combined elements. Orca3D will then transform the model (ship) to its correct resultant equilibrium flotation condition. Once a static equilibrium condition has been achieved, the software also allows for external loadings such as wind loading, wind with icing, heavy lifting, towing, deck crowding and high speed turning to be applied to the model, and the relevant hydrostatic and stability criteria to be tested based on the updated flotation condition. In the case of the Bremen-Cog, all the constituent components of the vessel were solid modelled, and a material density applied to each8. The Orca3D software calculates the exact weight and centre of gravity for the entire ship and, based on the geometric shape of the hull form, alters the angles of heel, trim and displacement depth in order to establish the exact equilibrium flotation plane. This is done in real-time and the resulting flotation condition is the only possible solution for a vessel of that specific form and weight.

6. Static Stability

16A digital analysis of the vessel was carried out using Orca3D to determine its resultant equilibrium flotation condition in various weight and draught configurations. As the original flotation configuration for the original vessel is not known, the vessel was first tested in both a bare hull and fully rigged configuration to establish a baseline. Results showed that the bare vessel, without mast or rigging, floats in a stable condition. However, once the mast and rigging are added, the vessel becomes unstable and would require the addition of internal ballast. The quantity of internal ballast needs to be enough to counteract the overturning tendencies of the vessel itself as well as counteracting additional heeling moments caused by wind loading or wave roll. Modern rules for the stability of ships are formulated by the International Maritime Organisation (IMO): Bureau Veritas (BV) is one such classification organisation founded in Antwerp in 1828; it was originally Belgian but is now a French company (Bureau Veritas 2012, p. 81-97). The stability testing carried out by Orca3D used the Bureau Veritas criteria and the resulting static stability flotation conditions are shown in table 4.

Table 4: Various draught and displacement results

Condition Weight tonnes Cargo tonnes Displacement Draught aft Draught forward Freeboard Downflooding angle GMt
Bare hull and superstructure 43.25 0 43.25 1.25 m 0.64 m 3.26 m 49.5° 0.39 m
Fully rigged – unballasted 47.29 The vessel with a negative metacentric height is unstable, resulting in an angle of loll* of 4.9°.
Any slight heeling moment will capsize the ship.
– 0.29 m
Ballasted with 15 tonnes 62.29 0 62.29 1.49 m 0.95 m 2.97 m 44.7° 0.37 m
Draught set to 1.6 m (Hansekogge) 62.29 7.33 69.62 1.60 m 1.05 m 2.72 m 42.9° 0.34 m depending on cargo
Beams not submerged 62.29 45.01 107.30 2.06 m 1.54 m 2.72 m 35.32° 0.82 m depending on cargo
Draught set to 2.25 m 62.29 61.25 123.54 2.25 m 1.72 m 2.15 m 32.36° 0.86 m depending on cargo
Grågås Codex loading 62.29 108.01 170.30 2.77 m 2.17 m 1.74 m 24.21° 1.10 m depending on cargo
* Angle of loll is the state of a ship that is unstable when upright (i.e. has a negative metacentric height) and therefore takes on an angle of heel to either port or starboard. When this occurs, the vessel goes to neutral equilibrium, and the angle of heel at which it happens is called angle of loll.

7. Dynamic stability

17For lateral wind loading, the yard and sail were rotated as far as possible (36.3° in this case) in order to project the maximum possible surface area to a “beam-on” wind, representing a worst-case scenario wherein the sail was not released despite adverse winds. Orca3D uses this information to calculate a heeling moment, which is then applied to the vessel, in combination with wave roll action to determine the vessels resultant angle of heel and dynamic stability performance. Results from these tests indicated that 15 tonnes of internal ballast would be sufficient to satisfy the Marine Insurance Act (1906) and Bureau Veritas stability criteria. The term seaworthiness is a very broad one, as it not only includes the physical state of the vessel but also extends to other aspects and factors. Consequently, it is not easy to define seaworthiness in rigorous terms. A 13th-­century law defined a ship as seaworthy if it did not need to be bailed more than three times in 24 hours (Christensen 1968, p. 138-139). A medieval Icelandic law in the Grågås Codex states the minimum freeboard (F) of a cargo ship should be F=2D/5 where D = depth of hull amidships (Morken 1980, p. 178). In the case of the Bremen-Cog, this minimum freeboard would be F = 2 × 4.35 /5 = 1.74 m.

