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首页> 外文期刊>Journal of geophysical research. Planets >Mars Science Laboratory diurnal moisture observations and column simulations
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Mars Science Laboratory diurnal moisture observations and column simulations

机译:火星科学实验室日间湿度观测和色谱柱模拟

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摘要

Hourly observations of air temperature and relative humidity at 1.6m height from the surface(T 1.6m, RH 1.6m) measured by the Mars Science Laboratory (MSL) Rover Environmental Monitoring Station relative humidity (REMS-H) device are shown for MSL solar days 15–17 and 80–82, augmented with column model simulations. The diurnal range of T 1.6mwas 197–268 K in the first period, RH 1.6mbeing small (<1%) in daytime but increasing to 45–49% by sunrise. During the warmer second period the T 1.6m range was 201–275 K with RH 1.6m only up to 16% in the morning. The modeled temperatures were quite close to those observed when the local albedo was set to 0.15 and thermal inertia to 300 tiu. The modeled RH 1.6m was close to that observed when the well-mixed boundary layer values (0–4 km) of the mass mixing ratio q were 28–30ppmm (suggesting a precipitable water content (PWC) of ~5.5 μm) during the first period and 12 ppmm (PWC of ~2 μm) during the second period. The REMS-H observations indicate systematic diurnal variation in the near-surface mixing ratio.
机译:显示了由火星科学实验室(MSL)罗孚环境监测站相对湿度(REMS-H)设备测得的距地面1.6m高度(T 1.6m,RH 1.6m)处的每小时温度和相对湿度的观测值第15–17天和第80–82天,增加了列模型模拟。在第一时期,T 1.6m的日变化范围为197–268 K,白天的相对湿度1.6 m较小(<1%),但到日出时则增加至45–49%。在第二个较暖的时期,T 1.6m范围为201–275 K,相对湿度为1.6m,早晨最高可达16%。模拟的温度与局部反照率设定为0.15,热惯性设定为300 tiu时所观察到的温度非常接近。模拟的RH 1.6m接近于质量混合比q的充分混合的边界层值(0–4 km)为28–30ppmm(建议在约5.5μm的可沉淀水含量(PWC))时观察到的RH。第一阶段为12 ppmm(PWC约为2μm)。 REMS-H观测结果表明近地表混合比的系统日变化。

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