Long term active layer monitoring at a warm-based glacier front from maritime Antarctica

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• 作者：Ivan C.C. Almeida^a ; ^{ivancarreiro@yahoo.com.br} ; Carlos E.G.R. Schaefer^b ; ^{carlos.schaefer@ufv.br} ; Roberto F.M. Michel^c ; ^{roberto@michel.com} ; Raphael B.A. Fernandes^b ; ^{raphael@ufv.br} ; Thiago T.C. Pereira^d ; ^{thiago.pereira@uemg.br} ; André ; M. de Andrade^e ; ^{andre.medeiros@ufvjm.edu.br} ; Marcio R. Francelino^b ; ^{marcio.francelino@ufv.br} ; Elpidio I. Fernandes Filho^b ; ^{elpidio@ufv.br} ; James G. Bockheim^f ; ^{bockheim@wisc.edu}
• 关键词：Soil thermal regime ; Climate change ; Cryosol ; Permafrost ; Periglacial regime
• 刊名：CATENA
• 出版年：2017
• 出版时间：February 2017
• 年：2017
• 卷：149
• 期：part_P2
• 页码：572-581
• 全文大小：2308 K
• 卷排序：149

文摘

This paper analyses the long-term soil thermal regime of a paraglacial site. The TD, FD, number of ID, number of FTD, TDD, FDD, and the ATD were calculated. Most soil temperature readings were close to 0 °C, especially near permafrost table. ALT regime at LH is similar of periglacial environments from M. Antarctica.