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Evolution of water vapor profiles over complex terrain: observation and comparison with model simulations in the valley of Cosenza

机译:复杂地形上水汽剖面的演变:科森扎山谷的观测与模型模拟的比较

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Abstract: We have measured and simulated the evolution of the diurnal water vapor profile over the Crati valley during a clear sky summer day. A twin TEA CO$-2$/ laser based dial (Differential Absorption Lidar) system has been developed to measure the water vapor profiles. The acquired data shows the vertical daily trend at a range up to 1.5 km. These measurements are compared with modeled profiles. The simulations have been performed using the CSU-RAMS model. Preliminary results show that the orography plays a fundamental role in determining the vertical distribution of water vapor and in the development of the Planetary Boundary Layer (PBL). The diurnal evolution of the PBL can be inferred from the measured profiles and, as a consequence, they can be used to improve the model. The measured and modeled vertical profiles show reasonable agreement.!11
机译:摘要:我们已经测量并模拟了夏季晴天在Crati山谷上昼间水汽剖面的演变。已经开发了基于TEA CO $ -2 $ /激光的双刻度盘(差分吸收激光雷达)系统来测量水蒸气剖面。所获取的数据显示了在1.5 km范围内的垂直日趋势。将这些测量结果与建模的轮廓进行比较。使用CSU-RAMS模型进行了仿真。初步结果表明,地形学在确定水蒸气的垂直分布和行星边界层(PBL)的发展中起着基本作用。 PBL的日变化可以从测得的廓线中推断出来,因此,它们可以用于改进模型。测量和建模的垂直剖面显示合理的一致性。!11

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