在菲尔德斯半岛,乔治王岛 - 海上南极洲的地面温度趋势和活性层动态
Tamíres P Correia1,2, Marcio R Francelino3, Gustavo V Veloso3
1Federal Rural University of Rio de Janeiro, Department of Environmental Sciences, Km 07, Zona Rural, BR-465, 23890-000 Seropédica, RJ, Brazil.
Anais da Academia Brasileira de Ciencias
|July 31, 2024
概括
南极洲的地面温度监测显示了夏季显著的变暖趋势和与空气温度的积极相关性. 平均活性层厚度为92.61厘米,突出显示了温度.
科学领域:
- 地质科学 地质科学
- 气候科学 气候科学
- 永久土研究 永久土研究
背景情况:
- 土壤温度动态是气候变化影响的关键指标.
- 了解永久土的热态对于极地研究至关重要.
- 南极永久土对全球气温上升很敏感.
研究的目的:
- 为了监测和分析Fildes半岛,南极洲的地面温度的时间趋势.
- 估计活动层厚度 (ALT) 和它与空气温度的关系.
- 评估气候变化对南极永久土的影响.
主要方法:
- 数据质量控制和一致性分析.
- 统计方法的应用:序列自相关,曼-肯达尔,森-斯洛普,佩蒂特和回归分析.
- 斯皮尔曼的相关性将空气温度和地面深度联系起来;使用最大月度温度估计ALT.
主要成果:
- 在特定深度 (67.5和83.5厘米) 的地面温度中观察到显著的积极夏季季节趋势.
- 空气温度和地表地面深度之间存在强烈的正相关性 (r=0.82).
- 平均活动层厚度 (ALT) 测量为92.61厘米;从2008年至2018年,结条件持续存在.
结论:
- 南极洲的地面温度对气候变化敏感,显示出显著的变暖趋势.
- 活性层厚度受到空气温度的直接影响,这凸显了永久土对变暖的反应.
- 准确的地面温度监测和估计对于了解极地地区气候变化影响至关重要.
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