Observations of Autumnal Cooling in a Large Estuary: The Glider Data from Long Island Sound in 2014

<p>This data file is a component of the data used in a paper to appear in the Journal of Geophysical Research in 2023 entitled &quot;Observations of Autumnal Cooling in a Large Estuary&quot; by Amin Ilia, Grant McCardell, Kay Howard-Strobel, and James O&#39;Donnell.&nbsp; The data file contains the measurements from a Slocum Glider (V1) from Webb Research used in the paper. The data is in&nbsp;a MATLAB binary (.mat) file as a structure variable with a field&nbsp;MetaData containing&nbsp;some notes, and data in&nbsp;<br> &nbsp; &nbsp; SampleTimeEST- the date and time of the sample (EST) in MATLAB&#39;s datenum() format<br> &nbsp; &nbsp; Pressure_dBar - the pressure (or&nbsp;equivalently depth in m) that the sample was acquired&nbsp;<br> &nbsp; &nbsp; Temperature_C - the water temperature in Celcius<br> &nbsp; &nbsp; PracticalSalinty - the practical salinity<br> &nbsp; &nbsp; LatitudeDeg- the latitude of the sampling location (deg)<br> &nbsp; &nbsp; LongitudeDeg - the longitude of the sampling location (deg east)</p> <p>The paper&#39;s abstract is:&nbsp;</p> <p>Seasonal variations in solar insolation and wind create an annual water temperature cycle that impacts circulation and biological processes. The waters of Long Island Sound (LIS) warm from March-February until August-October and then begin to cool. Ship surveys show that the vertical temperature structure becomes almost uniform during this season when the area experiences low air temperatures and high winds. However, no observations have resolved the temporal evolution of the vertical structure of temperature during these cooling periods because conditions inhibit ship operations. We report glider measurements of the vertical structure of water temperatures and salinities from October 22 to November 4, 2014, in eastern LIS. We find that 20m of water can cool at approximately 0.5 C/day during intervals of cold air and strong winds. We use the data to estimate heat content tendencies and infer surface fluxes. We also estimate the surface heat fluxes using buoy-mounted instruments and show they are consistent. The net heat flux to the atmosphere exceeds 600 W/m²&nbsp;during the gilder deployment and approximately 66% of this is due to latent heat transfer. Using the buoy fluxes and products of an operation regional model, we show that the agreement with the fluxes derived from heat budget is improved by using local wind observations. In addition to confirming the extremely large cooling rates, our results demonstrate that gliders can be used in a complex region with strong tidal currents to resolve the temperature structure and heat budget during the severe weather of the cooling season.</p> <p>&nbsp;</p>