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Description:<\/SPAN><\/P> Seasonal sigma-t climatology of the Northeast Pacific Ocean was computed from historical observations including all available conductivity-temperature-depth (CTD), bottle, expendable bathy-thermograph (XBT), and Argo data in NOAA (http://www.argo.ucsd.edu/), Marine Environmental Data Service (MEDS), and Institute of Ocean Sciences archives over 1980 to 2010 period.<\/SPAN><\/P> Methods:<\/SPAN><\/P> Calculations, including smooth and interpolation, were carried out in sixty-five subregions and up to fifty-two vertical levels from surface to 5000m. Seasonal averages were computed as the median of yearly seasonal values. Spring months were defined as April to June, summer months were defined as July to September, fall months were defined as October to December, and winter months were defined as January to March. The data available here contain raster layers of seasonal sigma-t climatology for the Canadian Pacific Exclusive Economic Zone (EEZ), a subset of seasonal climatology of the Northeast Pacific Ocean, in high spatial resolution of 1/300 degree.<\/SPAN><\/P> References:<\/SPAN><\/P> Foreman, M. G. G., W. R. Crawford, J. Y. Cherniawsky, and J. Galbraith (2008). Dynamic ocean topography for the northeast Pacific and its continental margins, Geophys. Res. Lett., 35, L22606, doi: 10.1029/2008GL035152<\/SPAN><\/P> Data Sources:<\/SPAN><\/P> NOAA, MEDS and IOS observational data<\/SPAN><\/P> Uncertainties:<\/SPAN><\/P> Uncertainties are introduced when quality controlled observational data are spatially interpolated to varying distances from the observation point. Climatological averages are calculated from these interpolated values.<\/SPAN><\/P> Learn more or download this dataset from the Government of Canada's Open data portal.<\/SPAN><\/SPAN><\/A><\/P> Description:<\/SPAN><\/P> Données climatologiques saisonnières sur sigma-t de l\u2019océan Pacifique Nord-Est ont été calculées à partir d\u2019observations historiques comprenant toutes les données disponibles de conductivité-température-profondeur (CTD), de bouteilles, de bathythermographes non réutilisables (XBT), du programme Argo de la NOAA (http://www.argo.ucsd.edu/), du Marine Environmental Data Service (MEDS), ainsi que des archives de l\u2019Institut des sciences de la mer sur la période 1980-2010.<\/SPAN><\/P> Méthodes :<\/SPAN><\/P> Les calculs, y compris le lissage et l\u2019interpolation des données, ont été effectués dans soixante-cinq sous-régions et jusqu\u2019à cinquante-deux niveaux verticaux de la surface à 5 000 m. Les moyennes saisonnières ont été calculées comme la médiane des valeurs saisonnières annuelles. Les mois de printemps étaient définis comme allant d\u2019avril à juin, ceux d\u2019été comme allant de juillet à septembre, ceux d\u2019automne comme allant d\u2019octobre à décembre et ceux d\u2019hiver comme allant de janvier à mars. Les données disponibles ici contiennent des couches matricielles de données climatologiques saisonnières sur sigma-t pour la zone économique exclusive (ZEE) canadienne de l\u2019océan Pacifique, un sous-ensemble des données climatologiques saisonnières de l\u2019océan Pacifique Nord-Est, en haute résolution spatiale de 1/300 degré.<\/SPAN><\/P> Références:<\/SPAN><\/P> Foreman, M. G. G., W. R. Crawford, J. Y. Cherniawsky, and J. Galbraith (2008). Dynamic ocean topography for the northeast Pacific and its continental margins, Geophys. Res. Lett., 35, L22606, doi: 10.1029/2008GL035152<\/SPAN><\/P> Sources de données :<\/SPAN><\/P> Données d\u2019observation de la NOAA, du MEDS et de l\u2019iOS<\/SPAN><\/P> Incertitudes<\/SPAN><\/P> Des incertitudes sont engendrées lorsque les données d\u2019observation qui ont fait l\u2019objet d\u2019un contrôle de la qualité sont interpolées dans l\u2019espace à des distances variables du point d\u2019observation. Les moyennes climatologiques sont calculées à partir de ces valeurs interpolées.<\/SPAN><\/P> Apprenez-en plus ou téléchargez cet ensemble de données à partir du portail de données ouvertes du gouvernement du Canada.<\/SPAN><\/SPAN><\/A><\/P><\/DIV><\/DIV><\/DIV>",
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"Title": "Seasonal sigma-t climatology of the Canadian Pacific Exclusive Economic Zone (1980-2010) / Données climatologiques saisonnières sur sigma-t de la zone économique exclusive canadienne de l\u2019océan Pacifique (1980-2010)",
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"Comments": " Description:<\/SPAN><\/P> Seasonal sigma-t climatology of the Northeast Pacific Ocean was computed from historical observations including all available conductivity-temperature-depth (CTD), bottle, expendable bathy-thermograph (XBT), and Argo data in NOAA (http://www.argo.ucsd.edu/), Marine Environmental Data Service (MEDS), and Institute of Ocean Sciences archives over 1980 to 2010 period.<\/SPAN><\/P> Methods:<\/SPAN><\/P> Calculations, including smooth and interpolation, were carried out in sixty-five subregions and up to fifty-two vertical levels from surface to 5000m. Seasonal averages were computed as the median of yearly seasonal values. Spring months were defined as April to June, summer months were defined as July to September, fall months were defined as October to December, and winter months were defined as January to March. The data available here contain raster layers of seasonal sigma-t climatology for the Canadian Pacific Exclusive Economic Zone (EEZ), a subset of seasonal climatology of the Northeast Pacific Ocean, in high spatial resolution of 1/300 degree.<\/SPAN><\/P> References:<\/SPAN><\/P> Foreman, M. G. G., W. R. Crawford, J. Y. Cherniawsky, and J. Galbraith (2008). Dynamic ocean topography for the northeast Pacific and its continental margins, Geophys. Res. Lett., 35, L22606, doi: 10.1029/2008GL035152<\/SPAN><\/P> Data Sources:<\/SPAN><\/P> NOAA, MEDS and IOS observational data<\/SPAN><\/P> Uncertainties:<\/SPAN><\/P>