<eml:eml xmlns:eml="eml://ecoinformatics.org/eml-2.1.0" xmlns:stmml="http://www.xml-cml.org/schema/stmml-1.1" xmlns:ds="eml://ecoinformatics.org/dataset-2.1.0" xmlns:xs="http://www.w3.org/2001/XMLSchema" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="eml://ecoinformatics.org/eml-2.1.0 http://nis.lternet.edu/schemas/EML/eml-2.1.0/eml.xsd" packageId="knb-lter-mcm.2006.11" system="knb">
  <access scope="document" order="allowFirst" authSystem="knb">
    <allow>
      <principal>uid=MCM,o=EDI,dc=edirepository,dc=org</principal>
      <permission>all</permission>
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    <allow>
      <principal>public</principal>
      <permission>read</permission>
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  <dataset>
    <shortName>MSCHNG</shortName>
    <title>Snow, ice, and total glacier mass balance measurements, McMurdo Dry Valleys, Antarctica (1993-2023, ongoing)</title>
    <creator>
      <individualName>
        <givenName>Michael</givenName>
        <surName>Gooseff</surName>
      </individualName>
      <electronicMailAddress>michael.gooseff@colorado.edu</electronicMailAddress>
      <onlineUrl>http://goosefflab.weebly.com</onlineUrl>
      <userId directory="https://orcid.org">https://orcid.org/0000-0003-4322-8315</userId>
    </creator>
    <creator>
      <individualName>
        <givenName>Andrew</givenName>
        <surName>Fountain</surName>
      </individualName>
      <address>
        <deliveryPoint>P.O. Box 751</deliveryPoint>
        <city>Portland</city>
        <administrativeArea>OR</administrativeArea>
        <postalCode>97207</postalCode>
        <country>US</country>
      </address>
      <phone phonetype="voice">(503) 725-3386</phone>
      <electronicMailAddress>andrew@pdx.edu</electronicMailAddress>
      <onlineUrl>http://glaciers.pdx.edu/fountain/</onlineUrl>
      <userId directory="https://orcid.org">https://orcid.org/0000-0001-5299-2273</userId>
    </creator>
    <metadataProvider>
      <organizationName>McMurdo Dry Valleys LTER</organizationName>
      <onlineUrl>http://mcmlter.org/</onlineUrl>
    </metadataProvider>
    <associatedParty>
      <individualName>
        <givenName>Anna</givenName>
        <surName>Wright</surName>
      </individualName>
      <electronicMailAddress>anna.t.wright@colorado.edu</electronicMailAddress>
      <userId directory="https://orcid.org">https://orcid.org/0009-0003-4709-151X</userId>
      <role>field technician</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Renée</givenName>
        <surName>Brown</surName>
      </individualName>
      <electronicMailAddress>rfbrown@unm.edu</electronicMailAddress>
      <userId directory="https://orcid.org">https://orcid.org/0000-0002-4986-7663</userId>
      <role>data manager</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Anna</givenName>
        <surName>Bergstrom</surName>
      </individualName>
      <electronicMailAddress>annabergstrom@boisestate.edu</electronicMailAddress>
      <userId directory="https://orcid.org">https://orcid.org/0000-0002-9684-4018</userId>
      <role>former field crew</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Adam</givenName>
        <surName>Wlostowski</surName>
      </individualName>
      <electronicMailAddress>wlostowskiadam@gmail.com</electronicMailAddress>
      <role>former field crew</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Hassan</givenName>
        <surName>Basagic</surName>
      </individualName>
      <electronicMailAddress>basagic@gmail.com</electronicMailAddress>
      <role>former field crew</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Thomas</givenName>
        <surName>Nylen</surName>
      </individualName>
      <electronicMailAddress>thomasnylen@gmail.com</electronicMailAddress>
      <userId directory="https://orcid.org">https://orcid.org/0000-0001-9579-8702</userId>
      <role>former field crew</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Inigo</givenName>
        <surName>San Gil</surName>
      </individualName>
      <address>
        <deliveryPoint>Department of Biology, MSC03 2020 University of New Mexico</deliveryPoint>
        <city>Albuquerque</city>
        <administrativeArea>NM</administrativeArea>
        <postalCode>87131</postalCode>
        <country>US</country>
      </address>
      <phone phonetype="voice">(505) 277-2625</phone>
      <phone phonetype="facsimile">(505) 277-2541</phone>
      <electronicMailAddress>isangil@lternet.edu</electronicMailAddress>
