Top Australian navigator Adrienne Cahalan shares some expert tips on using currents on bluewater passages and ocean racesThere are a number of yacht races around the world in which strategic decisions on whether to go into or out of ocean currents can have a significant impact on how the race is won or lost. Ocean currents can be driven by wind (surface ocean currents), tides (estuary or near shore) or other factors such as water density. The Coriolis effect which deflects winds to the right in the northern hemisphere and to the left in the southern hemisphere also deflects major surface ocean currents to the right in the northern hemisphere in a clockwise spiral, and to the left in the southern hemisphere, counter-clockwise. These major spirals of ocean-circling currents are called ‘gyres’ and are found in the North Atlantic, South Atlantic, North Pacific, South Pacific and Indian Ocean. On the east and west edge of the gyres are boundary currents. The California, Humboldt (Peru) and Canary currents are examples of eastern boundary currents, which are characterised as shallow, broader and slower flowing. Western boundary currents such as the north-flowing Gulf Stream and Kuroshio (Japan), the south-flowing East Australian Current and Agulhas (South Africa) are characterised as faster flowing, deeper and narrower. Information on the rate and direction of ocean currents via the Global RTOFS (Real-Time Ocean Forecast System) model is easily accessed through navigation software programs that download data in GRIB format. Once you have obtained the current data the race strategy decision-making begins. In a Sydney Hobart Race, for example, if you are in a 100-footer then current as a percentage of boat speed is negligible; so sailing 12-15 miles further off course to get into current that will assist you at up to 2-3 knots may not be beneficial in the overall strategy of the race. Another important consideration is the effect on the sea state of wind against current. The East Australian Current has broken many boats when warm waters in a 2-3 knots south-flowing current meet cold, south-westerly winds as cold fronts travel up along the New South Wales coast, generating short, steep seas that can snap masts and delaminate hulls. For smaller boats in the Rolex Sydney-Hobart Race there can be a clear trade-off between extra mileage and sailing further to find favourable current. Once racing, it is up to the navigator to monitor the current relative to the observed conditions and forecast. When observing current on board, it is useful to know that there are differences in the way data is calculated and displayed through different instrument systems (eg B&G, Ockam) or navigation software packages (eg Expedition, Deckman, Adrena). Current/tide data is displayed as knots for rate and degrees for direction. Nick White is the software designer and owner of the tactical racing software program Expedition. He explained that Expedition calculates tide/current direction and rate from data output by the instrument system. There are pre-set current and drift calculations in Expedition, however these are for use where the instruments don’t provide it. In his experience the instrument system (eg H5000) has more precise and timely data. Mike Sugden from Navico, which manufactures the H5000 and B&G products including Deckman for Windows, explains that B&G and Deckman calculate tide and drift differently. On B&G Instruments tide is calculated from the difference between boat speed and SOG/heading and COG, whereas in Deckman the tide is calculated by comparing dead reckoning (course and boat speed) and the GPS fix position. In this case, it is really important to have calibrated boat speed, heading and leeway (if enabled). In Deckman the output can be adjusted to average over a specified number of minutes depending on the user’s preference. Leeway can be taken into account in current calculation but is not necessarily measured on a simple instrument or software package. However, when more boat speed devices come onto the market that can measure leeway accurately, there will be improvement in tide and drift calculations.