论文标题

从X射手和Saber观察的各种OH线的有效排放高度对过去的准2天波

Effective Emission Heights of Various OH Lines From X-shooter and SABER Observations of a Passing Quasi-2-Day Wave

论文作者

Noll, Stefan, Schmidt, Carsten, Kausch, Wolfgang, Bittner, Michael, Kimeswenger, Stefan

论文摘要

振动和旋转激发的OH激发的化学发光辐射在较宽的波长区域中占主导地球大气的近红外发射,是80至100 km之间中间区域的化学和动力学状态的重要示踪剂。由于辐射寿命和碰撞相关过渡的速率系数取决于OH能级,因此预计线相关的发射曲线。但是,除了主要基于卫星的测量结果揭示的整个频段的某些高度差异外,缺乏单个线的数据。由于在2017年的八个晚上共同观察了强烈的准2天波(Q2DW)的共同观察,我们成功地推导了有效的排放高度,并在Chile的Cerro Paranal的非常大的望远镜的中等分辨率光谱X射击器上,在CHILE的中等分辨率光谱X射击器上,并在尖锐的Saber Saber射线仪上对较大的Saber射线表进行了验证。我们的拟合程序显示了一个大约44小时的单个波的最具说服力结果,垂直波长约为32 km。然后,Q2DW的线依赖性和高度分辨阶段导致有效高度,其高度差异高达8 km,并且随着振动和旋转激发的增加而增加。测量的发射高度和波幅度的依赖性(午夜之后最强)对线参数的依赖性意味着每个振动水平的冷热和热量非热量群体的存在。

Chemiluminescent radiation of the vibrationally and rotationally excited OH radical, which dominates the nighttime near-infrared emission of the Earth's atmosphere in wide wavelength regions, is an important tracer of the chemical and dynamical state of the mesopause region between 80 and 100 km. As radiative lifetimes and rate coefficients for collision-related transitions depend on the OH energy level, line-dependent emission profiles are expected. However, except for some height differences for whole bands mostly revealed by satellite-based measurements, there is a lack of data for individual lines. We succeeded in deriving effective emission heights for 298 OH lines thanks to the joint observation of a strong quasi-2-day wave (Q2DW) in eight nights in 2017 with the medium-resolution spectrograph X-shooter at the Very Large Telescope at Cerro Paranal in Chile and the limb-sounding SABER radiometer on the TIMED satellite. Our fitting procedure revealed the most convincing results for a single wave with a period of about 44 h and a vertical wavelength of about 32 km. The line-dependent as well as altitude-resolved phases of the Q2DW then resulted in effective heights which differ by up to 8 km and tend to increase with increasing vibrational and rotational excitation. The measured dependence of emission heights and wave amplitudes (which were strongest after midnight) on the line parameters implies the presence of a cold thermalized and a hot non-thermalized population for each vibrational level.

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