      <role>former data manager</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Chris</givenName>
        <surName>Gardner</surName>
      </individualName>
      <electronicMailAddress>gardner.177@osu.edu</electronicMailAddress>
      <userId directory="https://orcid.org">https://orcid.org/0000-0003-0400-3754</userId>
      <role>former data manager</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Denise</givenName>
        <surName>Steigerwald</surName>
      </individualName>
      <role>former data manager</role>
    </associatedParty>
    <pubDate>2025-03-11</pubDate>
    <language>English</language>
    <abstract>
      <section>
        <para>
          <literalLayout>As part of the Long Term Ecological Research (LTER) project in the McMurdo Dry Valleys of Antarctica, a systematic sampling program has been undertaken to monitor glacial mass balance and meltwater flow. This data package includes mass balance changes at each stake on six glaciers (Canada, Commonwealth, Hughes, Suess, Howard, and Taylor) in Taylor Valley and one glacier (Adams) in Miers Valley, all of which are located in the McMurdo Dry Valleys region of Antarctica. The values are the result of an analysis of the raw data presented in other data files (glacier stake heights, snow depths, and glacier snow densities). Included here for each stake are the change in ice and snow water equivalent (mass) values, and the total mass change. The standard deviation or the range for each total is also given. Most measurements began during the 93-94 field season. Adams measurements were established during the 14-15 field season. Measurements are ongoing except at Hughes and Suess Glaciers where monitoring ceased following the 08-09 field season. Monitoring the changes in these measurements over time provides a record of mass balance, and aids in determining the role of glaciers in the polar hydrologic cycle.</literalLayout>
        </para>
      </section>
    </abstract>
    <keywordSet>
      <keyword>snow</keyword>
      <keyword>snow accumulation</keyword>
      <keyword>snow depth</keyword>
      <keywordThesaurus>LTER Controlled Vocabulary</keywordThesaurus>
    </keywordSet>
    <keywordSet>
      <keyword>disturbance</keyword>
      <keywordThesaurus>LTER Core Areas</keywordThesaurus>
    </keywordSet>
    <additionalInfo>
      <para>
        <literalLayout>&#160;In some circumstances we have the opportunity or need to measure the glaciers in mid-season (Dec).&#160; View the dates the measurements were made at the following URL: http://www.mcmlter.org/data/glaciers/timing/weqdates.pdf</literalLayout>
      </para>
    </additionalInfo>
    <intellectualRights>
      <section>
        <title>Data Policies</title>
        <para>
          <literalLayout>This data package is released under the Creative Commons Attribution 4.0 International License (CC BY 4.0; http://creativecommons.org/licenses/by/4.0/), which allows consumers (hereinafter referred to as “Data Users”) to freely reuse, redistribute, transform, or build on this work (even commercially) so long as appropriate credit is provided. Accordingly, Data Users are required to properly cite this data package in any publications or in the metadata of any derived products that result from its use (in whole or in part). A recommended citation is provided on the summary metadata page associated with this data package in the McMurdo Dry Valleys LTER Data Catalog (https://mcmlter.org/data), and a generic citation may be found on the summary metadata page in the repository where this data package was obtained. When these data contribute significantly to the contents of a publication, Data Users must also acknowledge that data were provided by the NSF-supported McMurdo Dry Valleys Long Term Ecological Research program (OPP-2224760). This data package has been released in the spirit of open scientific collaboration. Hence, Data Users are strongly encouraged to consider consultation, collaboration, and/or co-authorship (as appropriate) with the data package creator(s). Data Users should be aware these data may be actively used by others for ongoing research; thus, coordination may be necessary to prevent duplicate publication. Data Users should also recognize that misinterpretation of data may occur if they are used outside the context of the original study. Hence, Data Users are urged to contact the data package creator(s) if they have any questions regarding methodology or results. While substantial efforts are made to ensure the accuracy