K5 wave buoy (64045) with the GeoGarage platform (UKHO chart)
Buoy K5 (a part of the UK Met Office’s network of Marine Automatic Weather Stations,
or MAWS)[59°07.3'N, 11°42.5'W, elevation: 0m)]
Record Value : 19.0 m (62.3 ft) (Instrumentation Datawell heave sensor )
Date of Record : 0600 UTC 4/02/2013
A World Meteorological Organization expert committee has established a new world record significant wave height of 19 meters (62.3 feet) measured by a buoy in the North Atlantic.
The wave was recorded by an automated buoy at 0600 UTC on 4 February 2013 in the North Atlantic ocean between Iceland and the United Kingdom (approximately 59° N, 11° W).
It followed the passage of a very strong cold front, which produced winds of up to 43.8 knots (50.4 miles per hour) over the area.
The previous record of 18.275 meters (59.96 feet) was measured on 8 December 2007, also in the North Atlantic.
Note that this is "significant" wave height -- in essence, what an observer would have seen if he/she averaged over 15-20 waves passing by the buoy -- that is a much better thing than "rogue waves" which really cannot be accurately measured.
According to one of our of panel's "wave experts": "There have been many more less reliable estimates of rogue waves from other platforms, and from satellite SAR. These are generally unverifiable, since there is no ground truth for the satellite, and the others tend to be from pitching and rolling platforms such as ships, and estimates are often based on damage to the superstructure, which may not have been level at the time."
Significant wave height recorded is four times the RMS value of the water level above the average level of the water surface measured over a 17½ minute period.
The factor of 4 applied to the RMS value is because the waves are trochoidal in nature.
(Waves at sea, especially those growing under the influence of the wind, tend to be short-crested, i.e. the wave crests project further above the mean level than the troughs are below it.)
The ‘average’ wave period, again over a 17½ minute sample, is the average of the periods over 7 successive 2½ minute samples (each determined from the number of wave cycles in the sample).
Figure (above) shows the hourly significant wave heights from the Datawell heave sensor, together with the wave measurements from the Triaxys sensor.
The Committee consisted of scientists from the United Kingdom, Britain, Canada, the United States of America and Spain.
The buoy (K5) which recorded the wave is a part of the UK Met Office’s network of Marine Automatic Weather Stations.
Moored and drifting buoys form a vital part of an extensive international observing network coordinated by WMO and its partners.
They complement ship-based measurements and satellite observations which monitor the oceans and forecast meteorological hazards on the high seas.
During the period of the highest waves the wind speeds measured on the buoy were over 35 kn for the 12 hours preceding the highest waves, with a maximum wind speed reported of 43.8 kn, as shown in Figure 2 above.
The winds were measured using a Gill windsonic (acoustic) anemometer on the buoy at around 3½m above sea level.
The synoptic situation at 0600 on 4th February shows an intense depression to the north of the buoy with prolonged strong westerly to northwesterly winds at the K5 station.
Record was evaluated by the committee of J. Turton, M. Brunet .T. Peterson, V. Swail, and R. Cerveny.
“It highlights the importance of meteorological and ocean observations and forecasts to ensure the safety of the global maritime industry and to protect the lives of crew and passengers on busy shipping lanes,” he said.
“We need high quality and extensive ocean records to help in our understanding of weather/ocean interactions,” said Dr Zhang.
“Despite the huge strides in satellite technology, the sustained observations and data records from moored and drifting buoys and ships still play a major role in this respect,” he said.
A separate record – that of the highest significant wave height as measured by ship observation – was measured in February 2000 in the Rockall Trough, also in the North Atlantic between the UK and Iceland.
Wave height is defined as the distance from the crest of one wave to the trough of the next.
The term “significant wave height” means the average of the highest one-third of waves measured by an instrument, and is comparable to what an observer would see as an average of about 15-20 well-formed waves over a period of about 10 minutes.
The highest waves typically occur in the North Atlantic, rather than the Southern Ocean.
Wind circulation patterns and atmospheric pressure in the North Atlantic in winter leads to intense extra-tropical storms, often so-called "bombs".
This means that the area from the Grand Banks underwater plateaus off the Canadian coast around Newfoundland to south of Iceland and to the west coast of the UK, including the Rockall Trough, are prime candidates for wave records.
K5 buoy (64045)
conditions for Monday 4th of February 2013
Weather & Wave data
(courtesy of Weather Underground)
“The new world record will be added to the official WMO archive of weather and climate extremes which is being constantly updated and expanded thanks to continued improvements in instrumentation, technology and analysis,” said Randall Cerveny, Joint Rapporteur on World Records of Climate and Weather Extremes for WMO.
Data buoy center
“Oceans cover some 70 per cent of the world’s surface. Ocean observations are therefore critical to understanding and forecasting our weather and climate,” he said.
The archive includes the world’s highest and lowest temperatures, rainfall, heaviest hailstone, longest dry period, maximum gust of wind, as well as hemispheric weather and climate extremes.
A WMO committee of experts earlier this year established two new records - the longest reported distance and the longest reported duration for a single lightning flash in, respectively, Oklahoma (United States of America) and southern France.
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