Publications des scientifiques de l'IRD

Vazquez-Cuervo J., Dewitte Boris, Chin T. M., Armstrong E. M., Purca S., Alburqueque E. (2013). An analysis of SST gradients off the Peruvian coast : the impact of going to higher resolution. Remote Sensing of Environment, 131, p. 76-84. ISSN 0034-4257.

Titre du document
An analysis of SST gradients off the Peruvian coast : the impact of going to higher resolution
Année de publication
2013
Type de document
Article référencé dans le Web of Science WOS:000315546900006
Auteurs
Vazquez-Cuervo J., Dewitte Boris, Chin T. M., Armstrong E. M., Purca S., Alburqueque E.
Source
Remote Sensing of Environment, 2013, 131, p. 76-84 ISSN 0034-4257
The Peruvian Coastal Upwelling System (PCUS) is one of the most productive fisheries in the world. Upwelling events are associated with changes in the magnitude and location of frontal structures. SST gradients from four different data sets, NCDC, REMSS, OSTIA, and MUR are compared in two test areas off the PCUS: Paita (5 degrees S) and Pisco (14 degrees S). In both areas gradients derived from the MUR data set show greater magnitudes, as well as larger seasonal cycles. Off Pisco, the magnitude of the seasonal cycle of 2.2 degrees C/100 km in MUR is larger than the one derived from the lower resolution data sets. All data sets at Pisco exhibit a seasonal cycle that peaks in late Austral summer and early fall. Hovmoller diagrams calculated at 5.5 degrees S, 10.5 degrees S, and 14.5 degrees S show clearly defined offshore maxima in the cross-shore gradients for all the data sets. Upwelling scales determined by the distance to the first maxima vary depending on the data set used. At 5.5 degrees S upwelling scales vary from 10 km for MUR to 50 km for NCDC At 14.5 degrees S the scales vary from 20 km for MUR to 40 km for OSTIA. All four data sets show similar large-scale structures associated with the Peruvian upwelling. However, MUR shows finer scale structures that are most likely due to submesoscale to mesoscale eddies. Sub-sampled MUR 1 km data at the 25 km, 9 km, and 4 km resolutions compare well in magnitude and phase with the lower resolution products. Agreement in gradient magnitude between the lower resolution data sets and the MUR sub-sampled at their respective resolutions implies that the pixel-to-pixel analysis noise in MUR is at a similar level as the other data sets.
Plan de classement
Limnologie physique / Océanographie physique [032] ; Télédétection [126]
Description Géographique
PEROU
Localisation
Fonds IRD [F B010060716]
Identifiant IRD
fdi:010060716
Contact