of this data package (with all its components), complete accuracy cannot be guaranteed. Periodic updates to this data package may occur, and it is the responsibility of Data Users to check for new versions. This data package is made available “as is” and comes with no warranty of accuracy or fitness for use. The creator(s) of this data package and the repository where these data were obtained shall not be liable for any damages resulting from misinterpretation, use, or misuse of these data. Finally, as a professional courtesy, we kindly request Data Users notify the primary contact referenced in the metadata when these data are used in the production of any derivative work or publication. Notification should include an explanation of how the data were used, along with a digital copy of the derived product(s). Thank you.</literalLayout>
        </para>
      </section>
    </intellectualRights>
    <distribution>
      <online>
        <url function="information">https://mcm.lternet.edu/content/snow-ice-and-total-glacier-mass-balance-measurements-mcmurdo-dry-valleys-antarctica-1993</url>
      </online>
    </distribution>
    <coverage>
      <geographicCoverage>
        <geographicDescription>Located in the Miers Valley, this glacier became object of the MCMLTER program study in 2015.</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>163.582477569580</westBoundingCoordinate>
          <eastBoundingCoordinate>163.732166290280</eastBoundingCoordinate>
          <northBoundingCoordinate>-78.097276633989</northBoundingCoordinate>
          <southBoundingCoordinate>-78.118713184740</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The Canada Glacier a small&#160;glacier&#160;flowing south-east into the northern side of&#160;Taylor Valley. &#160;The glacier receives less than 10&#160;cm of snowfall annually. Its seasonal&#160;melting feeds&#160;Lake Hoare&#160;to the west and&#160;Lake Fryxell&#160;to the east.</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>162.894287109375</westBoundingCoordinate>
          <eastBoundingCoordinate>163.057708740234</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.598403930664</northBoundingCoordinate>
          <southBoundingCoordinate>-77.632133483887</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The Commonwealth&#160;glacier&#160;flows in a southeasterly direction and enters the northern side of&#160;Taylor Valley&#160;immediately west of&#160;Mount Coleman. Named by the British Antarctic Expedition&#160;for the&#160;Commonwealth of Australia&#160;in the early 1900s. &#160;</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>163.197784423828</westBoundingCoordinate>
          <eastBoundingCoordinate>163.373565673828</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.545059204102</northBoundingCoordinate>
          <southBoundingCoordinate>-77.589111328125</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>286</altitudeMinimum>
            <altitudeMaximum>286</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Howard is a small alpine&#160;glacier&#160;just west of&#160;Crescent Glacier, flowing into&#160;Taylor Valley&#160;on the north from the&#160;Kukri Hills. Geologist&#160;T.L. Pewe&#160;studied and named it for&#160;Arthur D. Howard,</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>163.036087036133</westBoundingCoordinate>
          <eastBoundingCoordinate>163.147994995117</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.662025451660</northBoundingCoordinate>
          <southBoundingCoordinate>-77.687744140625</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>717</altitudeMinimum>
            <altitudeMaximum>717</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Hughes Glacier is a small alpine&#160;glacier&#160;flowing toward&#160;Lake Bonney&#160;in&#160;Taylor Valley&#160;from the&#160;Kukri Hills&#160;on the south.&#160;Named for Professor&#160;McKenny Hughes.</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>162.437667846680</westBoundingCoordinate>
          <eastBoundingCoordinate>162.581527709961</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.727073669434</northBoundingCoordinate>
          <southBoundingCoordinate>-77.749969482422</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The Suess Glacier is&#160;between the&#160;Canada Glacier&#160;and&#160;Lacroix Glacier, flowing south into&#160;Taylor Valley. Scott named after the early nineties&#160;British Antarctic Expedition&#160;for Professor&#160;Eduard Suess.</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>162.647781372070</westBoundingCoordinate>
