Simulation and Analysis of Land-Surface Processes in the Taklimakan Desert Based on Noah LSM

<div>Contrast curve between the simulated (black) and observed (red) soil heat flux (<span class="nowrap"><svg height="11.927pt" id="M19" style="vertical-align:-3.291101pt" version="1.1" viewbox="-0.0498162 -8.6359 13.9062 11.927" width="13.9062pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.013,0,0,-0.013,0,0)"><path d="M673 297H417L411 270C517 261 522 258 506 183L487 92C476 38 428 19 360 19C207 19 123 132 123 287C123 472 243 631 441 631C557 631 617 583 617 469L647 472C650 545 655 604 658 632C625 643 554 666 467 666C201 666 23 502 23 278C23 90 156 -16 339 -16C410 -16 501 6 569 24C566 43 567 70 573 101L589 183C604 259 607 262 667 271L673 297Z"></path></g><g transform="matrix(.0091,0,0,-0.0091,8.827,3.132)"><path d="M245 635C92 635 37 457 37 312C37 149 91 -12 244 -12C395 -12 449 166 449 312C449 469 395 635 245 635ZM243 598C332 598 358 454 358 312C358 173 334 26 245 26C158 26 128 174 128 313S152 598 243 598Z"></path></g></svg>)</span> for the four weather types at the Tazhong station in 2014.</div>

Advances in Meteorology

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Figure 10

Figure 10: Simulation and Analysis of Land-Surface Processes in the Taklimakan Desert Based on Noah LSM 