<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Benjamin M. Jones</dc:contributor>
  <dc:contributor>Krista K. Bartz</dc:contributor>
  <dc:contributor>Daniel Young</dc:contributor>
  <dc:contributor>Christian E. Zimmerman</dc:contributor>
  <dc:creator>Carson Baughman</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Lake Clark is an important nursery lake for sockeye salmon (&lt;/span&gt;&lt;i&gt;Oncorhynchus nerka&lt;/i&gt;&lt;span&gt;) in the headwaters of Bristol Bay, Alaska, the most productive wild salmon fishery in the world. Reductions in water clarity within Alaska lake systems as a result of increased glacial runoff have been shown to reduce salmon production via reduced abundance of zooplankton and macroinvertebrates. In this study, we reconstruct long-term, lake-wide water clarity for Lake Clark using the Landsat TM and ETM+ surface reflectance products (1985–2014) and&lt;/span&gt;&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in situ&lt;/i&gt;&lt;span&gt;water clarity data collected between 2009 and 2013. Analysis of a Landsat scene acquired in 2009, coincident with&lt;/span&gt;&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in situ&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&lt;span&gt;measurements in the lake, and uncertainty analysis with four scenes acquired within two weeks of field data collection showed that Band 3 surface reflectance was the best indicator of turbidity (&lt;/span&gt;&lt;i&gt;r&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&lt;span&gt;= 0.55,&lt;/span&gt;&lt;i&gt;RMSE&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&lt;span&gt;&amp;lt;&amp;lt; 0.01). We then processed 151 (98 partial- and 53 whole-lake) Landsat scenes using this relation and detected no significant long-term trend in mean turbidity for Lake Clark between 1991 and 2014. We did, however, detect interannual variation that exhibited a non-significant (&lt;/span&gt;&lt;i&gt;r&lt;/i&gt;&lt;sup&gt;2&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/sup&gt;&lt;span&gt;= 0.20) but positive correlation (&lt;/span&gt;&lt;i&gt;r&lt;/i&gt;&lt;sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/sup&gt;&lt;span&gt;= 0.20) with regional mean summer air temperature and found the month of May exhibited a significant positive trend (&lt;/span&gt;&lt;i&gt;r&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&lt;span&gt;= 0.68,&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/span&gt;&lt;i&gt;p&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&lt;span&gt;= 0.02) in turbidity between 2000 and 2014. This study demonstrates the utility of hindcasting turbidity in a glacially influenced lake using the Landsat surface reflectance products. It may also help land and resource managers reconstruct turbidity records for lakes that lack&lt;/span&gt;&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in situ&lt;/i&gt;&lt;span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;monitoring, and may be useful in predicting future water clarity conditions based on projected climate scenarios.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3390/rs71013692</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>MDPI</dc:publisher>
  <dc:title>Reconstructing turbidity in a glacially influenced lake using the Landsat TM and ETM+ surface reflectance climate data record archive, Lake Clark, Alaska</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>