          <eastBoundingCoordinate>162.744598388672</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.633750915527</northBoundingCoordinate>
          <southBoundingCoordinate>-77.651824951172</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>1000</altitudeMinimum>
            <altitudeMaximum>1000</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The&#160;Taylor Glacier&#160;is an&#160;Antarctic&#160;glacier&#160;about 54 kilometres (34&#160;mi) long, flowing from the plateau of&#160;Victoria Land&#160;into the western end of&#160;Taylor Valley, north of the&#160;Kukri Hills, south of the&#160;Asgard Range. The middle part of the glacier is bounded on the south by&#160;Beacon Valley.Scott&#160;(early nineties British Antarctic expedition) named the glacier for&#160;Griffith Taylor, geologist and leader of the Western Journey Party of the British Antarctic expedition.Like other glaciers in the&#160;McMurdo Dry Valleys, Taylor Glacier is “cold-based,” meaning its bottom is frozen to the ground below.&#160;&#160;</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>161.683044433594</westBoundingCoordinate>
          <eastBoundingCoordinate>162.280426025391</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.721229553223</northBoundingCoordinate>
          <southBoundingCoordinate>-77.769035339355</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <temporalCoverage>
        <rangeOfDates>
          <beginDate>
            <calendarDate>1993-10-22</calendarDate>
          </beginDate>
          <endDate>
            <calendarDate>2023-01-24</calendarDate>
          </endDate>
        </rangeOfDates>
      </temporalCoverage>
    </coverage>
    <purpose>
      <para>
        <literalLayout>The goal of each summer season is to take measurements in early spring (Oct/Nov) and late summer (late January). This provides a measure of seasonal winter/summer changes of glacier mass.</literalLayout>
      </para>
    </purpose>
    <maintenance>
      <description>
        <para>
          <literalLayout>&#160; Data for the glacier snow and ice mass changes was submitted by Andrew G. Fountain to the &#160;data manager in August, 1997. The column showing "file name" identifies the original file containing that record. These are provenance ascii text files and can be found by the McMurdo &#160;LTER data manager's office. &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160;&#160; Once submitted, the data manager used Microsoft Excel and Access software to produce files that were in more of a relational mode. Based on feedback from Andrew G. Fountain and Karen Lewis, unnecessary fields (such as ice height change, snow height &#160;change, and range) were removed, and others (such as snow WEQ change) were added &#160;to the file. &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160;&#160; &#160;In March, 2000, Thomas Nylen revised the existing data, and added new data from the &#160;more recent seasons. Instead of lumping all of the results for each glacier under one file, they were separated into files for each glacier. Results for Hughes and Suess glaciers were also added. Changes made to the original data can be viewed by clicking here. Metadata fields were also revised at this time. &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160;&#160; In April, 2000, Denise Steigerwald added fields for dataset code and glstkid. Dataset code &#160;would allow the data to be linked to the metadata in a relational database. Glstkid is a code that ties stake records to points on a GIS base map being developed by Michael Prentice at the &#160;University of New Hampshire. &#160; &#160; &#160; In 2006, Chris Gardner and Inigo San Gil standardized the metadata using the EML format. &#160;In addition, metadata was distributed at the LTER Metadata catalogs and Federal metadata clearinghouses. &#160; &#160; In 2014, metadata was revamped by Inigo San Gil, using the Drupal Ecological Metadata Language &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160; &#160;&#160;</literalLayout>
        </para>
      </description>
    </maintenance>
    <contact>
      <individualName>
        <givenName>McMurdo Dry Valleys LTER</givenName>
        <surName>Information Manager</surName>
      </individualName>
      <electronicMailAddress>im@mcmlter.org</electronicMailAddress>
    </contact>
    <publisher>
      <organizationName>McMurdo Dry Valleys LTER</organizationName>
