Wind influence on surface current variability in the Ibiza Channel from HF Radar
Autor: | Arancha Lana, Julien Marmain, Joaquín Tintoré, Alejandro Orfila, Vicente Fernandez |
---|---|
Přispěvatelé: | European Commission, Consejo Superior de Investigaciones Científicas (España) |
Rok vydání: | 2016 |
Předmět: |
0106 biological sciences
Water mass Mass transport 010504 meteorology & atmospheric sciences Mesoscale meteorology HF Radar Oceanography 01 natural sciences law.invention Ibiza Channel Mediterranean sea law 14. Life underwater Radar 0105 earth and related environmental sciences Surface currents 010604 marine biology & hydrobiology Ocean current Mode (statistics) Wind-current variability Current (stream) Drifter 13. Climate action Climatology Geology |
Zdroj: | Ocean Dynamics Digital.CSIC. Repositorio Institucional del CSIC instname |
ISSN: | 1616-7228 |
Popis: | Surface current variability is investigated using 2.5 years of continuous velocity measurements from an high frequency radar (HFR) located in the Ibiza Channel (Western Mediterranean Sea). The Ibiza Channel is identified as a key geographical feature for the exchange of water masses but still poorly documented. Operational, quality controlled, HFR derived velocities are provided by the Balearic Islands Coastal Observing and Forecasting System (SOCIB). They are assessed by performing statistical comparisons with current-meter, ADCP, and surface lagrangian drifters. HFR system does not show significant bias, and its accuracy is in accordance with previous studies performed in other areas. The main surface circulation patterns are deduced from an EOF analysis. The first three modes represent almost 70 % of the total variability. A cross-correlation analysis between zonal and meridional wind components and the temporal amplitudes of the first three modes reveal that the first two modes are mainly driven by local winds, with immediate effects of wind forcing and veering following Ekman effect. The first mode (37 % of total variability) is the response of meridional wind while the second mode (24 % of total variability) is linked primarily with zonal winds. The third and higher order modes are related to mesoscale circulation features. HFR derived surface transport presents a markedly seasonal variability being mostly southwards. Its comparison with Ekman-induced transport shows that wind contribution to the total surface transport is on average around 65 %. A. Lana thanks the financial support from the CSIC-JAE doc program co-funded by the European Social Fund (ESF). J. Marmain is supported by Sur-Baleares Project. A. Orfila thanks the support from ENAP-Colombian Army through several grants. This work has been done thanks to the financial support from JERICO-NEXT project. |
Databáze: | OpenAIRE |
Externí odkaz: |