Transporte de massa por ondas internas não lineares - INTIFANTE 00 = Mass transport by non linear  internal waves - INTIFANTE 00

dc.contributor.author	Clemente, Catarina
dc.contributor.author	Coelho, Emanuel Ferreia
dc.contributor.author	Vitorino, João Paulo do Nascimento
dc.date.accessioned	2025-08-01T14:45:28Z
dc.date.available	2025-08-01T14:45:28Z
dc.date.issued	2002
dc.description	3.ª Assembleia Luso-Espanhola de Geodesia e Geofísica, Valência, 4-8 de fevereiro de 2002
dc.description.abstract	Packets of non-linear internal waves were observed in 3 moorings on the southwest Portuguese shelf during 15 to 18 October 2000. The observed temperature in the first mooring shows a vertical displacement of about 50m to 35m during the passage of non-linear internal waves with duration of about 3h. The first empirical mode dominated the motion with the first eigenvalue with 66% on the 16''', 86% on the ]7lh and 74% on the 1 Ef" day of October. With this assumption, we will discuss the mass transport by non-liner internal waves using the methodology of lnall et al (2001) applied to the southwest shelf near Setubal canyon
dc.description.sponsorship	Universidade Politécnica de Valência
dc.language.iso	por
dc.subject	Marés internas
dc.subject	Massas de água
dc.subject	Canhões submarinos
dc.subject	Setúbal (Portugal)
dc.subject	Reuniões internacionais
dc.title	Transporte de massa por ondas internas não lineares - INTIFANTE 00 = Mass transport by non linear internal waves - INTIFANTE 00
dc.type	Article