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As soon as the position-finding vessels stop, stop likewise or move at creeping pace; when position-finding vessels start on again, do the same, in certain cases at a higher speed, with considerable alteration of course. |
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This procedure has been successfully carried out by some boats. |
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If the foregoing manner of defence against position-finding is not successful, remain at the bottom as far as possible, by way of defence against depth-sounding. This appears to be particularly efficacious in the case of great depths, since differences of 6-8 metres are then difficult to estimate. |
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If the bearings have been lost, the English destroyer appears to steer a searching curve (similar to our Berghoff curve). As this course is built on the assumption of a constant course and speed on the part of the U-boat, it should be possible to outmaneoeuvre it accordingly. It is possible that in the above described procedure the bearing is obtained by means of a horizontal sounding apparatus. |
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A position-finding apparatus similar to our S-device must in any case be reckoned with. Experiments with our S-device have shown that the quality and strength of the echo depends on the submerged depth of the boat one is sounding for, and mostly decreases as this depth increases. |
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By listening to the enemy's sound impulses the most favourable depth may therefore be determined in certain cases. |
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The more faintly the impulses are heard, the smaller is the echo that the enemy detects. |
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*"It is always best to show a narrow silhouette. At a greater distance it is better to take the enemy from ahead than from astern, until the most favorable depth is ascertained. Lie on the bottom only if there is no other possibility left" |
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Conditions of position-finding. |
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The accuracy of position-finding was at first very poor, of late it is often very good, but only in a few cases continuously effacious and successful. An unfavorable effect on position-finding is produced by a marked water stratification, such as is found in front of estuaries and in certain sea areas. A stratification of this kind is e.g. well known to us in the Skagerrak, appearing specially in the spring, early summer and autumn, and rendering our own position-finding very |
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* slip in ordinary typescript pasted on, marked in red ink "to 4)" |
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