Add Olson, et al (2020) to publications page

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+  <h2>Salish Model Ecosystem-Lower Trophic (SMELT), the biological component of SalishSeaCast</h2>
+  <p>
+    The 3 nutrient- 3 phytoplankton- 1.5 zooplankton compartment model described in
+    Moore-Maley et al . (2016) was adapted to three dimensions and coupled to the Salish
+    Sea NEMO model described by Soontiens et al. (2016). Description and evaluation of the
+    model can be found in:
+  </p>
+  <p>
+    Olson, E. M., S. E. Allen, V. Do, M. Dunphy, and D. Ianson (in press).
+    Assessment of Nutrient Supply by a Tidal Jet in the Northern Strait of Georgia Based on a Biogeochemical Model.
+    J. Geophys. Res. Oceans.
+  </p>
+  <p>
+    <a href="https://dx.doi.org/10.1029/2019JC015766">
+      https://dx.doi.org/10.1029/2019JC015766
+    </a>
+  </p>
+
+
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       <h2>BibTeX Citations</h2>
@@ -249,6 +268,53 @@ suggests that the removal of the Hollingsworth instability will correct a fresh
 drift in the deep and intermediate waters in an operational version of this
 model.",
     doi = "10.1002/2015JC011118",
+}
+      </pre>
+    </div>
+  </div>
+
+  <div class="row">
+    <div class="col-md-12">
+      <h3>
+        Olson, <em>et al</em>, 2020,
+        Assessment of Nutrient Supply by a Tidal Jet in the Northern Strait of Georgia Based on a Biogeochemical Model
+      </h3>
+    </div>
+  </div>
+  <div class="row">
+    <div class="col-md-8 col-md-offset-1">
+      <pre>
+@unpublished{Olson-etal-2020,
+    author = "Olson, E. M. and S. E. Allen and V. Do and M. Dunphy and D. Ianson",
+    title = "Assessment of Nutrient Supply by a Tidal Jet in the
+Northern Strait of Georgia Based on a Biogeochemical Model",
+    journal = "Journal of Geophysical Research: Oceans",
+    year = "2020",
+    note = "(in press)",
+    url = "https://dx.doi.org/10.1029/2019JC015766",
+    keywords = "nitrate, tidal jet, Discovery Passage, Strait of Georgia,
+biogeochemical model, new production",
+    abstract = "We present a coupled three-dimensional biological-physical model for
+the Salish Sea and evaluate it by comparison to nitrate, silicate, and chlorophyll
+observations. It accurately reproduces nitrate concentrations with Willmott skill
+scores, root mean squared error, and bias ranging from 0.84–0.95, 4.02–6.5 μM,
+and −2.33–1.84 μM, respectively, compared to three independent discrete sample
+data sets. A prominent feature of the model output is a tidal jet emanating from
+Discovery Passage producing a downstream plume of elevated surface nitrate.
+The signal is present from April to September, when surface nitrate is otherwise
+drawn down. It has a weak but statistically significant correlation to
+Discovery Passage tidal velocity (R=0.37, p<0.01). Within the turbulent jet and
+associated plume, the average rate of vertical nitrate supply due to mixing and
+advection across a depth of roughly 6 m is 0.46 μmol m−2 s−1 between May 15, 2015,
+and August 20, 2015, compared to 0.10 μmol m−2 s−1 for the northern Strait of Georgia
+as a whole. Close to Discovery Passage, where velocities and shear are strongest,
+the majority of the vertical nitrate flux is due to mixing. As velocities weaken
+downstream, vertical advection becomes more important relative to mixing, but vertical
+velocities also decrease. The tidal pulses out of Discovery Passage drive waves that
+contribute net upward nitrate flux as far south as Cape Lazo, 40 km away. The nitrate
+supply drives new production, consistent with existing observations. Similar dynamics
+have been described in many other tidally influenced coastal systems.",
+    doi = "10.1029/2019JC015766",
 }
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