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Precipitable Water Vapor: Considerations on the water vapor scale height, dry bias of the radiosonde humidity sensors, and spatial and temporal variability of the humidity field

机译:可降水的水蒸气:水蒸气水垢的考虑因素   高度,无线电探空仪湿度传感器的干燥偏压,以及空间和时间   湿度场的变化

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摘要

The Thirty Meter Telescope (TMT) and the European Extremely Large Telescope(E-ELT) site testing teams have recently finalized their site testing studies.Since atmospheric water vapor is the dominant source of absorption andincreased thermal background in the infrared, both projects includedprecipitable water vapor (PWV) measurements in their corresponding site testingcampaigns. TMT planned to monitor PWV at the sites of interest by means ofusing infrared radiometers. Technical failures and calibration issues preventedthem from having a sufficiently long PWV time-series to characterize the sitesusing this method. Therefore, for the sites in Chile TMT used surface watervapor density measurements, which taken together with an assumed water vaporscale height, allowed for the estimation of PWV. On the other hand, the E-ELTteam conducted dedicated PWV measurement campaigns at two of their observatorysites using radiosonde soundings to validate historical time-series of PWVreconstructed by way of a spectroscopic analysis of astronomical standardsources observed at the La Silla and the Paranal sites. The E-ELT alsoestimated the median PWV for the Armazones site from extrapolation of theirParanal statistics accounting for the difference in elevation between the twoplaces; and also from archival analysis of radiosonde data available from thecity of Antofagasta by integration of the humidity profile starting from 3000 maltitude. In the case of the Armazones site, the published median of PWV byboth groups differ by about 1 mm with the E-ELT values being drier than thoseestimated by the TMT group. This work looks at some of the reasons that couldexplain this difference, among them the water vapor scale height, thehorizontal variability of the water vapor field, and an unaccounted correctiondue to a dry bias known to affect the radiosondes relative humidity sensors.
机译:30米望远镜(TMT)和欧洲超大型望远镜(E-ELT)现场测试团队最近完成了现场测试研究。由于大气中的水蒸气是红外吸收的主要来源,并且红外的热本底增加,因此两个项目都包括可沉淀的水。蒸气(PWV)测量在其相应的现场测试活动中。 TMT计划通过使用红外辐射计监测感兴趣地点的PWV。技术故障和校准问题使他们无法使用足够长的PWV时间序列来使用此方法来表征站点。因此,对于智利TMT站点,使用地表水蒸气密度测量值以及假定的水蒸气水垢高度来估算PWV。另一方面,E-ELTteam使用探空探空仪在其两个观测站进行了专门的PWV测量活动,以通过对在La Silla和Paranal站点观测到的天文标准源进行光谱分析来验证重建的PWV的历史时间序列。 E-ELT还通过推算Armazones站点的Paranal统计数据来估算Armazones站点的中值PWV,这解释了两个地方之间的海拔差异。以及从安托法加斯塔市获得的无线电探空仪数据的档案分析中,从3000海拔开始的湿度廓线的积分。在Armazones站点的情况下,两组公布的PWV中值相差约1 mm,其中E-ELT值比TMT组估计的值更干燥。这项工作着眼于一些可能解释这种差异的原因,其中包括水蒸气水垢高度,水蒸气场的水平变化以及由于干偏见而造成的未知修正,这些偏见已知会影响无线电探空仪的相对湿度传感器。

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