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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/3118.rdf" xlink:actuate="onRequest">Air temperature and barometric pressure from autonomous buoys from ARSV Laurence M. Gould LMG0106 in the Southern Ocean, Aug-Nov, 2001 (SOGLOBEC project, Sea Ice Microbes project)</gmx:Anchor>
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        <gco:CharacterString>Air temp and barometric press results from autonomous buoys, Aug-Nov, 2001 Dataset Description: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Related datasets:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://globec.whoi.edu/jg/serv/globec/soglobec/buoy_position.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/buoy_position%7D&amp;quot;&amp;gt;buoy_position&amp;lt;/a&amp;gt; Autonomous buoy position data, Aug. - Nov. 2001&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://globec.whoi.edu/jg/serv/globec/soglobec/buoy_therm.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/buoy_therm%7D&amp;quot;&amp;gt;buoy_therm&amp;lt;/a&amp;gt;&amp;lt;strong&amp;gt; &amp;lt;/strong&amp;gt; Thermistor data at 10 cm intervals in air, ice, water from autonomous buoys, Aug. - Nov. 2001&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://globec.whoi.edu/jg/serv/globec/soglobec/buoy_radm.html0%7Bdir=globec.whoi.edu/jg/dir/globec/soglobec/,info=globec.whoi.edu/jg/info/globec/soglobec/buoy_radm%7D&amp;quot;&amp;gt;buoy_radm&amp;lt;/a&amp;gt;&amp;lt;strong&amp;gt; &amp;lt;/strong&amp;gt; Radiometer data from autonomous buoy 07949, Aug. - Nov. 2001&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;During the July-September 2001 Southern Globec cruises of the Palmer and Gould we installed four buoys. Two of the buoys (07413, 07440) were standard off-the-shelf Met-Ocean Ice buoys (see above photograph). These buoys measured barometric pressure, air temperature, and GPS position. The data were transmitted via ARGOS. A radar reflector was mounted on a wooden 4 x 4 to help find the site if there was an opportunity to return, however the reflector return was difficult to discern among all the backscatter clutter caused by deformed ice and icebergs.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The other two buoys (07949, 07950) were custom made CRREL ice mass balance buoys (photo on right). These buoys reported barometric pressure, Argos position, and air temperature. In addition they had a thermistor string that measured a vertical profile of temperature, at 10 cm spacing, from the air, through the snow and ice, and into the upper ocean. There were acoustic sensors measuring the positions of the snow surface and ice bottom. A fluorometer was mounted under the ice. One of the buoys (07949) had three spectroradiometers; one mounted about the ice, one mounted directly below the ice, and one a few meters deep in the upper ocean. Results from all buoys are compared.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Tracks from all 2001 buoys:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;img alt=&amp;quot;buoy tracks&amp;quot; src=&amp;quot;https://datadocs.bco-dmo.org/static/globec.whoi.edu/images/so/fritsen_buoy_drftall.gif&amp;quot; style=&amp;quot;height:606px; width:593px&amp;quot; /&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54688.rdf" xlink:title="ANT-9910098" xlink:actuate="onRequest">Funding provided by NSF Antarctic Sciences (NSF ANT) Award Number: ANT-9910098 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9910098</gmx:Anchor>
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                <gco:CharacterString>&amp;lt;p&amp;gt;During the July-September 2001 Southern Globec cruises of the Palmer and Gould we installed four buoys. Two of the buoys (07413, 07440) were standard off-the-shelf Met-Ocean Ice buoys (see above photograph). These buoys measured barometric pressure, air temperature, and GPS position. The data were transmitted via ARGOS. A radar reflector was mounted on a wooden 4 x 4 to help find the site if there was an opportunity to return, however the reflector return was difficult to discern among all the backscatter clutter caused by deformed ice and icebergs.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The other two buoys (07949, 07950) were custom made CRREL ice mass balance buoys (photo on right). These buoys reported barometric pressure, Argos position, and air temperature. In addition they had a thermistor string that measured a vertical profile of temperature, at 10 cm spacing, from the air, through the snow and ice, and into the upper ocean. There were acoustic sensors measuring the positions of the snow surface and ice bottom. A fluorometer was mounted under the ice. One of the buoys (07949) had three spectroradiometers; one mounted about the ice, one mounted directly below the ice, and one a few meters deep in the upper ocean. Results from all buoys are compared.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Tracks from all 2001 buoys:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;img alt=&amp;quot;buoy tracks&amp;quot; src=&amp;quot;https://datadocs.bco-dmo.org/static/globec.whoi.edu/images/so/fritsen_buoy_drftall.gif&amp;quot; style=&amp;quot;height:606px; width:593px&amp;quot; /&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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The surface float contains sensors that measure different parameters, such as sea surface temperature, barometric pressure, salinity, wave height, etc. Data collected from these sensors are transmitted to satellites passing overhead, which are then relayed to land-based data centers.

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    <gmi:citation>
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          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54020.rdf"
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/50488.rdf" xlink:actuate="onRequest">Daniel P. Costa</gmx:Anchor>
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/260.rdf" xlink:title="Affiliation" xlink:actuate="onRequest">University of California-San Diego</gmx:Anchor>
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