18The vessel was subsequently analysed in three flotation condi­tions: Condition A – fully rigged and ballasted with 15 tonnes; Condition B – with the protruding beam-ends not submerged, equating to a fully rigged ship, 15 tonnes of ballast and 45 tonnes of additional cargo; and Condition C – the Grågås Codex minimum freeboard condition, equating to a fully rigged ship, 15 tonnes of ballast and an additional 108 tonnes of cargo. For each flotation condition the vessel was then tested for various wind load and wave roll conditions using the Bureau Veritas criteria: the results are shown in Table 5.

  • 9  For all conditions, a sail area of 100 m² plus three additional ‘bonnets’ of 33 m² each giving a t (...)

Table 5: Resulting wind heel angle9

Wind strength Power generated from sail area Speed @ 70% efficient Sail Speed @ 40% efficient Sail Wind heel angle Freeboard remaining Gust heel angle 150% wind Freeboard remaining
Condition A Force 3 23.48 kW 7.45 6.75 7.98° 2.42 m 15.71° 1.92 m
Force 4 32.04 kW 7.85 7.15 15.71° 1.92 m 26.01° 1.21 m
Force 5 31.2 kW 7.80 7.1 15.80° 1.91 m 16.11° 1.20 m
Force 6 55.9 kW 8.85 7.82 21.3° 1.53 m 32.4° 0.79m
Condition B Force 3 23.48 kW 5.9 4.9 0.8° 1.54 m 4.47° 2.05 m
Force 4 32.04 kW 6.5 5.5 4.47° 2.05 m 9.67° 1.76 m
Force 5 31.2 kW 6.4 5.4 4.42° 2.05 m 9.60° 1.76 m
Force 6 55.9 kW 7.4 6.4 6.84° 1.92 m 14.17° 1.49m
Condition C Force 3 23.48 kW 4.85 4.00 0.76° 1.70 m 1.70° 1.63 m
Force 4 32.04 kW 5.40 4.45 1.70° 1.63 m 3.89° 1.49 m
Force 5 31.2 kW 5.35 4.40 1.65° 1.64 m 3.68° 1.50 m
Force 6 55.9 kW 6.37 5.35 2.57° 1.57 m 5.71° 1.37 m
  • 10  Fetch is the distance of open water that the wind blows over.

19So far, the vessel has been tested to assess how it would float in various loading conditions as well as examining the heeling moments generated with various wind and wave roll loadings. These results give an indication of the vessel’s initial static stability and demonstrate how the vessel will float at given cargo loads and various flotation depths and with various wind conditions. However, each test is a static snapshot and does not ­consi­der the dynamic and changing conditions of a body floating in water. Other than the vessel itself, the other major influencing factor on any sea voyage is the sea state, which is primarily influenced by waves. The three main factors which make up waves are wind speed, wind duration, and fetch10. These factors work together to create waves, and the greater each of the variables in the equation, the greater the size of the wave. The most significant variable of the three is fetch. Within the Baltic and North Seas, the fetch is limited to less than 300 nautical miles, thereby limiting the significant wave heights. Storm waves in the Baltic seldom exceed 2.4 m in height and 30 m in length, while those in the North Atlantic can reach heights of 10.6 m with a length of 304 m (Marchaj 1964, p. 400-401).

20Computational fluid dynamics is a potential approach to analyse both aero- and hydrodynamic interactions with a vessel, however, the calculation process is a static one and the vessel will require to be re-orientated for each changing environmental factor, and the computing requirements are large. An alternative approach was to use Unity3D, a real-time development platform that includes a built-in physics engine to handle calculations based on real world physics. Blocks of appropriate size were created to represent the wave height and length for both the Baltic Sea and Atlantic Ocean and the computer-­generated wind adjusted in order to create realistic sea conditions for both areas (fig. 4, top right). The digital model of the Bremen-Cog was then imported from Rhinoceros 3D to Unity, and with its characteristics set for Condition B (with the protruding beam ends not submerged, equating to a fully rigged ship, 15 tonnes of ballast and 45 tonnes of additional cargo), the physics engine applied a gravitational force on the vessel.

Fig. 4: Various sea states in the Baltic Sea and Atlantic Ocean

Fig. 4: Various sea states in the Baltic Sea and Atlantic Ocean

(P. Tanner)

  • 11  A voxels represents a single sample, or data point, on a regularly spaced, three-dimensional grid. (...)

