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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/3397.rdf" xlink:actuate="onRequest">Determining the effect of Eastern Maine bottom currents on lobster gear groundlines from F/V Time-n-Tide NEC-LL2006-1 in the Gulf of Maine, off Jonesport, Maine from 2007-2007 (NEC_ProjDev project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Ludwig, L. (2011) Determining the effect of Eastern Maine bottom currents on lobster gear groundlines from F/V Time-n-Tide NEC-LL2006-1 in the Gulf of Maine, off Jonesport, Maine from 2007-2007 (NEC_ProjDev project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2011-01-20 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/3397 [access date]</gco:CharacterString>
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        <gco:CharacterString>Determining the effect of Eastern Maine bottom currents on lobster gear groundlines Dataset Description: &amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;quot;Determining the Effect of Eastern Maine Bottom Currents on Groundlines&amp;quot;&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;This project sought to examine the effect of bottom currents on lobster gear in nearshore eastern Maine waters, to establish whether bottom currents there are strong enough to significantly reduce the profile of floating rope used as groundline between traps, thus reducing the risk of whale entanglements in lobster gear.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Assessment of the current meter data indicates that the current off Jonesport, Maine, where all the equipment was deployed, measured at the bottom of the ocean on level with the traps (1-2m off bottom), is often over 30 cm/sec and has little to no 'slack' period between tides. Analysis of the sensor data showed the floating groundlines at or below 2m (one fathom) of arc height over a 20 fathom length, and overall the measurements suggest that the flow of current is significantly stronger near the ocean bottom than anticipated, which would tend to depress the floating line more than would be estimated assuming much lower flows.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;See &amp;lt;a href=&amp;quot;http://nec.whoi.edu/pdf/Ludwig2006_groundlines_final.pdf&amp;quot; target=&amp;quot;blank&amp;quot;&amp;gt;final report&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Associated dataset: &amp;lt;a href=&amp;quot;https://www.bco-dmo.org/dataset/3414&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Groundline rope height (m) above seafloor between lobster traps &amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Datasets from three measuring devices were collected during five months of field-work. Depth and groundline height data was extrapolated from Star-Oddi pressure sensors deployed on a 20-trap trawl each month; current velocity and directional data was recorded by a Sensor Data 6000 current meter deployed near the lobster trawl; and three months' worth of data from acoustic Doppler current profilers (ADCP), rigged in a customized 3' lobster trap directly into the trawl, gave more detailed information about the velocity and direction of current acting on the groundline.&amp;lt;/p&amp;gt;</gco:CharacterString>
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           xlink:actuate="onRequest">F/V Time-n-Tide</gmx:Anchor>
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                      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/deployment/58163.rdf" xlink:title="Cruise" xlink:actuate="onRequest">NEC-LL2006-1</gmx:Anchor>
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                      <gmd:individualName>
                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/51282.rdf" xlink:actuate="onRequest">Ms Laura Ludwig</gmx:Anchor>
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                        <gmd:organisationName>
                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/225.rdf" xlink:title="Affiliation" xlink:actuate="onRequest">Gulf of Maine Lobster Foundation</gmx:Anchor>
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