©2020 Biological and Chemical Oceanography Data Management Office.Count of number of dives observed in each dataset of four trials (T1-T4) of increasing turbulence (s0-s7), corresponding to tank forcing frequencies of 0-1.75 Hz. Dives are identified as per the method described in Wheeler et al. (2013). PIV recordings were performed by J. Wheeler in Summer 2011 and 2012.
Relevant Reference:
Wheeler J.D., Helfrich K.R., Anderson E.J., McGann B., Staats P., Wargula A.E., Wilt K., Mullineaux L.S. (2013) Upward swimming of competent oyster larvae Crassostrea virginica persists in highly turbulent flow as detected by PIV flow subtraction. Mar Ecol Prog Ser 488, 171-185.
Wheeler J.D., Helfrich K.R., Anderson E.J., Mullineaux L.S. (2015) Isolating the hydrodynamic triggers of the dive response in eastern oyster larvae. Limnol Oceanogr, (doi:10.1002/lno.10098)
Mullineaux, L., Helfrich, K. R. (2015) Data on number of dives observed and total number of larval tracks across all turbulence regimes collected at Wood Hole Oceanographic Institution in 2011 (Larvae in turbulence project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2015-06-08) Version Date 2015-06-08 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/561205 [access date]
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