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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>Tyler D. Hennon</dc:contributor>
  <dc:contributor>Daniel Monson</dc:contributor>
  <dc:contributor>Robert M. Suryan</dc:contributor>
  <dc:contributor>Rob W. Cambell</dc:contributor>
  <dc:contributor>Steven J. Baird</dc:contributor>
  <dc:contributor>Kristine Holderied</dc:contributor>
  <dc:contributor>Thomas J. Weingartner</dc:contributor>
  <dc:creator>Seth L. Danielson</dc:creator>
  <dc:date>2022</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts u-font-serif"&gt;&lt;div id="abs0010" class="abstract author" lang="en"&gt;&lt;div id="abssec0010"&gt;&lt;p id="abspara0010"&gt;Surface and subsurface moored buoy, ship-based, remotely sensed, and reanalysis datasets are used to investigate thermal variability of northern Gulf of Alaska (NGA) nearshore, coastal, and offshore waters over synoptic to century-long time scales. NGA sea surface temperature (SST) showed a larger positive trend of 0.22&amp;nbsp;±&amp;nbsp;0.10&amp;nbsp;°C per decade over 1970–2021 compared to 0.10&amp;nbsp;±&amp;nbsp;0.03&amp;nbsp;°C per decade over 1900–2021. Over synoptic time scales, SST covariance between two stations is small (&amp;lt;10%) when separation exceeds 100&amp;nbsp;km, while stations separated by 500&amp;nbsp;km retain 50% of their co-variability for seasonal and longer fluctuations. Relative to&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;in situ&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;sensor data, remotely sensed SST data has limited accuracy in some NGA settings, capturing 60–70% of the daily SST anomaly in coastal and offshore waters, but often &amp;lt;25% nearshore. North Pacific and NGA leading modes of SST variability leave 25–50% of monthly variance unresolved. Analysis of the 2014–2016 Pacific marine heatwave shows that NGA coastal surface temperatures warmed contemporaneously with offshore waters through 2013, but deep inner shelf waters (200–250&amp;nbsp;m) exhibited delayed warming. Offshore surface waters cooled from 2014 to 2016, while shelf waters continued to warm from the combined effects of local air-sea and advective heat fluxes. We find that annually averaged Sitka air temperature is a leading predictor (r&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;=&amp;nbsp;0.37, p&amp;nbsp;&amp;lt;&amp;nbsp;0.05) for following-year NGA coastal water column temperature. Our results can inform future environmental monitoring designs, assist forward-looking projections of marine conditions, and show the importance of&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;in situ&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;measurements for nearshore studies that require knowledge of thermal conditions over time scales of days and weeks.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.dsr2.2022.105155</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Temperature variations in the northern Gulf of Alaska across synoptic to century-long time scales</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>