Optimal Configuration Method of Sampling Points Based on Variability of Sea Surface Temperature

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/5638289/figures/5638289.fig.002a.svgz" name="5638289.fig.002a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Monthly mean SST field</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/5638289/figures/5638289.fig.002b.svgz" name="5638289.fig.002b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Sub-SST field</td></tr></table>

<div>The monthly mean SST field in February 2009 in the East China Sea.</div>

Advances in Meteorology

fig2

Figure 2

Figure 2: Optimal Configuration Method of Sampling Points Based on Variability of Sea Surface Temperature 