      <onlineUrl>http://mcmlter.org/</onlineUrl>
    </publisher>
    <pubPlace>McMurdo Dry Valleys LTER</pubPlace>
    <methods>
      <methodStep>
        <description>
          <section>
            <para>
              <literalLayout>The methods of data collection are described in the glacier stake heights, snow depths and glacier snow density metadata files. To convert the data to mass values, the total change in ice height (usually negative) and snow height (depth for snow covered ice) at each stake are multiplied by their respective densities. The density for ice is 0.9 g/cm3 and the density for snow is measured in nearby snowpits. The final error of the mass balance measurement is based on the errors in the stake heights and snow depths found by replicated measurements. The errors were carried through the calculations based on Baird, D.C., 1962. Experimentation: An Introduction to Measurement Theory and Experiment Design. Prentice Hall, Englewood. We assume no error in the snow density measurements. A Note about Stake names A stake with an H or V indicates a stake along the ice cliff that forms the boundary of the glacier terminus. An H is a horizontal stake placed into the vertical wall of the glacier terminus, and V is a stake placed into the ice apron at the base of the ice cliff. The vertical stakes were installed to support the horizontal stakes and provide a nearby measure of ablation for a surface with a much different slope. A Note about the Zone variable: The accumulation zone is the region on the glacier where snow accumulation exceeds ablation, therefore the region is always snow covered, and typically restricted to the higher altitudes of the glacier. The ablation zone is the region where ablation exceeds snow accumulation and the surface is ice, although occasionally covered with seasonal snow. This is important for evaluating the other variables. In the accumulation zone, for example, there will be no height to ice. A Note about Ice WEQ Change: The density used can be calculated from snow height change, or directly examined in the glacier snow density file. A Note about Standard Deviation Calculations: During the early years only one or two measurements of surface height were taken at each stake. If two measurements were taken, the average was used and the range expressed as the error; note of this was made in "comments" field. If greater than 2 measurements of surface height and snow depth were taken, standard deviation of Total WEQ Change was based on a calculation of errors.</literalLayout>
            </para>
          </section>
        </description>
      </methodStep>
    </methods>
    <dataTable>
      <entityName>ADAMSCHNG</entityName>
      <entityDescription>Adams Glacier - Mass Balance</entityDescription>
      <physical>
        <objectName>mcmlter-glac-adams-masschange-20250311.csv</objectName>
        <size>16905</size>
        <dataFormat>
          <textFormat>
            <numHeaderLines>1</numHeaderLines>
            <numFooterLines>1</numFooterLines>
            <recordDelimiter>\n</recordDelimiter>
            <attributeOrientation>column</attributeOrientation>
            <simpleDelimited>
              <fieldDelimiter>,</fieldDelimiter>
              <quoteCharacter>"</quoteCharacter>
            </simpleDelimited>
          </textFormat>
        </dataFormat>
        <distribution>
          <online>
            <url>https://mcm.lternet.edu/sites/default/files/data/mcmlter-glac-adams-masschange-20250311.csv</url>
          </online>
        </distribution>
      </physical>
      <attributeList>
        <attribute>
          <attributeName>DATASET CODE</attributeName>
          <attributeLabel>DATASET CODE</attributeLabel>
          <attributeDefinition>CODE REPRESENTING GLACIER SNOW AND ICE MASS CHANGES DATASET</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>CODE REPRESENTING GLACIER SNOW AND ICE MASS CHANGES DATASET</definition>
                </textDomain>
              </nonNumericDomain>
            </nominal>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>GLACIER</attributeName>
          <attributeLabel>GLACIER</attributeLabel>
          <attributeDefinition>NAME OF GLACIER WHERE MEASUREMENT WAS MADE</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>NAME OF GLACIER WHERE MEASUREMENT WAS MADE</definition>
                </textDomain>
              </nonNumericDomain>
            </nominal>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>STAKE</attributeName>
          <attributeLabel>STAKE</attributeLabel>
