![]() ![]() 1D), or click the table icon to select a particular period that you are interested in (Fig. 1B), click on the movie icon for a movie of daily images surrounding a particular date (Fig. You can explore the data in several ways click on the calendar icon to look at a specific date (Fig. ![]() 1E) explains the datasets and what is shown on the graphics. The information icon at the top menu (Fig. 1A) provides information and references about the mooring and the dataset. The ‘ About the EAC mooring array dataset’ button (Fig. In recognition of this knowledge gap, IMOS and CSIRO launched a flagship effort between 2012-2022 to measure the EAC with a moored array of instruments, continuously, over a decade-long period. To complement the publication of this dataset, we are very excited to announce the publication of daily visualisations of the moored-array data, seen in the context of satellite observations, here in the IMOS-OceanCurrent website.Įxplore the EAC by clicking on the ‘EAC Mooring Array’ button in the menu on the right, in the website’s frontpage. But do we know its vital statistics?Īctually, not until now (other than from a handful of brief field campaigns or modelling exercises). The East Australian Current (EAC) is Australia’s most influential ocean feature. How strong is the East Australian Current? The science is finally in.īernadette Sloyan, David Griffin, and Gabriela Pilo 13 October, 2023 You should in any case be extremely wary swimming around exposed coasts and straits.Noticed something interesting, on this website, or on the water? Hence stick to sheltered bays unless you understand exactly what you’re doing which involves careful planning using the relevant tidal stream atlas. A world-class swimmer travels at a sprint speed of around 4 knots, while dolphins cruise at 6-7 knots. To put these speeds into perspective, A mature river typically flows at 3 knots and a steep whitewater river at 6.5 knots. Places in the UK with tidal races include the Pentland Firth between the northern coast of Scotland and Orkney at 10 knots, the Menai Straits between mainland Wales and the island of Anglesey at 8 knots. The average speed of the water there is 7-9 knots, increasing to an estimated 20 knots which creates large whirlpools. The Skerstadfjord fills and empties through a narrow gap about 150 metres wide. While uninterrupted tidal streams seldom flow at more than 2 knots (2.3 mph or 3.7 kph), the fastest current in the sea is at the Saltstraumen near Bodø, in Norway. Thus currents are correspondingly stronger on springs than on neaps. On spring tides, where you will remember the low tide is lower, and the high tide is higher, more water is moving further between those two extremes. And there can be other places where swimming is safer at low tide. Do also be aware, however, that while it’s generally safer in most places to swim on a slack tide, the actual times of slack water may vary from the official tide times depending on local geography and weather conditions. But this can vary, with different conditions in some places so it’s vital that you always check local conditions. The slack tide is in many places one hour either side of high or low tide, and in some places the water barely moves. The significance of tides is in understanding that more water moves during the middle two hours of both an incoming ( flood) and outgoing ( ebb) tide this results in stronger currents. In general, learn to read websites, tide tables and sea charts and to understand them, and ask experienced local swimmers, sailors and other knowledgeable experts in how the water behaves at the place you are considering a swim. Magic Seaweed is a useful website for checking sea conditions in general, wave and swell heights, tides, and forecasts for your local area and all around the world. in Dorset where the North Sea tides meet Atlantic tides). Others have mixed tides where tides from two directions meets (e.g. Some places have semi-diurnal tides (two high tides at roughly 12 hour intervals, interspersed with two low tides). The actual heights and intervals of tides vary according to where you are. Spring tides are more extreme, so a low spring will be lower than a low neap while a high spring will be higher than a high neap. Spring tides occur at full moon and new moon, approximately every 2 weeks. The short answer is that the sea, depending on where you are in relation to the earth’s axis, is affected by the gravitational pull of the moon and sun relative to earth. High tide seas swell and billow like the sails on a galleon and take on a new depth and richness of colour. The water at low tide often appears sparser, flatter, less dense. Firstly the view is entirely different miles of damp sand and exposed rocks, versus a tiny ridge of weeds and dry sand. The sea at low tide is a very different animal from the same sea at high tide, particularly on a spring. ![]()
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