LS10.21 PROBABLE ERRORS OF POSITION

Section: LS10 SAR Operations

Date: 20th September 2016

Purpose

Page: 1 of 4

To outline factors that may cause probable errors of position when planning and undertaking a SAR activity.

Policy

Surf Life Saving NSW (SLSNSW) provides the following guidelines to assist personnel in effectively performing their duties.

Procedure

Drift Error for Waterborne Targets

Over land, the datum is the last known position; however when survivors are known or thought to be in or on the water an allowance must be made for movement of the water resulting from the effects of wind and current. The degree of displacement of the datum from the last known position assumes increasing importance with the passing of time, and MUST be allowed for in search planning. Survival Craft Drift, as the displacement is called, is a function of:

1. The average sea current;

2. The average wind current; and

3. Leeway.

Sources of information include data held by the SurfCom, vessels passing through the search area, and individuals with local knowledge.

The direction and speed of these factors is referred to as ‘SET’. Contrary to the convention of expressing wind velocity, the direction component indicates the direction of movement. The speed component is usually quoted in knots. Care must be taken to ensure that the speed unit is both stated and interpreted correctly.

Sea Current

Tidal and local geographic features may affect sea currents near the coast. When areas near the coast are to be searched, the water movement for the area should be discussed more fully with local experts.

Tidal Streams

Tides are caused by the gravitational pull of the moon and sun, modified by the depth and shape of the sea basin along the coastal areas. Currents in coastal waters are usually affected by tides, changing in predictable velocity as the state of the tide changes. In some locations tidal streams are of the reversing type, abruptly changing direction 180 degrees at about the time of high and low water. In other places the direction will change in small increments so as to create a constant rotary movement. Variations of these tidal effects may also be found.

The exact effect of the tide on currents in any specific area may be found by consulting tide tables or local charts. Local knowledge is again of great value in dealing with movements of tidal streams. While the changes in direction of tidal streams have a tendency to nullify the cumulative effect, they must nevertheless be considered in computing drift for the following reasons:

1. Often, with reversing streams, the effect in one direction is greater than in the other so that, over a period of time, the resultant effect is more in one direction than in the other.

2. Even over short periods of time the flow of tidal streams will cause significant changes in the probable position of a search object.