All dates shown inOceanography and Meteorology section use Coordinated Universal Time (UTC) reference(UTC). Local time in the Iberian Peninsula and the Balearic Islands UTC is UTC+1 in winter time and UTC UTC+2 in summer time. In the Canary Islands the convention for local time is UTC UTC+0 in winter time and UTC UTC+1 in summer time. Therefore, to translate the dates shown on this web into winter local time, it is necessary to add 1 hour in case of the Iberian Peninsula or Balearic Islands, but nothing has to be done in case of the Canary Islands where UTC and winter local time are coincident During the summer time use, the local time in the Peninsula and Balearic Islands is obtained by adding 2 hours to the dates shown here and 1 hour for the Canary Islands. UTC.
Click on the item Oceanography from the menu on Puertos del Estado main page. That will take you directly to the Forecast, Real Time and Climate Section. Information is clasified by parameters and organised in three main sections: Forecasts, Real Time Data and Historical Data. When choosing Waves on the Real Time Data menu, all the available buoys will be displayed on the map. Click on the station closer to your area of interest. Then, a floating window will come up. Clicking on the menu, users can choose to visualize plots or tables of the time series. The most representative parameters of waves are significant height (Hs), mean period (Tm), peak period (Tp) and peak direction (Dirp, direction of the most energetic waves).
SIGNIFICANT HEIGHT (Hs). It is one of the most widely used parameters of waves. Significant height represents the height of waves that a trained observer would determine with the naked eye from an observing position (not from the coast). It is accepted to be equivalent to the mean value of the 1/3rd highest waves recorded in the measuring interval.
MEAN PERIOD (Tm). Describes the mean value of the period from the waves recorded in the measuring interval.
PEAK PERIOD (Tp).Is the period of the most energetic group of waves. The more regular are waves, the more Tp and Tm look alike, though usually Tp is bigger than Tm.
PEAK DIRECTION (Dirp). Describes the direction of the most energetic group of waves.
Traditionally the description of the wave conditions at a certain location and time is characterized by some parameters that define the sea state. Nowadays the sea state can be assessed through instruments like buoys (scalar and directional). In case of Puertos del Estado buoys, every hour they record instant elevations of sea level for a time interval in which the sea state can be considered to be constant. This duration (e.g. 20 minutes) depends on the buoy model and will be enough to obtain a representative sample of the wave conditions in that hour. In case of Puertos del Estado buoys, every hour they record instant elevations of sea level for a time interval in which the sea state can be considered to be constant. This duration (e.g. 20 minutes) depends on the buoy model and will be enough to obtain a representative sample of the wave conditions in that hour. Then the time series of instant elevations is processed using standard methods (zero crossing and spectral analysis) to determine the parameters that characterize the sea state in that hour: Hs,Tm,Tp, etc. Today, all this process is usually done on board the buoy and later the outputs are transmitted to land. Though, the scalar buoys of the Coastal Network still transmit the measured sample of elevations to a station on land where the analysis is performed.
The strongest storms in Spain are usually detected in the Northwestern Coast (Galician coast). In this area storms mainly come from the north-est. They cause highest waves with largest periods because they are generated in the North Atlantic and then propagated to the Galician Coast (when waves get older the period grows). These are the most characteristic storms in this area and can produce waves up to significant height of 10 meters with maximum wave height of 17 meters and wave periods up to 20 seconds. I would like to know how to interpret the wave, wind and currents directions measured by the buoys.
The zero angle indicates the geographic north and the angles increase clockwise.In general, when we talk about buoy-measured waves and wind data, angles indicate the "coming from" direction. Nevertheless, when we talk about measured sea currents directions it is usually accepted that angles indicate the "going to" direction (propagation).However, when talking about modelled data these criteria change. It is generally agreed that modelled waves and wind as well as sea currents angles show the propagation direction.
No, we do not make any correction due to magnetic declination because it is different in every position and it changes in time. But we take it into account, if necessary.
Puertos del Estado has two buoy-based monitoring networks providing real-time waves measurements: Deep Water Network and Coastal Network. Deep Water buoys are moored in the open sea (more than 200 meters depth), far away from the coast line. Therefore, measurements are not affected by coastal and local phenomena and characterize the open sea waves in the area around the buoy. When using this kind of data for coastal studies, users mus be aware that the characteristics of waves at the sea side will be affected by the dominant direction of the open sea waves, but also by the sea ground and the coast line shape. In these cases, it would be advisable to propagate deep sea data to the coastal location of interest. Coastal buoys are moored in swallow waters, in the vicinity of the port facilities (less than 100 meters depth). In most of the cases, measurements are affected by the shape of the coast line and the sea ground. This means that they obtain information that is only representative of the local conditions. Therefore, these data must be used carefully to draw conclusions in areas away from the buoy position.
Click on the item Oceanography from the menu on Puertos del Estado main page. That will take you directly to the Forecast, Real Time and Climate Section. Information is clasified by parameters and organised in three main sections: Forecasts, Real Time Data and Historical Data. When choosing Sea Level on the Real Time Data menu, all the available tide-gauges will be displayed on the map. Click on the station closer to your area of interest. Then, a floating window will come up. Clicking on the menu, users can choose to visualize plots or tables of the time series.
