Active layer thickness as a function of soil water content

Active layer thickness (ALT) is a critical metric for monitoring permafrost. How soil moisture influences ALT depends on two competing hypotheses: (a) increased soil moisture increases the latent heat of fusion for thaw, resulting in shallower active layers, and (b) increased soil moisture increases...

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Vydané v:	Environmental research letters Ročník 16; číslo 5; s. 55028 - 55036
Hlavní autori:	Clayton, Leah K, Schaefer, Kevin, Battaglia, Michael J, Bourgeau-Chavez, Laura, Chen, Jingyi, Chen, Richard H, Chen, Albert, Bakian-Dogaheh, Kazem, Grelik, Sarah, Jafarov, Elchin, Liu, Lin, Michaelides, Roger John, Moghaddam, Mahta, Parsekian, Andrew D, Rocha, Adrian V, Schaefer, Sean R, Sullivan, Taylor, Tabatabaeenejad, Alireza, Wang, Kang, Wilson, Cathy J, Zebker, Howard A, Zhang, Tingjun, Zhao, Yuhuan
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Bristol IOP Publishing 01.05.2021
Predmet:	active layer thickness Alaska Environmental monitoring ENVIRONMENTAL SCIENCES Heat Heat conductivity Heat of fusion Heat transfer Hypotheses Latent heat Moisture content Permafrost Soil conductivity Soil investigations Soil layers Soil moisture Soil temperature Soil water thaw depth Thermal conductivity Thickness Water content Canada United States > US Alaska
ISSN:	1748-9326, 1748-9326
On-line prístup:	Získať plný text
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