21Voxels11 were used to check whether each grid point on the hull was submerged (fig. 4, top left), and if so, to exert the appropriate upward (flotation) pressure to counteract the gravitational weight thereby causing the vessel to ‘float’ in a realistic manner. The speed of the vessel was adjusted to suit each of the relevant wind strengths, and with the simulation running, the vessel was observed to see if the simulated ship remained afloat or if any seawater was taken onboard. Results indicated the ship remained afloat in the Baltic Sea-type sea conditions in any weather condition, but struggled to remain afloat in anything over 20 knots of wind in the Atlantic, when waves of 5 m led to large volumes of water breaking over the sides. If, as suggested by Ellmers (1994, p. 41), the deck of the cog did not form a watertight connection with the hull, but rather allowed water to flow directly into the bilges, such quantities of water breaking onto the deck as seen in the 5 m waves of the Atlantic during 20 knot winds would quickly overwhelm any attempts at bailing out with a bilge pump (fig. 4, bottom right).

8. Conclusion

22The Bremen-Cog, based on its hull shape, if restricted to not having the through-hull beams submerged, can carry a cargo of 45 tonnes, potentially increased to 60 tonnes if the ballast were replaced with cargo. At 2.25 m draught, each of the replica ships sail with beams wholly or partially submerged and the rebates for hull planking on the beam ends would suggest they were constructed in such a manner as to prevent water ingress. Archaeological evidence such as Doel 1 (Vermeersch, Haneca 2015) or Aber Wrac’h (L’Hour, Veyrat 1989), and iconographic representations depicting cogs, clearly show triangular or wedge-shaped blocks of timber attached to the exterior of the hull, adjacent to the through-hull beam ends. As discussed by Vermeersch and Haneca (2015, p. 123), these hemi-conical elements should be referred to as fairing blocks rather than fenders, as their design appears more to guide objects past the exposed square beam-ends than to protect against side impact. Perhaps the fairing blocks and rebated treatment of the through-hull beams indicates that having the beam ends submerged was not considered an issue (Waldus et al. 2019, p. 477). If this were the case the vessel could be loaded much deeper, to the Grågås Codex laws, allowing a cargo capacity of over 100 tonnes while maintaining a freeboard of 1.74 m.

23The archaeological evidence for vessels of the Bremen-type shipbuilding method confirm the presence of such vessels all over the Baltic Sea and the southern North Sea (Abel et al. 1969; Crumlin-Pedersen 1979; Adams 1990; Ellmers 1994; Hoheisel 1994; Weski 1999; Adams, Rönnby 2002; von Arbin, Daly 2012; Hocker, Daly 2016; Waldus et al. 2019). It is obviously a vessel well suited to this activity, for if it were not, it simply would not have flourished to such an extent (Ellmers 1994). Ellmers also noted the need for increased cargo capacity due to expanding trade and cites a cog mentioned in AD 1241 with a cargo capacity of about 240 tonnes (Ellmers 1994, p. 38). Hocker (Hocker, Ward 2004, p. 75) says of the Bremen cog, “As deep-water cogs go, it is of medium size, at 24 m long, with a capacity of 40 lasts (about 120 m³, which is about 80 metric tons of rye). In fact, it is smaller than nearly all contemporary accounts would suggest was typical. Medieval documents show that some Hanseatic cogs exceeded 100 lasts by the 1240s and cogs of 150 lasts were known in the fifteenth century.”

24It is not possible to state whether a vessel of the Bremen-type ever successfully completed a voyage to Iceland, or crossed the exposed Bay of Biscay, en route to the Mediterranean. Certainly, the historical record suggests that ships termed “cogs” were known at least in the Mediterranean (Springmann, Schreier 2008), but this use of the term might not always correspond to the same archaeological definition. Perhaps the larger cogs suggested by Ellmers and Hocker might be better suited to voyages such as crossing the Atlantic to Iceland. One possibility could be the Ijsselcog (Waldus et al. 2019): with a midship height of 5.8 m it is over 1.5 m higher than the Bremen-Cog, and almost 3 m longer. The Bremen-Cog as tested had a cargo of 61.25 tonnes and ballast of 15 tonnes leaving a static freeboard of 2.15 m. A similar quantity of cargo on the Ijsselcog would leave a static freeboard of 3.95 m.