A basic aspect to work with sea level data is the reference or zero. In Spain, the Geographic National Institute (Instituto Geográfico Nacional, IGN) is responsible of establishing the national references of heights in land. In the Spanish Iberian Peninsula the reference is the mean sea level measured in Alicante (NMMA) (Nivel Medio del Mar en Alicante). In the islands (Balearic and Canary Islands), the local mean sea level is used. This value is obtained using the sea level data from a tide gauge located in the island. For example, heights in Tenerife Island will be refered to the Mean Sea Level in Tenerife, and so on... Every harbour, on its own, define an adecuate reference or zero for dredge, operations, works etc. It is known as the harbour zero and usually matches up with the lowest low tide. All the sensors in the Spanish Harbour System Tide Gauge Network (REDMAR) use the harbour zero for the reference of sea level measurements. This reference value is supposed not to change, unless the corresponding Harbour Authority demands a new definition of the harbour zero. The relation between the harbour zero and the National Reference of Heights (NMMA or equivalent on islands) is shown in our web site when available as well as a bench mark sheet that shows a diagram of the datums comparison. This information comes from high precision levelings that have been made in cooperation with IGN using its methodology and is updated when a new leveling is made. To check the zero and bench mark information Click on the item Oceanography from the menu on Puertos del Estado main page. That will take you directly to the Forecast, Real Time and Climate Section. Select Sea Level from Real Time or Historical Data menu. Then, once the tide gauge pop-up window opens, select the Datums tab.
Yes, users can check and download information from our monitoring networks and forecast systems:
1) Online access to data base. In the Historical Data section through clickable maps, users have access to waves, sea level, wind and sea currents, salinity and temperature data. The most representative information collected is available since the beginning of measurements in every station that has ever been part of our monitoring networks. For some of these parameters there is also available information of modeled data obtained from the analysis of the forecast system.
2) Annual Reports. Periodically we process the data collected in every station for the meteorological year (December to November) to obtain plots and statistics. The resulting reports are posted on the web. To download them click on the parameter of interest at the Historical Data menu. Then, all the available sources of information will be displayed on the map. Select the station closer to your area of interest. Annual Reports is the first item in the menu that will pop up. Users just have to choose the year and the section (reports have been splitted to speed up downloads).
3) Waves an Sea Level Long-term and Long-term Extreme values Reports are available when measured time series are long enough to be statistically representative. These reports are accessible choosing waves and sea level parameters in the Historical Data section. To download them click on the parameter fom the menu. Then, all the available sources of information will be displayed on the map. Select the station closer to your area of interest. Reports, if avaliable, are placed under the chapter heading "Global Reports" in the menu that will pop up.
4) Data Request. If any of the above-mentioned sources of information does not cover the user needs, we also have an online service to request and download measured and modelled data time series. The download process is centralized from the Historical Data menu on the Oceanography web section. The access to this service is completely open and free of charge, with a limit of 5 files on each request. There is no limitation in the length of the time series, with the exception of tide gauge data, due to its sampling rate the resulting file sizes are very large. After the request is registered users will receive an e-mail with the links to download the data. Since that moment, files will be available for 10 days. For more information about this service, please, read the following user guide.
A wave pattern on the ocean can be shown to comprise a number of groups of simple waves, each group with its own period. The Mean Period is the mean of all the periods and in Spanish is denoted by Tz and the period of the most energetic wave group is the Peak Period and in Spanish is denoted by Tp. The more regular the wave pattern is, the more similar are the Mean and the Peak periods, but normally the Peak Period is higher than the Mean Period.
The wave height is different from one wave to another so a useful concept is the Significant Wave Height that approximately corresponds to the averaged height of the one third highest waves. It is denoted by Hs or Hm0.
The wind sea is composed by irregular short waves that are being generated by the wind and are still growing. They usually have foam in the crests. The swell is composed by regular long waves that have been generated in a different place and propagate up to the area of interest. The total sea (in Spanish Mar Total) is the composition of wind sea and swell. In open waters it is easy to find swell coming from a place far away and wind sea that is being generated at the area of interest. Sometimes it can be observed two different swells at the same time, with different directions and periods. In these situations we will call "mar de fondo 1" to the most energetic swell and "mar de fondo 2" to the other.
The waves that could be found at the beach will depend on the wave direction in the open sea, on the sea bottom and on the coast line. There is not a general rule to estimate the waves at the coast from the waves at open waters. Depending on the beach characteristics the waves will be different from a place to another. The most important parameter for this estimation will be the beach orientation and the wave direction in open sea.
The wind, which in this forecast is denoted by Vv, is the 10 meter high wind over the sea surface. This wind must be consider at open waters because at the coast the wind can be very affected by the orography and the terrain.
The zero indicates the geographic north and the angles increase clockwise. Sometimes the direction indicates the "coming from" direction and in other times the direction is the propagation or the "blowing to" direction. This aspect is always indicated in the table, map or graphic that is being consulted.