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<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>Cynthia S. Loftin</dc:contributor>
  <dc:contributor>Steven A. Sader</dc:contributor>
  <dc:creator>Ian M. McCullough</dc:creator>
  <dc:date>2013</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Water clarity is a strong indicator of regional water quality. Unlike other common water-quality metrics, such as chlorophyll&amp;nbsp;&lt;/span&gt;&lt;i&gt;a&lt;/i&gt;&lt;span&gt;, total P, or trophic status, clarity can be accurately and efficiently estimated remotely on a regional scale. Satellite-based remote sensing is useful in regions with many lakes where traditional field-sampling techniques may be prohibitively expensive. Repeated sampling of easily accessed lakes can lead to spatially irregular, nonrandom samples of a region. Remote sensing remedies this problem. We applied a remote monitoring protocol we had previously developed for Maine lakes &amp;gt;8&amp;nbsp;ha based on Landsat satellite data recorded during 1995&amp;ndash;2010 to identify spatial and temporal patterns in Maine lake clarity. We focused on the overlapping region of Landsat paths 11 and 12 to increase availability of cloud-free images in August and early September, a period of relative lake stability and seasonal poor-clarity conditions well suited for annual monitoring. We divided Maine into 3 regions (northeastern, south-central, western) based on morphometric and chemical lake features. We found a general decrease in average statewide lake clarity from 4.94 to 4.38&amp;nbsp;m during 1995&amp;ndash;2010. Water clarity ranged from 4 to 6&amp;nbsp;m during 1995&amp;ndash;2010, but it decreased consistently during 2005&amp;ndash;2010. Clarity in both the northeastern and western lake regions has decreased from 5.22&amp;nbsp;m in 1995 to 4.36 and 4.21&amp;nbsp;m, respectively, in 2010, whereas lake clarity in the south-central lake region (4.50&amp;nbsp;m) has not changed since 1995. Climate change, timber harvesting, or watershed morphometry may be responsible for regional water-clarity decline. Remote sensing of regional water clarity provides a more complete spatial perspective of lake water quality than existing, interest-based sampling. However, field sampling done under existing monitoring programs can be used to calibrate accurate models designed to estimate water clarity remotely.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1899/12-070.1</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>The University of Chicago Press</dc:publisher>
  <dc:title>Landsat imagery reveals declining clarity of Maine’s lakes during 1995-2010</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>