          <attributeDefinition>UNIQUE NUMBER FOR EACH STAKE ON GLACIER</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>UNIQUE NUMBER FOR EACH STAKE ON GLACIER</definition>
                </textDomain>
              </nonNumericDomain>
            </nominal>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>START_DATE</attributeName>
          <attributeLabel>START_DATE</attributeLabel>
          <attributeDefinition>BEGINNING DATE OF DATA MEASUREMENT</attributeDefinition>
          <storageType>date</storageType>
          <measurementScale>
            <dateTime>
              <formatString>MM/DD/YYYY</formatString>
            </dateTime>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>END_DATE</attributeName>
          <attributeLabel>END_DATE</attributeLabel>
          <attributeDefinition>ENDING DATE OF DATA MEASUREMENT</attributeDefinition>
          <storageType>date</storageType>
          <measurementScale>
            <dateTime>
              <formatString>MM/DD/YYYY</formatString>
            </dateTime>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>ZONE</attributeName>
          <attributeLabel>ZONE</attributeLabel>
          <attributeDefinition>REGION OF THE GLACIER (ABLATION OR ACCUMULATION)</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>REGION OF THE GLACIER (ABLATION OR ACCUMULATION)</definition>
                </textDomain>
              </nonNumericDomain>
            </nominal>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>SNOW_WEQ_CHANGE</attributeName>
          <attributeLabel>SNOW_WEQ_CHANGE</attributeLabel>
          <attributeDefinition>SNOW HEIGHT CHANGE IN TERMS OF WATER EQUIVALENT - Cm3/Cm2 (cm water depth)</attributeDefinition>
          <measurementScale>
            <ratio>
              <unit>
                <customUnit>Cm3/Cm2</customUnit>
              </unit>
              <numericDomain>
                <numberType>real</numberType>
              </numericDomain>
            </ratio>
          </measurementScale>
          <missingValueCode>
            <code>NULL</code>
            <codeExplanation>None given</codeExplanation>
          </missingValueCode>
        </attribute>
        <attribute>
          <attributeName>ICE_WEQ_CHANGE</attributeName>
          <attributeLabel>ICE_WEQ_CHANGE</attributeLabel>
          <attributeDefinition>ICE HEIGHT CHANGE IN TERMS OF WATER EQUIVALENT - Cm3/Cm2 (cm water depth)</attributeDefinition>
          <measurementScale>
            <ratio>
              <unit>
                <customUnit>Cm3/Cm2</customUnit>
              </unit>
              <numericDomain>
                <numberType>real</numberType>
              </numericDomain>
            </ratio>
          </measurementScale>
          <missingValueCode>
            <code>NULL</code>
            <codeExplanation>None given</codeExplanation>
          </missingValueCode>
        </attribute>
        <attribute>
          <attributeName>TOTAL_WEQ_CHANGE</attributeName>
          <attributeLabel>TOTAL_WEQ_CHANGE</attributeLabel>
          <attributeDefinition>Total mass change in terms of water equivalent (sum of ice WEQ change and snow WEQ change; ice density = 0.9g/cm3)</attributeDefinition>
          <measurementScale>
            <ratio>
              <unit>
                <customUnit>Cm3/Cm2</customUnit>
              </unit>
              <precision>0.1</precision>
              <numericDomain>
                <numberType>real</numberType>
                <bounds>
                  <maximum exclusive="false">400</maximum>
                </bounds>
              </numericDomain>
            </ratio>
          </measurementScale>
          <missingValueCode>
            <code>NULL</code>
            <codeExplanation>None given</codeExplanation>
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            </nominal>
          </measurementScale>
        </attribute>
      </attributeList>
    </dataTable>
  </dataset>
  <additionalMetadata>
    <metadata>
      <stmml:unitList xmlns:stmml="http://www.xml-cml.org/schema/stmml-1.1" xmlns="http://www.xml-cml.org/schema/stmml" xmlns:sch="http://www.ascc.net/xml/schematron" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.xml-cml.org/schema/stmml-1.1 http://nis.lternet.edu/schemas/EML/eml-2.1.0/stmml.xsd">
        <stmml:unit id="Cm3/Cm2" name="Cm3/Cm2" abbreviation="" unitType="">
          <stmml:description />
        </stmml:unit>
      </stmml:unitList>
    </metadata>
  </additionalMetadata>
</eml:eml>