Ground temperature trend and active layer dynamics in the Fildes Peninsula, King George Island - Marine Antarctica.

• Published in: Anais da Academia Brasileira de Ciências
• Main Authors: Correia, Tamíres P, Francelino, Marcio R, Veloso, Gustavo V, Michel, Roberto F, Schaefer, Carlos Ernesto, Fernandes Filho, Elpídio Inácio, Justino, Flávio B, Lyra, Gustavo B
• Format: Article in Journal/Newspaper
• Language: English
• Published: Scientific Electronic Library Online 2024
• Subjects: Active layer thickness; Antarc*; Antarctica; King George Island; permafrost
• Online Access: https://doi.org/10.1590/0001-3765202420230743; https://pubmed.ncbi.nlm.nih.gov/39082479

Ground temperature's sensitivity to climate change has garnered attention. This study aimed to monitor and analyze temporal trends and estimate Active Layer Thickness from a monitoring point at Fildes Peninsula, King George Island, in Antarctica. Quality control and consistency analysis were performed on the data. Methods such as serial autocorrelation, Mann-Kendall, Sen-Slope, Pettitt, and regression analysis tests were applied. Spearman's correlation examined the relationship between air temperature and ground depths. The active layer thickness was estimated using the maximum monthly temperature, and the permafrost lower limit used the minimum monthly temperature. Significant summer seasonal trends were observed with Mann-Kendall tau, positive Sen-Slope, and Pettitt slope at depths of 67.5 and 83.5 cm. The regression analysis was significant and positive for all ground depths and in different seasons. The highest correlation (r=0.82) between air temperature and surface ground depth was found. Freezing prevailed at all depths during 2008-2018. The average Active Layer Thickness (ALT) was 92.61 cm. Temperature is difficult to monitor, and its estimation is still complex. However, it stands out as a fundamental element for studies that refer to the impacts of climate change.