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Comparisons of spectrally resolved nightglow emission locally simulated with space and ground level observations

机译:用空间和地面观测局部模拟光谱分辨夜间发射的比较

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A mesospheric model of the airglow emission is developed to recover the night variations observed at ground level. The model is based on a 1D vertical photochemical model, including the photodissociation and heating processes. The spectral radiation is calculated at high altitude and propagated through the atmosphere to the ground. We also include short scale vertical dynamic such as turbulences and the molecular diffusion. Simulations reveal realistic emissions when compared with space observations. In addition, we estimate the impact of changes associated with parameterized atmospheric tides. The comparison with observations is performed over high altitude and ground level. We confront the model outputs at high altitude with satellite observations (SABER and GOMOS) and the simulations propagated at ground level are compared to local measurements campaigns performed in France and India. Biases between observed and simulated radiances and volume emission rates are suspected to be due to the impact of gravity waves or the large scale dynamic.
机译:开发了一种释放排放的伴奏模型,以回收在地面观察到的夜间变化。该模型基于1D垂直光化学模型,包括光沉积和加热过程。光谱辐射以高海拔计算并通过大气传播到地面。我们还包括短尺度垂直动态,如湍流和分子扩散。与空间观测相比,仿真揭示了现实的排放。此外,我们估计与参数化大气潮汐相关的变化的影响。与观察结果的比较在高海拔高度和地面上进行。我们面对具有卫星观测(Sabre和Gomos)的高海拔地区的模型输出,并将在地面上传播的模拟与法国和印度进行的局部测量活动进行比较。观察和模拟的辐射之间的偏差和体积排放率被怀疑是由于重力波或大规模动态的影响。

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