Study on the Influence of Aerosol Radiation Balance in One-Dimensional Atmospheric Medium Using <svg xmlns:xlink="http://www.w3.org/1999/xlink" xmlns="http://www.w3.org/2000/svg" style="vertical-align:-4.5247pt" id="M1" height="16.402pt" version="1.1" viewBox="-0.0657574 -11.8773 16.4133 16.402" width="16.4133pt"><g transform="matrix(.018,0,0,-0.018,0,0)"><path id="g113-81" d="M600 480C600 590 528 650 384 650H143L137 622C222 614 225 607 210 531L130 127C113 41 106 36 23 28L17 0H294L300 28C204 36 195 42 212 127L243 284L314 263C327 263 339 263 352 264C465 271 600 337 600 480ZM508 481C508 351 402 304 329 304C289 304 265 311 250 317L295 559C302 594 310 606 323 611C335 616 350 619 367 619C455 619 508 573 508 481Z"/></g><g transform="matrix(.013,0,0,-0.013,9.157,4.308)"><path id="g50-111" d="M504 89L488 119C453 85 428 69 416 69C408 69 405 75 412 102L462 304C492 438 460 451 436 451S388 441 356 423C311 397 229 336 170 256H168L189 340C208 418 200 451 177 451C144 451 82 413 24 352L40 322C65 345 98 369 108 369C114 369 119 363 112 335L28 -3L36 -12C54 -3 83 4 112 10C125 73 138 122 153 174C205 258 328 382 376 382C395 382 399 369 384 305L330 93C312 25 323 -12 351 -12C378 -12 439 21 504 89Z"/></g></svg>-Approximation Method

<table class="table-group" width="800px"><tr class="fig-image" id="a"><td><img alt="767231.fig.003a" src="https://static.hindawi.com/articles/mpe/volume-2014/767231/figures/767231.fig.003a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>Atmosphere temperature field (0–50 km)</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="767231.fig.003b" src="https://static.hindawi.com/articles/mpe/volume-2014/767231/figures/767231.fig.003b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>Atmosphere temperature field (0–10 km)</td></tr></table></td></tr></table>

<table>Influence of aerosols species on temperature fields.</table>

Mathematical Problems in Engineering

fig3

Figure 3

Figure 3: Study on the Influence of Aerosol Radiation Balance in One-Dimensional Atmospheric Medium Using <svg xmlns:xlink="http://www.w3.org/1999/xlink" xmlns="http://www.w3.org/2000/svg" style="vertical-align:-4.5247pt" id="M1" height="16.402pt" version="1.1" viewBox="-0.0657574 -11.8773 16.4133 16.402" width="16.4133pt"><g transform="matrix(.018,0,0,-0.018,0,0)"><path id="g113-81" d="M600 480C600 590 528 650 384 650H143L137 622C222 614 225 607 210 531L130 127C113 41 106 36 23 28L17 0H294L300 28C204 36 195 42 212 127L243 284L314 263C327 263 339 263 352 264C465 271 600 337 600 480ZM508 481C508 351 402 304 329 304C289 304 265 311 250 317L295 559C302 594 310 606 323 611C335 616 350 619 367 619C455 619 508 573 508 481Z"/></g><g transform="matrix(.013,0,0,-0.013,9.157,4.308)"><path id="g50-111" d="M504 89L488 119C453 85 428 69 416 69C408 69 405 75 412 102L462 304C492 438 460 451 436 451S388 441 356 423C311 397 229 336 170 256H168L189 340C208 418 200 451 177 451C144 451 82 413 24 352L40 322C65 345 98 369 108 369C114 369 119 363 112 335L28 -3L36 -12C54 -3 83 4 112 10C125 73 138 122 153 174C205 258 328 382 376 382C395 382 399 369 384 305L330 93C312 25 323 -12 351 -12C378 -12 439 21 504 89Z"/></g></svg>-Approximation Method 

Mathematical Problems in Engineering

Study on the Influence of Aerosol Radiation Balance in One-Dimensional Atmospheric Medium Using -Approximation Method

Figure 3