<p>Observations were made at intervals ranging from 0.93 to 1.32 hr over a 12.22-hr period. They extended from 0.43 hr before (−) high tide (Hi) to 0.50 hr before (−) high tide and encompassed both flood (F) and ebb (E) stages. Rates of temperature change (<sup>o</sup>C hr<sup>−1</sup>) were calculated using differences in seabed temperature (ΔT) and the time elapsed from the previous observation. Rates were highest at or just after mid-ebb tide (CTD sta 059, −2.48<sup>o</sup>C hr<sup>−1</sup>; CTD sta 060, −1.83<sup>o</sup>C hr<sup>−1</sup>) and just before mid-flood tide (CTD sta 070, 1.14<sup>o</sup>C hr<sup>−1</sup>). Maximum flood and ebb rates of temperature change used for Area A in <a href="http://www.plosone.org/article/info:doi/10...
Seasonal, tidal, and spring-vs.-neap changes in water content, atmospheric exposure, and temperature...
Sea level rise (SLR) is causing acceleration in the frequency and duration of minor tidal flooding (...
<p>Data was obtained from the northern margin of Georges Bank in August 2009. Subareas 1–7 of are sh...
<p>Data at sites were collected during tidal cycles, including at both high and low tide, over perio...
<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>Values in each subarea are changes in seabed temperature (°C) during tidal front movement off ban...
<p>Temperature change from high to low tide is shown for the parts of transects where seabed tempera...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Alternating inundation and exposure of large tidal flats regions suggest that differences in thermod...
<p>Examples of rapid temperature changes within the tidal front in off-bank subareas. A. Single rapi...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Temperature changes in sediment and the inundating water of a subtropical mudflat were determined us...
<p>Record of seawater temperature measured every 10 min in the upwelling (Houbibu, HBH) and control ...
The initial flooding waters from twenty-four consecutive tides were examined for changes in water pr...
Seasonal, tidal, and spring-vs.-neap changes in water content, atmospheric exposure, and temperature...
Sea level rise (SLR) is causing acceleration in the frequency and duration of minor tidal flooding (...
<p>Data was obtained from the northern margin of Georges Bank in August 2009. Subareas 1–7 of are sh...
<p>Data at sites were collected during tidal cycles, including at both high and low tide, over perio...
<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>Values in each subarea are changes in seabed temperature (°C) during tidal front movement off ban...
<p>Temperature change from high to low tide is shown for the parts of transects where seabed tempera...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Alternating inundation and exposure of large tidal flats regions suggest that differences in thermod...
<p>Examples of rapid temperature changes within the tidal front in off-bank subareas. A. Single rapi...
Georges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previ...
Temperature changes in sediment and the inundating water of a subtropical mudflat were determined us...
<p>Record of seawater temperature measured every 10 min in the upwelling (Houbibu, HBH) and control ...
The initial flooding waters from twenty-four consecutive tides were examined for changes in water pr...
Seasonal, tidal, and spring-vs.-neap changes in water content, atmospheric exposure, and temperature...
Sea level rise (SLR) is causing acceleration in the frequency and duration of minor tidal flooding (...
<p>Data was obtained from the northern margin of Georges Bank in August 2009. Subareas 1–7 of are sh...