(Table 1) Relative phase shift at moorings F1, F2, F3 and F4 for different oscillations
Cobertura |
MEDIAN LATITUDE: -74.349100 * MEDIAN LONGITUDE: -36.189500 * SOUTH-BOUND LATITUDE: -74.514700 * WEST-BOUND LONGITUDE: -36.604700 * NORTH-BOUND LATITUDE: -74.155000 * EAST-BOUND LONGITUDE: -35.703300 * DATE/TIME START: 1998-01-22T13:00:00 * DATE/TIME END: 1999-02-23T13:00:00 * MINIMUM ELEVATION: -1984.0 m * MAXIMUM ELEVATION: -647.0 m |
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Data(s) |
07/03/2009
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Formato |
text/tab-separated-values, 50 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.808591 doi:10.1594/PANGAEA.808591 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.808593 Darelius, Elin; Smedsrud, Lars Henrik; Østerhus, Svein; Foldvik, Arne; Gammelsrød, Tor (2009): Structure and variability of the Filchner overflow plume. Tellus Series A-Dynamic Meteorology and Oceanography, 61(3), 446-464, doi:10.1111/j.1600-0870.2009.00391.x |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Bjerknes Centre for Climate Research |
Palavras-Chave | #Elevation of event; Endurance; Event label; F1; F2; F3; F4; Latitude of event; Longitude of event; Mooring (long time); MOORY; Oscillation; Phase shift, relative; Phase shift, standard deviation; ROPEX; Station; Weddell Sea |
Tipo |
Dataset |