An Explainable Deep-learning Model of Proton Auroras on Mars

IF 3.8 Q2 ASTRONOMY & ASTROPHYSICS The Planetary Science Journal Pub Date : 2024-06-10 DOI:10.3847/psj/ad45ff
Dattaraj B. Dhuri, Dimitra Atri, Ahmed AlHantoobi
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Abstract

Proton auroras are widely observed on the dayside of Mars, identified as a significant intensity enhancement in the hydrogen Lyα (121.6 nm) emission at altitudes of ∼110 and 150 km. Solar wind protons penetrating as energetic neutral atoms into Mars’ thermosphere are thought to be primarily responsible for these auroras. Recent observations of spatially localized “patchy” proton auroras suggest a possible direct deposition of protons into Mars’ atmosphere during unstable solar wind conditions. Improving our understanding of proton auroras is therefore important for characterizing the interaction of the solar wind with Mars’ atmosphere. Here, we develop a first purely data-driven model of proton auroras using Mars Atmosphere and Volatile Evolution (MAVEN) in situ observations and limb scans of Lyα emissions between 2014 and 2022. We train an artificial neural network that reproduces individual Lyα intensities and relative Lyα peak intensity enhancements with Pearson correlations of ∼94% and ∼60% respectively for the test data, along with a faithful reconstruction of the shape of the observed altitude profiles of Lyα emission. By performing a Shapley Additive Explanations (SHAP) analysis, we find that solar zenith angle, solar longitude, CO2 atmosphere variability, solar wind speed, and temperature are the most important features for the modeled Lyα peak intensity enhancements. Additionally, we find that the modeled peak intensity enhancements are high for early local-time hours, particularly near polar latitudes, and the induced magnetic fields are weaker. Through SHAP analysis, we also identify the influence of biases in the training data and interdependences between the measurements used for the modeling, and an improvement of those aspects can significantly improve the performance and applicability of the ANN model.
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火星质子极光的可解释深度学习模型
质子极光在火星日侧被广泛观测到,被确定为氢 Lyα(121.6 nm)发射在 110 至 150 千米高度的显著增强。太阳风质子作为高能中性原子穿透火星热层被认为是这些极光的主要原因。最近对空间局部 "斑块状 "质子极光的观测表明,在不稳定的太阳风条件下,质子可能直接沉积到火星大气中。因此,加深对质子极光的了解对于描述太阳风与火星大气的相互作用非常重要。在这里,我们利用火星大气与挥发演化(MAVEN)在2014年至2022年期间的原位观测数据和Lyα发射的边缘扫描数据,首次建立了一个纯数据驱动的质子极光模型。我们训练了一个人工神经网络,该网络可以再现单个 Lyα 强度和相对 Lyα 峰强度增强,与测试数据的皮尔逊相关性分别为 ∼94% 和 ∼60%,并忠实地重建了观测到的 Lyα 辐射高度剖面的形状。通过 Shapley Additive Explanations(SHAP)分析,我们发现太阳天顶角、太阳经度、CO2 大气变率、太阳风速和温度是模拟 Lyα 峰值强度增强的最重要特征。此外,我们还发现,建模的峰值强度增强在当地时间早期较高,尤其是在极地纬度附近,而且诱导磁场较弱。通过 SHAP 分析,我们还发现了训练数据中偏差的影响以及建模所用测量数据之间的相互依赖关系,这些方面的改进可以显著提高 ANN 模型的性能和适用性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
The Planetary Science Journal
The Planetary Science Journal Earth and Planetary Sciences-Geophysics
CiteScore
5.20
自引率
0.00%
发文量
249
审稿时长
15 weeks
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