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Pan-Antarctic map of near-surface permafrost temperatures at 1 kmsup2/sup scale

机译:泛南极地图的近表面永久冻土温度为1 km 2 scale

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Permafrost is present within almost all of the Antarctic's ice-free areas, but little is known about spatial variations in permafrost temperatures except for a few areas with established ground temperature measurements. We modelled a temperature at the top of the permafrost (TTOP) for all the ice-free areas of the Antarctic mainland and Antarctic islands at 1 km2 resolution during 2000–2017. The model was driven by remotely sensed land surface temperatures and downscaled ERA-Interim climate reanalysis data, and subgrid permafrost variability was simulated by variable snow cover. The results were validated against in situ-measured ground temperatures from 40 permafrost boreholes, and the resulting root-mean-square error was 1.9 °C. The lowest near-surface permafrost temperature of ?36 °C was modelled at Mount Markham in the Queen Elizabeth Range in the Transantarctic Mountains. This is the lowest permafrost temperature on Earth, according to global-scale modelling results. The temperatures were most commonly modelled between ?23 and ?18 °C for mountainous areas rising above the Antarctic Ice Sheet and between ?14 and ?8 °C for coastal areas. The model performance was good where snow conditions were modelled realistically, but errors of up to 4 °C occurred at sites with strong wind-driven redistribution of snow.
机译:多年冻土以几乎所有的南极的无冰区存在,但除了具有建立的地温测量的几个区域之外,多年冻土温度的空间变化很少。我们在2000-2017期间,为南极大陆和南极岛的所有无冰区建模的温度建模了一个温度,为南极大陆和南极岛的所有无冰区。该模型由远程感测的土地表面温度和较低的ERA-临时气候再分析数据驱动,并通过可变雪盖模拟划分冻土变异性。结果验证了40多年冻土钻孔的原位测量的地温度,并得到的根平均方误差为1.9℃。在Transantarctic山脉的女王伊丽莎白范围内的Mount Markham近近近表面Pudafrost温度为36°C。根据全球规模的建模结果,这是地球上最低的PERMAFROST温度。温度最常见于南极冰板上方的山区23和18°C之间的最常用的山区和沿海地区的14°C和?8°C。模型性能是良好的,雪条件是现实建模的,但在具有强大风力驱动的雪的遗址上发生了最多4°C的误差。

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