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首页> 外文期刊>Icarus: International Journal of Solar System Studies >In search of water vapor on Jupiter: Laboratory measurements of the microwave properties of water vapor under simulated jovian conditions
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In search of water vapor on Jupiter: Laboratory measurements of the microwave properties of water vapor under simulated jovian conditions

机译:在木星上寻找水蒸气:模拟木星条件下水蒸气微波特性的实验室测量

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Detection and measurement of atmospheric water vapor in the deep jovian atmosphere using microwave radiometry has been discussed extensively by Janssen et al. (Janssen, M.A., Hofstadter, M.D., Gulkis, S., Ingersoll, A.P., Allison, M., Bolton, S.J., Levin, S.M., Kamp, L.W. [2005]. Icarus 173 (2), 447-453.) and de Pater et al. (de Pater, I., Deboer, D., Marley, M., Freedman, R., Young, R. [2005]. Icarus 173 (2), 425-447). The NASA Juno mission will include a six-channel microwave radiometer system (MWR) operating in the 1.3-50cm wavelength range in order to retrieve water vapor abundances from the microwave signature of Jupiter (see, e.g., Matousek, S. [2005]. The Juno new frontiers mission. Tech. Rep. IAC-05-A3.2.A.04, California Institute of Technology). In order to accurately interpret data from such observations, nearly 2000 laboratory measurements of the microwave opacity of H_2O vapor in a H_2/He atmosphere have been conducted in the 5-21cm wavelength range (1.4-6GHz) at pressures from 30 mbars to 101 bars and at temperatures from 330 to 525K. The mole fraction of H_2O (at maximum pressure) ranged from 0.19% to 3.6% with some additional measurements of pure H_2O. These results have enabled development of the first model for the opacity of gaseous H_2O in a H2/He atmosphere under jovian conditions developed from actual laboratory data. The new model is based on a terrestrial model of Rosenkranz et al. (Rosenkranz, P.W. [1998]. Radio Science 33, 919-928), with substantial modifications to reflect the effects of jovian conditions. The new model for water vapor opacity dramatically outperforms previous models and will provide reliable results for temperatures from 300 to 525K, at pressures up to 100 bars and at frequencies up to 6GHz. These results will significantly reduce the uncertainties in the retrieval of jovian atmospheric water vapor abundances from the microwave radiometric measurements from the upcoming NASA Juno mission, as well as provide a clearer understanding of the role deep atmospheric water vapor may play in the decimeter-wavelength spectrum of Saturn.
机译:Janssen等人已广泛讨论了使用微波辐射测定法在深木星大气中检测和测量大气中的水蒸气。 (Janssen,MA,Hofstadter,MD,Gulkis,S.,Ingersoll,AP,Allison,M.,Bolton,SJ,Levin,SM,Kamp,LW [2005]。Icarus 173(2),447-453。)和de Pater等。 (de Pater,I.,Deboer,D.,Marley,M.,Freedman,R.,Young,R。[2005]。Icarus173(2),425-447)。 NASA Juno任务将包括一个在1.3-50cm波长范围内运行的六通道微波辐射计系统(MWR),以便从木星的微波特征中检索水蒸气的丰度(例如,参见Matousek,S. [2005]。 Juno的新边疆任务(技术代表,IAC-05-A3.2.A.04,加利福尼亚理工学院)。为了准确地解释来自这些观察的数据,已经在5-21cm波长范围(1.4-6GHz)中,在30毫巴至101巴的压力下,对H_2 / He气氛中H_2O蒸气的微波不透明度进行了近2000次实验室测量。温度在330至525K之间。 H_2O的摩尔分数(在最大压力下)范围为0.19%至3.6%,还需要另外一些纯H_2O的测量值。这些结果使得能够开发出第一个模型,该模型根据实际实验室数据开发了在木马条件下在H2 / He气氛中气态H_2O的不透明性。新模型基于Rosenkranz等人的地面模型。 (Rosenkranz,P.W. [1998]。Radio Science 33,919-928),进行了实质性修改以反映木马条件的影响。新的水蒸气不透明度模型大大优于以前的模型,在300至525K的温度,高达100 bar的压力和高达6GHz的频率下,将提供可靠的结果。这些结果将大大减少即将到来的NASA Juno任务进行微波辐射测量获得的木柴大气中水汽丰度的不确定性,并使人们更清楚地了解深层大气水汽在分米波长光谱中的作用。土星

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