<p>Temperature change from high to low tide is shown for the parts of transects where seabed temperature is influenced (Y) or not influenced (N) by frontal movement. Station pair groups (column 2) are numbered in each area from north to south (1–10; i.e. off-bank to on-bank). Each pair group contains up to 8 pairs of CTD stations, at which temperature was recorded at high or low tide. H Temp and L Temp are the ranges of seabed temperatures within the pair group measured at high and low tide, respectively. H-L ΔT is the range of temperature differences between high and low tides at stations within the pair group. This value is the criterion on which frontal influence is based. If the minimum value for H-L ΔT is >1.0°C, the pair group is cons...
Nearshore temperature fluctuations are associated with energetic cross-shore two-way flows that infl...
Alternating inundation and exposure of large tidal flats regions suggest that differences in thermod...
The mechanisms controlling the temperature and salinity structure of shallow continental shelf seas ...
<p>Seabed temperature change per kilometer is given for parts of transects where individual sites ar...
<p>Temperature data was collected at CTD stations located along transects, at time-series stations, ...
<p>Data at sites were collected during tidal cycles, including at both high and low tide, over perio...
This paper presents a mechanism to explain the observed formation of a surface temperature minimum ...
<p>Values in each subarea are changes in seabed temperature (°C) during tidal front movement off ban...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
<p>Observations were made at intervals ranging from 0.93 to 1.32 hr over a 12.22-hr period. They ext...
International audienceThe Ushant tidal front is the dominant feature of the summer season hydrologic...
<p>Examples of rapid temperature changes within the tidal front in off-bank subareas. A. Single rapi...
<p>Data was obtained from the northern margin of Georges Bank in August 2009. Subareas 1–7 of are sh...
The characteristics of a shear front system in a tidal channel have been investigated through a fiel...
Nearshore temperature fluctuations are associated with energetic cross-shore two-way flows that infl...
Alternating inundation and exposure of large tidal flats regions suggest that differences in thermod...
The mechanisms controlling the temperature and salinity structure of shallow continental shelf seas ...
<p>Seabed temperature change per kilometer is given for parts of transects where individual sites ar...
<p>Temperature data was collected at CTD stations located along transects, at time-series stations, ...
<p>Data at sites were collected during tidal cycles, including at both high and low tide, over perio...
This paper presents a mechanism to explain the observed formation of a surface temperature minimum ...
<p>Values in each subarea are changes in seabed temperature (°C) during tidal front movement off ban...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
<p>Observations were made at intervals ranging from 0.93 to 1.32 hr over a 12.22-hr period. They ext...
International audienceThe Ushant tidal front is the dominant feature of the summer season hydrologic...
<p>Examples of rapid temperature changes within the tidal front in off-bank subareas. A. Single rapi...
<p>Data was obtained from the northern margin of Georges Bank in August 2009. Subareas 1–7 of are sh...
The characteristics of a shear front system in a tidal channel have been investigated through a fiel...
Nearshore temperature fluctuations are associated with energetic cross-shore two-way flows that infl...
Alternating inundation and exposure of large tidal flats regions suggest that differences in thermod...
The mechanisms controlling the temperature and salinity structure of shallow continental shelf seas ...