Probabilistic relationships between wind and surface water circulation patterns in the SE Bay of Biscay
HF RADAR DATA
CURRENTS
DYNAMICS
0106 biological sciences
SLOPE
High-frequency radar
Wind-induced circulation
SOUTHERN BAY
OIL-SPILL
01 natural sciences
VARIABILITY
13. Climate action
Shelf slope circulation
Ocean surface currents
SOUTHEASTERN BAY
RECONSTRUCTION
14. Life underwater
Iberian Poleward Current
TEMPERATURE
Clustering technique
DOI:
10.1007/s10236-015-0871-5
Publication Date:
2015-09-11T08:41:54Z
AUTHORS (8)
ABSTRACT
Non-linear K-means classification algorithm was used to obtain a comprehensive description of the winds and high-frequency radar-derived currents in the SE Bay of Biscay (study area), taking into account a wide range of scales, from several days to interannual variability. The results in the study area show that in summer, a stronger variability in winds and surface currents can be expected, while in winter, intense southwesterly winds and a cyclonic circulation prevail. In addition to the seasonal component of the currents, a significant spatial variability in terms of current patterns and a temporal variability at shorter and interannual scales were also identified, highlighting the complexity of the surface current dynamics. Moreover, the probabilistic relationships between wind and current patterns were explored, obtaining conditional probabilities. Most of the surface current patterns are clearly related to specific wind patterns that are recurrent in the study area. However, other common current patterns are not so clearly related to specific wind conditions. The presence of a seasonal slope current (Iberian Poleward Current, IPC) is one of the most relevant features of the local circulation. An IPC occurrence time series based on Sea Surface Temperature satellite imagery was used to obtain conditional probabilities with the high-frequency radar surface current patterns, showing a relation between the strongest IPC events and closed cyclonic currents, which are not linked to specific winds.
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