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The distribution and dynamics of aufeis in permafrost regions. / Ensom, T.; MARSH , P.; Makarieva, O.; ALEKSEEV, V.; MORSE, P.; KANE , D.

In: Permafrost and Periglacial Processes, Vol. 31, No. 3, 2020, p. 383-395.

Research output: Contribution to journalArticlepeer-review

Harvard

Ensom, T, MARSH , P, Makarieva, O, ALEKSEEV, V, MORSE, P & KANE , D 2020, 'The distribution and dynamics of aufeis in permafrost regions.', Permafrost and Periglacial Processes, vol. 31, no. 3, pp. 383-395. https://doi.org/10.1002/ppp.2051

APA

Ensom, T., MARSH , P., Makarieva, O., ALEKSEEV, V., MORSE, P., & KANE , D. (2020). The distribution and dynamics of aufeis in permafrost regions. Permafrost and Periglacial Processes, 31(3), 383-395. https://doi.org/10.1002/ppp.2051

Vancouver

Ensom T, MARSH P, Makarieva O, ALEKSEEV V, MORSE P, KANE D. The distribution and dynamics of aufeis in permafrost regions. Permafrost and Periglacial Processes. 2020;31(3):383-395. https://doi.org/10.1002/ppp.2051

Author

Ensom, T. ; MARSH , P. ; Makarieva, O. ; ALEKSEEV, V. ; MORSE, P. ; KANE , D. / The distribution and dynamics of aufeis in permafrost regions. In: Permafrost and Periglacial Processes. 2020 ; Vol. 31, No. 3. pp. 383-395.

BibTeX

@article{5bf2955738c344699b7c366c2aa80fe3,
title = "The distribution and dynamics of aufeis in permafrost regions.",
abstract = "Aufeis, also known as an icing or naled, is an accumulation of ice that forms primarily during winter when water is expelled onto frozen ground or ice surfaces and freezes in layers. Process-oriented aufeis research initially expanded in the 20th century, but recent interest in changing hydrological conditions in permafrost regions has rejuvenated this field. Despite its societal relevance, the controls on aufeis distribution and dynamics are not well defined and this impedes projections of variation in aufeis size and distribution expected to accompany climate change. This paper reviews the physical controls on aufeis development, current broad-scale aufeis distribution and anticipated change, and approaches to aufeis investigation. We propose an adjustment to terminology to better distinguish between the formation process and resulting ice bodies, a clarification of the aufeis classification approach based on source water, and a size threshold for broad-scale aufeis inventory to facilitate collab",
author = "T. Ensom and P. MARSH and O. Makarieva and V. ALEKSEEV and P. MORSE and D. KANE",
year = "2020",
doi = "10.1002/ppp.2051",
language = "English",
volume = "31",
pages = "383--395",
journal = "Permafrost and Periglacial Processes",
issn = "1045-6740",
publisher = "Wiley-Blackwell",
number = "3",

}

RIS

TY - JOUR

T1 - The distribution and dynamics of aufeis in permafrost regions.

AU - Ensom, T.

AU - MARSH , P.

AU - Makarieva, O.

AU - ALEKSEEV, V.

AU - MORSE, P.

AU - KANE , D.

PY - 2020

Y1 - 2020

N2 - Aufeis, also known as an icing or naled, is an accumulation of ice that forms primarily during winter when water is expelled onto frozen ground or ice surfaces and freezes in layers. Process-oriented aufeis research initially expanded in the 20th century, but recent interest in changing hydrological conditions in permafrost regions has rejuvenated this field. Despite its societal relevance, the controls on aufeis distribution and dynamics are not well defined and this impedes projections of variation in aufeis size and distribution expected to accompany climate change. This paper reviews the physical controls on aufeis development, current broad-scale aufeis distribution and anticipated change, and approaches to aufeis investigation. We propose an adjustment to terminology to better distinguish between the formation process and resulting ice bodies, a clarification of the aufeis classification approach based on source water, and a size threshold for broad-scale aufeis inventory to facilitate collab

AB - Aufeis, also known as an icing or naled, is an accumulation of ice that forms primarily during winter when water is expelled onto frozen ground or ice surfaces and freezes in layers. Process-oriented aufeis research initially expanded in the 20th century, but recent interest in changing hydrological conditions in permafrost regions has rejuvenated this field. Despite its societal relevance, the controls on aufeis distribution and dynamics are not well defined and this impedes projections of variation in aufeis size and distribution expected to accompany climate change. This paper reviews the physical controls on aufeis development, current broad-scale aufeis distribution and anticipated change, and approaches to aufeis investigation. We propose an adjustment to terminology to better distinguish between the formation process and resulting ice bodies, a clarification of the aufeis classification approach based on source water, and a size threshold for broad-scale aufeis inventory to facilitate collab

U2 - 10.1002/ppp.2051

DO - 10.1002/ppp.2051

M3 - Article

VL - 31

SP - 383

EP - 395

JO - Permafrost and Periglacial Processes

JF - Permafrost and Periglacial Processes

SN - 1045-6740

IS - 3

ER -

ID: 78390339