Analysis of Nonstationary Change of Annual Maximum Level Records in the Yangtze River Estuary

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/7205723/figures/7205723.fig.002a.svgz" name="7205723.fig.002a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Linear trend was 0.019 m/a and standard deviation was 0.350 m</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/7205723/figures/7205723.fig.002b.svgz" name="7205723.fig.002b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Linear trend was 0.013 m/a, SRC test</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/7205723/figures/7205723.fig.002c.svgz" name="7205723.fig.002c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Standard deviation was 0.350 m, MK test</td></tr></table>

<div>Relationship between trend test efficiency and sample size in different combinations.</div>

Advances in Meteorology

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Figure 2

Figure 2: Analysis of Nonstationary Change of Annual Maximum Level Records in the Yangtze River Estuary 