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has gloss(noun) a strong surface current flowing outwards from a shore
riptide, rip current
has glosseng: A rip current is a strong channel of water flowing seaward from near the shore, typically through the surf line, and can occur on any shore that has breaking waves. Rip currents cause 80% of rescues by beach lifeguards.
has glosseng: A rip current is a strong surface flow of water returning seaward from near the shore (not to be confused with an undertow). It is often mistakenly called a "rip tide" or "riptide", though the occurrence is not related to the tides. Colloquially a rip current is known simply as a rip. Although rip currents would exist even without the tides, tides can make an existing rip much more dangerous (especially low tide). Typical flow is at 0.5 meters per second (1-2 feet per second), and can be as fast as 2.5 meters per second (8 feet per second). Rip currents can move to different locations on a beach break, up to tens of metres (a few hundred feet) a day. They can happen at any beach with breaking waves, including the world's oceans, seas, and large lakes such as the Great Lakes in Canada and the United States.
lexicalizationeng: rip current
lexicalizationeng: riptide
subclass of(noun) a steady flow of a fluid (usually from natural causes); "the raft floated downstream on the current"; "he felt a stream of air"; "the hose ejected a stream of water"
stream, current
Meaning
Catalan
lexicalizationcat: corrent de ressaca
Czech
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Danish
has glossdan: Et hestehul eller revlehul er et hul i en revle, hvor der kan dannes en kraftig udadgående lokal og midlertidig strøm. Revlehullerne ligger med 100-400 meters interval langs (sand)stranden og opstår, når der er tilstrækkeligt meget vand inden for revlen grundet bølger, som giver et pres, der danner en udadgående strøm gennem revlen.
lexicalizationdan: revlehul
German
has glossdeu: Brandungsrückströme (auch Rippströmung oder Trecker, englisch: riptides oder genauer rip currents) sind an den Meeresküsten die wichtigste Ursache für Badeunfälle.
lexicalizationdeu: Brandungsrückstrom
lexicalizationdeu: Brandungsrückströmung
lexicalizationdeu: Rippströmung
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French
has glossfra: Un courant darrachement, flot de retour, courant de déchure ou courant sagittal, est un fort courant de retour qui entraîne en direction du large les eaux apportées par les grosses vagues qui se brisent sur les plages . Ce courant peut être accentué par la marée basse. Le flux caractéristique de ce courant est dentre 0,5 et 2,5 mètres par secondes et peut changer de place le long de la plage selon la marée et la houle au large.
lexicalizationfra: courant d'arrachement
Galician
has glossglg: Unha corrente de resaca é unha forte corrente superficial (ou case superficial) de auga, que retrocede desde a costa cara o mar. Xérase fundamentalmente no rompemento irregular das ondas ao longo da crista, chegando bruscamente á praia cun índice elevado de enerxía, desvanecendo logo sobre o fondo para, posteriormente, regresar cara ao mar por un carreiro a través das ondas.
lexicalizationglg: Corrente de resaca
Italian
has glossita: La corrente di ritorno o risacca (in inglese rip current) è un tipo di corrente marina molto pericolosa.
lexicalizationita: corrente di ritorno
Japanese
has glossjpn: 離岸流(りがんりゅう)とは、海岸の波打ち際から沖合に向かってできる潮の流れのこと。幅10m前後で生じる局所的に強い引き潮。
lexicalizationjpn: 離岸流
lexicalizationjpn: riganryū
lexicalizationjpn: りがんりゅう
Korean
lexicalizationkor: 심적 갈등
lexicalizationkor: 이안류
lexicalizationkor: 조충
Dutch
has glossnld: Een muistroom is de benaming voor de onderstroom van water nabij de kust. De onderstroom is namelijk niet gelijk verdeeld langst de kust, maar zal zich in een geconcentreerde vorm voordoen.
lexicalizationnld: muistroom
lexicalizationnld: mui
Norwegian
has glossnor: Rip current (ordet kommer fra engelsk) beskriver et rift i sjøen, der sterke lokale vannmasser strømmer utover. En rip current er mellom 5 og 30 meter bred. Den oppstår i intervaller på mellom 100 og 400 meter på badestrender.
lexicalizationnor: rip current
Polish
lexicalizationpol: prąd odpływowy
Portuguese
has glosspor: O que são Correntes de Retorno? As correntes de retorno podem ser definidas como o refluxo do volume de água que retorna da costa de volta para o mar, em virtude da força gravitacional. Também é conhecida como maré de retorno, rip current ou simplesmente vala, devido ao canal rompendo o banco de areia criado pelo o escoamento da água. Apesar das correntes de retorno existirem independentemente ao fenômenos das marés, as marés podem intensificar o perigo das correntes de deriva, em especial na maré baixa. A velocidade do fluxo de água retornando ao mar pode variar de 0,5m/s a até 3,5m/s.
lexicalizationpor: Corrente de retorno
Swedish
has glossswe: En ripström är ett fenomen som uppstår när vatten sköljs över ett hinder, som till exempel ett sandrev. Vattnet kan då inte strömma tillbaka under det inkommande vattnet utan kanaliseras tillbaka genom smala öppningar i revet. Strömmarna kan bli väldigt starka och om man fastnar i en sådan ström kan man dras iväg fort och långt ut från stranden. Man ska aldrig simma rakt mot en ripström.
lexicalizationswe: ripström
Links
part of(noun) the periodic rise and fall of the sea level under the gravitational pull of the moon
tide
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Media
media:imgBackcomp-clean.gif
media:imgBackcomp-it.gif
media:imgBackcomp.gif
media:imgDanger courant baines.jpg
media:imgHanakapiai Beach Warning Sign Only.jpg
media:imgRip current.PNG
media:imgRipfromabove.jpg

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