TY - JOUR
AU - W. Austin
AU - A. Cage
AU - J. Scourse
AB - Pronounced seasonal variability, particularly in the surface ocean heat flux, imparts an important control that drives thermal stratification of the tide-dominated middle-and high-latitude shelf seas. Bottom water temperature and salinity data, resolved on a grid 20\textquoteright latitude by 30\textquoteright longitude, were combined with a regional synthesis of the salinity: δ18O relationship in order to generate a spatial and temporal understanding of oxygen isotopes in seawater around the shelf seas of NW Europe. The data are expressed according to equilibrium calcite (δ18OEq.calcite) and, in the shallow mixed water column, exhibit large seasonal changes that are primarily driven by bottom water temperature. Annual bottom water temperature varies from  3\textdegreeC to 17\textdegreeC in the southern North Sea, generating a seasonal δ18OEq.calcite signal of up to 3.2\%. The amplitude of the seasonal d18OEq.calcite signal is significantly damped (0.1 - 0.2o/oo) in deeper, thermally stratified shelf waters. Maps of the monthly distribution δ18OEq.calcite provide the first systematic overview of the spatial and temporal changes on the NW European shelf and highlight the importance of understanding seasonal growth on the incorporation of geochemical signatures into marine organisms.
BT - The Holocene
DA - November 1, 2006
M1 - 7
N2 - Pronounced seasonal variability, particularly in the surface ocean heat flux, imparts an important control that drives thermal stratification of the tide-dominated middle-and high-latitude shelf seas. Bottom water temperature and salinity data, resolved on a grid 20\textquoteright latitude by 30\textquoteright longitude, were combined with a regional synthesis of the salinity: δ18O relationship in order to generate a spatial and temporal understanding of oxygen isotopes in seawater around the shelf seas of NW Europe. The data are expressed according to equilibrium calcite (δ18OEq.calcite) and, in the shallow mixed water column, exhibit large seasonal changes that are primarily driven by bottom water temperature. Annual bottom water temperature varies from  3\textdegreeC to 17\textdegreeC in the southern North Sea, generating a seasonal δ18OEq.calcite signal of up to 3.2\%. The amplitude of the seasonal d18OEq.calcite signal is significantly damped (0.1 - 0.2o/oo) in deeper, thermally stratified shelf waters. Maps of the monthly distribution δ18OEq.calcite provide the first systematic overview of the spatial and temporal changes on the NW European shelf and highlight the importance of understanding seasonal growth on the incorporation of geochemical signatures into marine organisms.
PY - 2006
SP - 937
EP - 947
T2 - The Holocene
TI - Mid-latitude shelf seas: a NW European perspective on the seasonal dynamics of temperature, salinity and oxygen isotopes
UR - http://hol.sagepub.com/content/16/7/937.abstract
VL - 16
ER -