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            <gco:CharacterString>Cite this dataset as: DeGrandpre, M. (2016) SAMI-CO2, SAMI-pH, temperature and dissolved oxygen from multiple moorings near Media Luna Reef, Puerto Rico from 2007-2008 (DOGEE-II project, NH10_ShelfBreak_MLR project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 12 January 2012) Version Date 2016-01-12 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/632551 [access date]</gco:CharacterString>
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        <gco:CharacterString>SAMI-CO2, SAMI-pH, temperature and dissolved O2 data from Media Luna Reef, Puerto Rico Dataset Description: &amp;lt;p&amp;gt;SAMI-CO2, SAMI-pH, temperature and dissolved O2 data from Media Luna Reef, Puerto Rico&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Media Luna Reef, NOAA CREWS buoy&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Locations:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Reef Head: 17.9381N, 67.0403W, depth of 4m&amp;lt;br /&amp;gt;
Reef Tail (#2):17.9386N, 67.0519W, depth of 5m&amp;lt;br /&amp;gt;
Reef Tail (#3): 17.9353N, 67.0483W, depth of 4m&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;The SAMIs sampled on a 30 minute interval. The SAMI-CO2 ran a non-absorbing blank measurement every 3.5 days. Oxygen was measured with a calibrated Aanderaa 4175 optode attached to a SAMI.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Related files and references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Gray, S. E. C.&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;M. D. DeGrandpre&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;C. Langdon&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;and&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt; &amp;lt;/em&amp;gt;J. E. Corredor&amp;lt;em&amp;gt; (&amp;lt;/em&amp;gt;2012&amp;lt;em&amp;gt;), &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;Short-term and seasonal pH, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;&amp;lt;em&amp;gt;p&amp;lt;/em&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;CO&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;&amp;lt;em&amp;gt;2 &amp;lt;/em&amp;gt;&amp;lt;/sub&amp;gt;&amp;lt;em&amp;gt;and saturation state variability in a coral-reef ecosystem&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;Global Biogeochem. Cycles&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;26&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, GB3012.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/630383.rdf" xlink:title="OCE-0628569" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0628569 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0628569</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/630384.rdf" xlink:title="OCE-0623294" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0623294 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0623294</gmx:Anchor>
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UK SOLAS Final Report (.pdf)
International SOLAS Web site</gco:CharacterString>
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                  <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/project/630393.rdf" xlink:title="Project" xlink:actuate="onRequest">Collaborative Research: Near-Surface controls of Air-Sea CO2 Exchange: A Contribution to the UK-SOLAS &amp;quot;Deep Ocean Gas Exchange Experiment&amp;quot;</gmx:Anchor>
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                            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/project/630393.rdf" xlink:title="Project Name" xlink:actuate="onRequest">Collaborative Research: Near-Surface controls of Air-Sea CO2 Exchange: A Contribution to the UK-SOLAS &amp;quot;Deep Ocean Gas Exchange Experiment&amp;quot;</gmx:Anchor>
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                            <gco:CharacterString>&lt;p&gt;The problem of quantifying the rate of gas flux across the air-water interface is one of the central questions of oceanography and is critical in the context of greenhouse gases and ocean-atmosphere budgets. The large uncertainty surrounding the flux of carbon dioxide (CO2) between the atmosphere and ocean prevent us from determining the partitioning of the sink of anthropogenic CO2 between the ocean and the terrestrial biosphere. This uncertainty also limits the ability to realistically model future atmospheric CO2 levels. The International SOLAS (Surface Ocean - Lower Atmosphere Study) science plan and implementation strategy highlights the need for an improved understanding of gas exchange. One of the stated goal of the SOLAS program to develop quantitative understanding of processes responsible for air-sea exchange of mass, momentum and energy to permit accurate calculation of regional and global gas and aerosol fluxes. This requires establishing the dependence of these interfacial transfer mechanisms on physical, biological and chemical factors within the atmospheric and oceanic boundary layers.&lt;/p&gt;
