Amazon Rainforest Exchange of Carbon and Subcanopy Air Flow: Manaus LBA Site—A Complex Terrain Condition

<table class="table-group" width="800px"><tr class="fig-image" id="a"><td><img alt="165067.fig.009a" src="https://static.hindawi.com/articles/tswj/volume-2012/165067/figures/165067.fig.009a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>Dry period-2006</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="165067.fig.009b" src="https://static.hindawi.com/articles/tswj/volume-2012/165067/figures/165067.fig.009b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>Wet period-2006</td></tr></table></td></tr><tr class="fig-image" id="c"><td><img alt="165067.fig.009c" src="https://static.hindawi.com/articles/tswj/volume-2012/165067/figures/165067.fig.009c.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(c) </b>Vertical Gradient of the Virtual Potential Temperature-DRAINO System south slopE</td></tr></table></td></tr></table>

<table>Daily course of the vertical deviation of the virtual potential temperature for dry (a) and wet (b) periods of the year 2006, and the virtual potential temperature vertical gradient (c), over slope area DRAINO system tower.</table>

The Scientific World Journal

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Figure 9

Figure 9: Amazon Rainforest Exchange of Carbon and Subcanopy Air Flow: Manaus LBA Site—A Complex Terrain Condition 