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Effects of the MY34/2018 Global Dust Storm as Measured by MSL REMS in Gale Crater

机译:MY34 / 2018全球沙尘暴的影响MSL REMS在Gale Crater中测量

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The Rover Environmental Monitoring Station (REMS) instrument is on board NASA's Mars Science Laboratory (MSL) Curiosity rover. REMS has been measuring surface pressure, air, and ground brightness temperature, relative humidity, and ultraviolet (UV) irradiance since MSL's landing in 2012. In Mars Year (MY) 34 (2018) a global dust storm reached Gale Crater at L_s ~ 190°. REMS offers a unique opportunity to better understand the impact of a global dust storm on local environmental conditions, which complements previous observations by the Viking landers and Mars Exploration Rovers. All atmospheric variables measured by REMS are strongly affected albeit at different times. During the onset phase, the daily maximumUV radiation decreased by 90% between sols 2075 (opacity ~1) and 2085 (opacity ~8.5). The diurnal range in ground and air temperatures decreased by 35 and 56 K, respectively, with also a diurnal-average decrease of ~2 and 4 K respectively. The maximum relative humidity, which occurs right before sunrise, decreased to below 5%, compared with prestorm values of up to 29%, due to the warmer air temperatures at night, while the inferred water vapor abundance suggests an increase during the storm. Between sols 2085 and 2130, the typical nighttime stable inversion layer was absent near the surface as ground temperatures remained warmer than near-surface air temperatures. Finally, the frequency domain behavior of the diurnal pressure cycle shows a strong increase in the strength of the semidiurnal and terdiurnal modes peaking after the local opacity maximum, also suggesting differences in the dust abundance inside and outside Gale.
机译:Rover环境监测站(REMS)仪器正在船上的美国航空航天局的火星科学实验室(MSL)好奇地揽胜。自2012年MSL着陆以来,REMS一直测量表面压力,空气和地面亮度温度,相对湿度和紫外线(UV)辐照症。在火星年(我的)34(2018)全球沙尘暴达到了L_S〜190 °。 REMS提供了一个独特的机会,可以更好地了解全球尘暴对当地环境条件的影响,这些条件补充了Viking Landers和Mars Exploration Rovers的先前观察。 REMS测量的所有大气变量都在不同时间受到强烈影响。在起始阶段期间,溶胶2075(不透明度〜1)和2085(不透明度〜8.5)之间的每日最终辐射降低90%。地面和空气温度的昼夜范围分别降低35和56 k,分别的〜2和4 k的昼夜平均降低。由于夜间温暖的空气温度较温暖的空气温度,在日出前发生的最大相对湿度降至5%以下,而在日出前达到5%,而较高的温度,而推断的水蒸汽丰度则表明风暴期间的增加表明增加。在溶胶2085和2130之间,在表面附近缺乏典型的夜间稳定反转层,因为地温度保持比近表面空气温度升温。最后,昼夜压力周期的频域行为显示出在局部透明度最大值之后的半衰老和特定模式强度的强度增加,这也表明大风内外灰尘丰富的差异。

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