Effects of Ocean Ecosystem on Marine Aerosol-Cloud Interaction

<table>Time series of the area-averaged MODIS Aerosol optical depth (AOD), liquid cloud effective radii (<svg height="11.9625" id="M160" style="vertical-align:-3.3907pt" version="1.1" viewbox="0 0 12.85 11.9625" width="12.85" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
<g transform="matrix(.017,-0,0,-.017,.062,7.675)"><path d="M393 379q-9 -16 -28 -29q-15 -10 -23 -2q-19 19 -36 19q-21 0 -52 -38q-57 -72 -82 -126l-40 -197q-23 -3 -75 -18l-7 7q49 196 74 335q7 43 -2 43q-7 0 -30 -14.5t-47 -37.5l-16 23q37 42 82 73t67 31q41 0 15 -113l-11 -50h4q41 71 85 117t77 46q29 0 45 -26
q13 -21 0 -43z" id="x1D45F"></path></g>
<g transform="matrix(.012,-0,0,-.012,7.238,11.762)"><path d="M391 364q0 -28 -20.5 -53.5t-50 -43.5t-70 -34t-73.5 -25t-68 -17v-29q0 -48 20 -81t65 -33q73 0 157 76l16 -23q-107 -113 -221 -113q-21 0 -40.5 6.5t-39 22t-31.5 47t-12 75.5q0 69 33.5 139.5t95.5 114.5q77 55 143 55q42 0 69 -24.5t27 -59.5zM313 350
q0 26 -14.5 40.5t-37.5 14.5q-32 0 -44 -7q-82 -46 -104 -175q200 49 200 127z" id="x1D452"></path></g>
</svg>), sea surface temperature (SST), liquid water path (LWP), liquid cloud optical thickness (COT), liquid cloud top pressure (CTP) and SeaWiFS [Chl-<i>a</i>] in Northwest Atlantic (42°N to 60°N and 55°W to 21°W).</table>

Advances in Meteorology

Effects of Ocean Ecosystem on Marine Aerosol-Cloud Interaction

Figure 1