&lt;p&gt;The investigator in this project will participate in the recently funded UK-SOLAS &quot;Deep Ocean Gas Exchange Experiment&quot;, DOGEE. As part of this field experiment, two deliberate dual tracer patches will be released in close proximity to each other in the North Atlantic. One will be &quot;labeled&quot; with a surfactant in order to mimic the role of surface organic slicks in modifying gas transfer. The funded UK ship-based efforts will be enhanced with high resolution Lagrangian measurements of the air-sea interface. Specifically two Air-Sea Interaction Spar (ASIS) buoys, one in each patch, will be deployed to measure direct fluxes along with controlling surface physical processes (wind speed, wind stress, stability, surface waves, upper ocean turbulence and mixing, and key parameters governing mixed layer CO2 dynamics). In addition, a newly developed Air-Sea Interaction Profiler will be deployed to provide thermal and shear measurements in the very near surface. With these measurements, gas transfer process related specifically to surfactant effects, and to high wind processes will be better understood.&lt;/p&gt;
&lt;p&gt;Broader impacts: The current lack of an adequate parameterization of air-sea gas transfer rates contributes directly to our inability to predict with certainty future concentrations of CO2 and other climate relevant compounds in the atmosphere. This project will improve the accuracy of the global ocean carbon dioxide flux estimates and increase our understanding of the causes of its variability. Another broader impact is that this proposal establishes an international collaboration between research institutes in the US (RSMAS/U. Montana/ODU) and the UK. The proposed measurements employ state-of-the-art instrumentation, which will enhance the DOGEE experiment. The opportunity to participate in this experiment, and access to the data for subsequent analysis will provide for a unique dataset with which to increase our understanding of the role of air-sea CO2 exchange in influencing climate. The project will involve students as undergraduate and post-graduate research assistants. The University of Miami is a Hispanic Serving Institution and thereby fosters the participation of under-represented groups in science and engineering. The data will be made available through several data bases via WWW. The project will contribute to the active outreach activities coordinated through the RSMAS Dean's Office.&lt;/p&gt;
&lt;p&gt;This project is a contribution to the international SOLAS program.&lt;br /&gt;
&lt;strong&gt;PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH&lt;/strong&gt;&lt;br /&gt;
&lt;em&gt;&lt;strong&gt;Note:&lt;/strong&gt;  When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher. Some full text articles may not yet be available without a charge during the embargo (administrative interval).&lt;/em&gt;&lt;/p&gt;
&lt;p&gt;Some links on this page may take you to non-federal websites. Their policies may differ from this site.&lt;/p&gt;
&lt;p&gt;Brooks, I.M. et al. (M.D. DeGrandpre 12th of 54 authors in alphabetical order). &quot;Physical exchanges at the air-sea interface: UK-SOLAS field measurements,&quot; &lt;em&gt;Bulletin of the American Meteoroligical Society&lt;/em&gt;, v.90, 2009, p. 629. doi:10.1175/2008BAMS2578.1&lt;/p&gt;
&lt;p&gt;Byrne, R.H., DeGrandpre, M.D., Short, R.T., Martz, T.R., Merlivat, L., McNeil, C., Sayles, F.L., Bell, R. and P. Fietzek. &quot;Sensors and systems for observation of marine CO2 system variables,&quot; &lt;em&gt;roceedings of OceanObsâ??09: Sustained Ocean Observations and Information for Society (Vol. 2)&lt;/em&gt;, v.2, 2010. doi:doi:10.5270/OceanObs09.cwp.13&lt;/p&gt;
&lt;p&gt;Turk, D. Malacic, V., DeGrandpre, M.D. and W. R. McGillis. &quot;Carbon dioxide variability and air-sea fluxes in the northern Adriatic Sea,&quot; &lt;em&gt;Journal of Geophysical Research&lt;/em&gt;, v.115, 2010. doi:doi:10.1029/2009JC006034&lt;/p&gt;
&lt;p&gt;Edson, JB; Degrandpre, MD; Frew, N; McGillis, WR. &quot;Investigations of Air-Sea Gas Exchange in the CoOP Coastal Air-Sea Chemical Exchange Project,&quot; &lt;em&gt;OCEANOGRAPHY&lt;/em&gt;, v.21, 2008, p. 34. View record at Web of Science&lt;/p&gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;The earth's carbon cycle has been dramatically altered by global human industrialization. The movement of carbon from ancient fossil deposits to the atmosphere and into marine and terrestrial biospheres has many consequences, few of which are currently fully understood or predictable. Much of the needed understanding of the carbon cycle may come from better observational methods that can characterize large spans of time or space. One group of observational methods, autonomous sensors, can provide high temporal resolution data within air, earth or water systems. In this research, PIs from the University of Montana, Oregon State University and University of Miami will develop and use autonomous sensors to advance our understanding of carbon cycling within the earth's biosphere. With prior support, they have developed sensors for the partial pressure of CO2 (pCO2), pH and total alkalinity that can be used to quantify the amount of dissolved inorganic carbon through thermodynamic relationships. The more recently