A multiannual ground temperature dataset covering sixteen high elevation sites (3493–4377 m a.s.l.) in the Bale Mountains, Ethiopia

A. Groos, Janik Niederhauser, B. Lemma, Mekbib Fekadu, W. Zech, Falk Hänsel, Luise Wraase, N. Akçar, H. Veit
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Abstract

Abstract. Tropical mountains and highlands in Africa are under pressure because of anthropogenic climate and land-use change. To determine the impacts of global climate change on the afro-alpine environment and to assess the potential socio-economic consequences, the monitoring of essential climate and environmental variables at high elevation is fundamental. However, long-term climate observations on the continent above 3,000 m are very rare. Here we present a consistent multinannual ground temperature dataset for the BaleMountains in the southern Ethiopian Highlands, which comprise Africa's largest tropical alpine area. 29 ground temperature data loggers have been installed at 16 sites since 2017 to characterise and continuously monitor the mountain climate and ecosystem of the Bale Mountains along an elevation gradient from 3493 to 4377 m. At five sites above ∼ 3900 m, the monitoring will be continued to trace long-term changes. The generated time series provide insights in the spatio temporal ground temperature variations at high elevation, the energy exchange between the ground surface and atmosphere, as well as the impact of vegetation and slope orientation on the thermal dynamics of the ground. To promote the further use of the ground temperature dataset by the wider research community dealing with the climate and geo-ecology of tropical mountains in Eastern Africa, it is made freely available via the open-access repository Zenodo: https://doi.org/10.5281/zenodo.5172002 (Groos et al., 2021b).
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覆盖埃塞俄比亚贝尔山脉16个高海拔站点(海拔3493-4377 m)的多年地温数据集
摘要由于人为气候和土地利用变化,非洲的热带山地和高地正面临压力。为了确定全球气候变化对非洲-高山环境的影响并评估其潜在的社会经济后果,对高海拔地区基本气候和环境变量的监测至关重要。然而,在海拔3000米以上的大陆上进行长期气候观测是非常罕见的。在这里,我们提供了埃塞俄比亚南部高原balemmountains多年来一致的地温数据集,该数据集包括非洲最大的热带高山地区。自2017年以来,已在16个地点安装了29台地温数据记录器,以描述和持续监测贝尔山脉海拔梯度从3493米至4377米的山地气候和生态系统。在海拔约3900米以上的5个地点,将继续监测长期变化。生成的时间序列可以揭示高海拔地温的时空变化、地表与大气之间的能量交换以及植被和坡向对地面热动力学的影响。为了促进研究东非热带山区气候和地质生态的更广泛的研究界进一步使用地温数据集,该数据集通过开放存取库Zenodo: https://doi.org/10.5281/zenodo.5172002免费提供(Groos et al., 2021b)。
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