Active layer and permafrost thermal regime in a patterned ground soil in Maritime Antarctica, and relationship with climate variability models

作者：Chaves D A; Lyra G B; Francelino M R; Silva L D B; Thomazini A^*; Schaefer C E G R

来源：Science of the Total Environment, 2017, 584: 572-585.

DOI：10.1016/j.scitotenv.2017.01.077

• Antarctic oscillation mode (AAO)
• Southern oscillation mode (SOI)
• Polygonal soils
• Climate variability
• Soil thermal regime
• Cryosols

Permafrost and active layer studies are important to understand and predict regional climate changes. The objectives of this work were: i) to characterize the soil thermal regime (active layer thickness and permafrost formation) and its interannual variability and ii) to evaluate the influence of different climate variability modes to the observed soil thermal regime in a patterned ground soil in Maritime Antarctica. The study was carried out at Keller Peninsula, King George Island, Marititne Antarctica. Six soil temperatures probes were installed at different depths (10, 30 and 80 cm) in the polygon center (Tc) and border (Tb) of a patterned ground soil. We applied cross-correlation analysis and standardized series were related to the Antarctic Oscillation Index (MO). The estimated active layer thickness was approximately 0.75 cm in the polygon border and 0.64 cm in the center, indicating the presence of permafrost (within 80 cm). Results indicate that summer and winter temperatures are becoming colder and warmer, respectively. Considering similar active layer thickness, the polygon border presented greater thawing days, resulting in greater vulnerability to warming, cooling faster than the center, due to its lower volumetric heat capacity (Cs). Cross-correlation analysis indicated statistically significant delay of 1 day (at 10 cm depth) in the polygon center, and 5 days (at 80 cm depth) for the thermal response between atmosphere and soil. Air temperature showed a delay of 5 months with the climate variability models. The influence of southern winds from high latitudes, in the south facing slopes, favored freeze in the upper soil layers, and also contributed to keep permafrost closer to the surface. The observed cooling trend is linked to the regional climate variability modes influenced by atmospheric circulation, although longer monitoring period is required to reach a more precise scenario.

• 出版日期2017-4-15