Mary_kerr_2018BiologySeminar.pdf (1.18 MB)
The effects of increased ground moisture on permafrost sustainability
journal contribution
posted on 2018-04-21, 03:36 authored by Mary Kerr, Pascale Roy-léveilléePascale Roy-léveilléeKerr, M., Roy-Leveillee, P. 2018. The effects of increased ground moisture on permafrost sustainability. 2018 Biology Graduate Seminar at Laurentian University, April 2018, Sudbury, ON. doi:10.6084/m9.figshare.6167927
Early
stages of permafrost degradation and thermokarst development in Arctic and
subarctic lowlands are often characterized by increased soil moisture due to
thawing ground ice. In the field, increased soil moisture has been linked to two
contradictory effects on ground temperatures: a cooling effect due to the high
thermal conductivity of ice compared to water, and a warming effect due to the latent
heat of ground moisture slowing ground-frost penetration in early winter. However,
the factors controlling which effect will dominate at a given site, and whether
increased soil moisture will facilitate or inhibit further permafrost degradation
remain unclear. This research investigates the response of increased soil
moisture on permafrost temperatures under different climatic conditions using numerical
modelling and field data. It aims to identify the conditions under which
increasing soil moisture transitions from having a ground cooling effect to
having a warming effect that may facilitate continuous thermokarst development. A one-dimensional, heat conduction numerical
model will be used to predict active layer depth and mean annual temperature at
the top of permafrost based on air temperature, snow pack development, and
ground thermal properties. The model will be calibrated with field data from
monitoring stations located in peatlands of the
discontinuous and continuous permafrost zones in three latitudinal
gradients of Northern Canada. This will allow us to examine the effects of
current increasing ground moisture, snow cover and air temperature. This research aims to improve the
understanding of positive and negative feedback cycles that contribute to
permafrost degradation during the early stages of thermokarst development
and provide new insights into the timeline of these events. Knowledge of thermokarst
development will better inform future restoration and adaptive management
practices in response to climate change.