Open AccessSpatial and temporal variability of the sea surface temperature in the Ballenas‐Salsipuedes Channel (central Gulf of California)
Author(s) -
MartínezDíazdeLeón A.,
PachecoRuíz I.,
DelgadilloHinojosa F.,
ZertucheGonzález J. A.,
CheeBarragán A.,
BlancoBetancourt R.,
GuzmánCalderón J. M.,
GálvezTelles A.
Publication year - 2006
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jc002940
Subject(s) - outcrop , oceanography , sea surface temperature , anomaly (physics) , channel (broadcasting) , geology , period (music) , climatology , spatial variability , common spatial pattern , environmental science , convective mixing , annual cycle , convection , geography , meteorology , geomorphology , physics , statistics , mathematics , engineering , condensed matter physics , acoustics , electrical engineering
The Ballenas‐Salsipuedes Channel (BSC) is considered an oceanographic province on its own within the Gulf of California. In this region, tidal mixing is modulated by quarterdiurnal, semidiurnal, diurnal, and fortnightly frequencies, producing a strong outcropping of cold and nutrient‐rich waters. In this work we analyze the temporal and spatial variability of sea surface temperature (SST) data recorded simultaneously over a period of 1 year in six bays along the BSC. Minimum mean SST differences (< 0.5°C) among bays were observed in December, while maximum differences (> 2.5°C) were recorded in June. The monthly SST anomaly showed that from late October to late January, the channel behaved as a very well mixed region. In contrast, SST anomalies of up to 2.2°C among bays were observed from May to September, indicating intense heat gain in summer and highlighting spatial heterogeneity in the intensity of vertical mixing. Besides the seasonal temperature cycle, influenced by solar irradiation, four main periods (0.25, 0.5, 1, and 15 days) were identified, corresponding to the main timescales of variability induced by the tides. This work demonstrates that the main source of temporal SST variability in BSC is the tide‐induced fortnightly modulation, suggesting the possibility of a pulsation mechanism in the outcropping of nutrient‐rich waters reaching the surface layer throughout the channel; this could play a crucial role in explaining the exceptionally high biological production of this region.