Latitudinal Change of Tropical Cyclone Maximum Intensity in the Western North Pacific

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/5829162/figures/5829162.fig.004a.svgz" name="5829162.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Outgoing longwave radiation</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/5829162/figures/5829162.fig.004b.svgz" name="5829162.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>600 hPa relative humidity</td></tr></table>

<div>Same as in Figure <a href="../fig3/">3</a>, bur for (a) outgoing longwave radiation (OLR) and (b) 600 hPa relative humidity. In (b), contour interval is 1% and shaded areas are significant at the 95% confidence level.</div>

Advances in Meteorology

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Figure 4

Figure 4: Latitudinal Change of Tropical Cyclone Maximum Intensity in the Western North Pacific 