developed, currently laboratory-based sensors (pH and alkalinity) will be further refined for subsequent deployment, along with the more mature pCO2 sensor, in two contrasting marine environments; the coastal ocean waters off the U.S. central west coast, and a shallow coral ecosystem in Puerto Rico. Field studies will begin with a short, in situ test off Oregon State University's pier in Newport, Oregon followed by deployment on the Oregon shelf to study the processes that control air-sea carbon dioxide fluxes during periods of coastal upwelling. Concurrently, the same sensors will be deployed in La Parguera Marine Reserve, Puerto Rico, a Coral Reef Early Warning System (CREWS) site operated by NOAA to focus on the relationship of calcium carbonate saturation states to calcification rates in a coral reef ecosystem.&lt;/p&gt;
&lt;p&gt;The project will have a number of broad impacts including the technological development of rigorously tested sensors that will have a wide range of applications in marine and freshwater research. Students will be trained in the area of chemical sensor development who will subsequently become the next generation of leaders in this important research area. Outreach activities related to the grant will create awareness for contemporary carbon cycle issues such as greenhouse gas warming and ocean acidification.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH&lt;/strong&gt;&lt;br /&gt;
&lt;em&gt;&lt;strong&gt;Note:&lt;/strong&gt;  When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher. Some full text articles may not yet be available without a charge during the embargo (administrative interval).&lt;/em&gt;&lt;/p&gt;
&lt;p&gt;Some links on this page may take you to non-federal websites. Their policies may differ from this site.&lt;/p&gt;
&lt;p&gt;Edson, JB; Degrandpre, MD; Frew, N; McGillis, WR. &quot;Investigations of Air-Sea Gas Exchange in the CoOP Coastal Air-Sea Chemical Exchange Project,&quot; &lt;em&gt;OCEANOGRAPHY&lt;/em&gt;, v.21, 2008, p. 34. View record at Web of Science&lt;/p&gt;
&lt;p&gt;Hamme, R.C., Webley, P.W., Crawford, W.R., Whitney, F.A., DeGrandpre, M.D., Emerson, S.R., Eriksen, C.C., Giesbrecht, K.E., Gower, J.F.R., Kavanaugh, M.T., PeÃ±a, M.A., Sabine, C.L., Batten, S.D., Coogan, L.A., Grundle, D.S., and D. Lockwood. &quot;Volcanic ash fuels anomalous plankton bloom in subarctic Northeast Pacific,&quot; &lt;em&gt;Geophysical Research Letters&lt;/em&gt;, v.37, 2010, p. L19604. doi:10.1029/2010GL044629&lt;/p&gt;
&lt;p&gt;Byrne, R.H., DeGrandpre, M.D., Short, R.T., Martz, T.R., Merlivat, L., McNeil, C., Sayles, F.L., Bell, R. and P. Fietzek. &quot;Sensors and systems for observation of marine CO2 system variables,&quot; &lt;em&gt;Proceedings for Ocean Obs â??09&lt;/em&gt;, 2010.&lt;br /&gt;
 &lt;/p&gt;
&lt;p&gt; &lt;/p&gt;
&lt;p&gt;&lt;strong&gt;BOOKS/ONE TIME PROCEEDING&lt;/strong&gt;&lt;br /&gt;
Cullison, S.E.. &quot;MARINE APPLICATIONS OF AN&lt;br /&gt;
AUTONOMOUS INDICATOR-BASED pH&lt;br /&gt;
SENSOR&quot;, 10/01/2009-09/30/2010,  2010, &quot;The University of Montana&quot;.&lt;/p&gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Related files and references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Gray, S. E. C.&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;M. D. DeGrandpre&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;C. Langdon&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;and&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt; &amp;lt;/em&amp;gt;J. E. Corredor&amp;lt;em&amp;gt; (&amp;lt;/em&amp;gt;2012&amp;lt;em&amp;gt;), &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;Short-term and seasonal pH, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;&amp;lt;em&amp;gt;p&amp;lt;/em&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;CO&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;&amp;lt;em&amp;gt;2 &amp;lt;/em&amp;gt;&amp;lt;/sub&amp;gt;&amp;lt;em&amp;gt;and saturation state variability in a coral-reef ecosystem&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;Global Biogeochem. Cycles&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, &amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;26&amp;lt;/em&amp;gt;&amp;lt;em&amp;gt;, GB3012.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO Processing Notes&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
- Generated from the following list of original .xlsx files contributed by Cory Beatty&amp;lt;br /&amp;gt;
Media Luna Reef_Fall_SAMI-CO2 &amp;amp;amp; pH &amp;amp;amp; O2.xlsx&amp;lt;br /&amp;gt;
Media Luna Reef_Summer_SAMI-CO2 &amp;amp;amp; pH.xlsx&amp;lt;br /&amp;gt;
Media Luna Reef_Winter_SAMI-CO2 &amp;amp;amp; pH &amp;amp;amp; O2.xlsx&amp;lt;br /&amp;gt;
- Parameter names edited to conform to BCO-DMO naming convention found at &amp;lt;a href=&amp;quot;http://usjgofs.whoi.edu/naming-guidelines.html&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Choosing Parameter Name&amp;lt;/a&amp;gt;&amp;lt;br /&amp;gt;
- Params added to some datasets for compatibility&amp;lt;br /&amp;gt;
- If not reported, aded params assigned &amp;quot;NaN&amp;quot; values&amp;lt;br /&amp;gt;
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