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DAS-2238 - precommit fixes for trailing spaces
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tests/data/SC_SPL3FTP_004.dmr

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Original file line numberDiff line numberDiff line change
@@ -3357,7 +3357,7 @@ H5.EnableCheckNameClashing=true
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</gmd:purpose>
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<gmd:credit>
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<!-- This field can name individuals or organizations for credit. For now, it specifies NASA. -->
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<gco:CharacterString>The software that generates the Level 3 Freeze/Thaw product and the data system that automates its production were designed and implemented
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<gco:CharacterString>The software that generates the Level 3 Freeze/Thaw product and the data system that automates its production were designed and implemented
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at the Jet Propulsion Laboratory, California Institute of Technology in Pasadena, California.</gco:CharacterString>
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</gmd:credit>
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<gmd:status>
@@ -3478,8 +3478,8 @@ H5.EnableCheckNameClashing=true
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</gmd:thesaurusName>
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</gmd:MD_Keywords>
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</gmd:descriptiveKeywords>
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<gmd:aggregationInfo>
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<gmd:MD_AggregateInformation>
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<gmd:aggregationInfo>
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<gmd:MD_AggregateInformation>
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<gmd:aggregateDataSetIdentifier>
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<gmd:MD_Identifier>
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<gmd:code>
@@ -3520,11 +3520,11 @@ H5.EnableCheckNameClashing=true
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<gmd:extent>
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<gmd:EX_Extent>
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<gmd:description>
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<gco:CharacterString>Freeze-thaw binary state is retrieved from radiometer brightness temperature data on both descending (AM, fore/aft)
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<gco:CharacterString>Freeze-thaw binary state is retrieved from radiometer brightness temperature data on both descending (AM, fore/aft)
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and ascending (PM, fore-only) SMAP half-orbits. The L3_FT_P product includes only data northward of 45N latitude.
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Freeze-thaw state retrieval is inhibited for areas with permanent snow/ice and excessive static or transient open water in the cell,
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and when there is excessive RFI in the sensor data. Retrievals may be flagged as questionable for urban areas,
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mountainous areas with high elevation variability, and for cells in which the seasonal (thawed-frozen) reference
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Freeze-thaw state retrieval is inhibited for areas with permanent snow/ice and excessive static or transient open water in the cell,
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and when there is excessive RFI in the sensor data. Retrievals may be flagged as questionable for urban areas,
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mountainous areas with high elevation variability, and for cells in which the seasonal (thawed-frozen) reference
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difference is much smaller than the radiometer measurement error.</gco:CharacterString>
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</gmd:description>
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<gmd:geographicElement>
@@ -3552,7 +3552,7 @@ H5.EnableCheckNameClashing=true
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<!-- Mimics use in GHRSST. See no evidence of conformance to standard -->
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<gmd:extent>
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<gml:TimePeriod gml:id="swathTemporalExtent">
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<!-- This defines the time period covered by all SMAP Level 3 Freeze/Thaw data products.
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<!-- This defines the time period covered by all SMAP Level 3 Freeze/Thaw data products.
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ECS indicates that they will automatically extend the final time based on receipt of data products. -->
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<gml:beginPosition>2015-03-31T00:00:00.000Z</gml:beginPosition>
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<gml:endPosition>2020-12-31T00:00:00.000Z</gml:endPosition>
@@ -3757,7 +3757,7 @@ H5.EnableCheckNameClashing=true
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<Value>2023-08-31</Value>
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</Attribute>
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<Attribute name="credit" type="String">
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<Value>The software that generates the Level 3 Freeze/Thaw product and the data system that automates its production were designed and implemented
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<Value>The software that generates the Level 3 Freeze/Thaw product and the data system that automates its production were designed and implemented
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at the Jet Propulsion Laboratory, California Institute of Technology in Pasadena, California.</Value>
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</Attribute>
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<Attribute name="topicCategory" type="String">

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