25The Bremen-Cog would, as a cargo vessel, appear to be well suited to transporting cargo along coastal routes and relatively short sea crossings, taking circa two to three days on the sheltered waters of northern Europe. However, its flat bottom, which would be prone to slamming in a high sea, combined with the overall hull shape and performance characteristics would not indicate a vessel ideally suited to operations on the high seas of the exposed North Atlantic. It is the opinion of the authors that ships with the characteristics and dimensions of the Bremen-Cog would not be the primary choice for such an adventure.

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Notes

1  “Bremen-type” refers to the shipbuilding method defined on the base of the Bremen-Cog. It is used here to avoid the term “Cog/Kogge” for the archaeological/technical definition, which causes contradictions and misunderstandings (Belasus 2017).

2  The weight for Roland von Bremen has been attributed to the extra thick hull planking and thicker mast.

3  The still ongoing deformation processes are a subject of current research on monitoring of large-scale museum objects within preventive conservation by Amandine Colson, University of Bamberg, Germany.

4  The vessel remains were 3D-laser scanned in 2011 and 2014, and recorded using photogrammetry in 2014 by the German Maritime Museum.

5  This process is explained in detail in the reconstruction report on file at the German Maritime Museum, Bremerhaven, Germany (Tanner 2017a, p. 47-63).

6  This weight is based on using an average density for the oak, in this case 800 kg per m³ being typical for oak at 27% moisture content. This figure can be revised if the exact density of the PEG-treated oak is known.

7  The use of coefficients such as block, prismatic, midship, volumetric and slenderness coefficient are all values on a scale from 0 to 1. The values give no numerical values for what is good or below average.

8  For the timber elements, a density of 800 kg per m³ being typical for oak at 27% moisture content

9  For all conditions, a sail area of 100 m² plus three additional ‘bonnets’ of 33 m² each giving a total of 199 m² is used in Force 3 and 4 winds, and a mainsail alone of 100 m² for winds of Force 5 and above.

10  Fetch is the distance of open water that the wind blows over.

11  A voxels represents a single sample, or data point, on a regularly spaced, three-dimensional grid. This data point can consist of a single piece of data, such as an opacity, or multiple pieces of data, in this case each voxel would continually check if it were submerged or no, and if submerged apply the relevant buoyant force to the vessel.

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Table des illustrations

Titre Fig. 1: Comparison of the digital data sets
Légende The colour coding is as follows: blue is the hull shape from Lahn’s section drawings; green is the hull shape from Lahn’s lines plan drawings; and red is the hull shape during 3D laser scanning in 2014.
Crédits (P. Tanner)
URL http://journals.openedition.org/archaeonautica/docannexe/image/2699/img-1.jpg
Fichier image/jpeg, 643k
Titre Fig. 2: Top left, unfair strake runs; top right, strake runs not matching archaeological evidence; bottom left, reverse camber in castle deck; bottom right, transom beam bolted (yellow) 80 mm below existing hole (circled red)
Crédits (P. Tanner)
URL http://journals.openedition.org/archaeonautica/docannexe/image/2699/img-2.jpg
Fichier image/jpeg, 874k
Titre Fig. 3: Top left, difference between Lahn and reconstructed hull at Frame 10; top right, difference between two hull forms; middle left, archaeological remains 3D modelled; bottom left, missing elements extrapolated; bottom right, fully reconstructed hypothetical reconstruction of the Bremen cog
Crédits (P. Tanner)
URL http://journals.openedition.org/archaeonautica/docannexe/image/2699/img-3.jpg
Fichier image/jpeg, 876k
Titre Fig. 4: Various sea states in the Baltic Sea and Atlantic Ocean
Crédits (P. Tanner)
URL http://journals.openedition.org/archaeonautica/docannexe/image/2699/img-4.jpg
Fichier image/jpeg, 2,1M
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Pat Tanner et Mike Belasus, « The Bremen-Cog: reconstructed one more time »Archaeonautica, 21 | 2021, 315-324.

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Pat Tanner et Mike Belasus, « The Bremen-Cog: reconstructed one more time »Archaeonautica [En ligne], 21 | 2021, mis en ligne le 01 juillet 2022, consulté le 08 décembre 2024. URL : http://journals.openedition.org/archaeonautica/2699 ; DOI : https://doi.org/10.4000/archaeonautica.2699

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Auteurs

Pat Tanner

Centre for Maritime Archaeology, University of Southampton, Southampton, UK

Mike Belasus

Saxo-Institute, University of Copenhagen, Copenhagen, Denmark

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