During the 1617 season, new equations were determined for ELB and WLB to account for lake level rise. These equations were better able to correct the CTD measured depths at the deeper depths of these lakes. The equations are as follows:
ELB: y = -0.0028x2 + 1.0437x + 0.5828WLB: y = -0.0017x2 + 1.0179x + 0.6418
Note that the depth calculated from the CTD pressure sensor can vary by up to 0.6 m depending on atmospheric pressure at the time of the cast.
Note that no corrections have been determined for other lakes profiled.
For more details on wire corrected data, see Spigel and Priscu 1996.