Modelling the late Holocene and future evolution of Monacobreen, northern Spitsbergen

Abstract

Monacobreen is a 40 km long surge-type tidewater glacier in northern Spitsbergen. During 1991During -1997 Monacobreen surged and advanced by about 2 km, but the front did not reach the maximum Little Ice Age (LIA) stand. Since 1997 the glacier front is retreating at a fast rate ( ∼ 125 m a −1 ). The questions addressed in this study are as follows: (1) Can the late Holocene behaviour of Monacobreen be understood in terms of climatic forcing?, and (2) What will be the likely evolution of this glacier for different scenarios of future climate change?Monacobreen is modelled with a minimal glacier model, including a parameterization of the calving process as well as the effect of surges. The model is driven by an equilibriumline altitude (ELA) history derived from lake sediments of a nearby glacier catchment in combination with meteorological data from 1899 onwards. The simulated glacier length is in good agreement with the observations: the maximum LIA stand, the front position at the end of the surge, and the 2.5 km retreat after the surge (1997)(1998)(1999)(2000)(2001)(2002)(2003)(2004)(2005)(2006)(2007)(2008)(2009)(2010)(2011)(2012)(2013)(2014)(2015)(2016) are well reproduced (the mean difference between observed and simulated glacier length being 6 % when scaled with the total retreat during 1900-2016). The effect of surging is limited. Directly after a surge the initiated mass balance perturbation due to a lower mean surface elevation is about −0.13 m w.e. a −1 , which only has a small effect on the longterm evolution of the glacier. The simulation suggests that the major growth of Monacobreen after the Holocene climatic optimum started around 1500 BCE. Monacobreen became a tidewater glacier around 500 BCE and reached a size comparable to the present state around 500 CE. For the mid-B2 scenario (IPCC, 2013), which corresponds to a ∼ 2 m a −1 rise of the ELA, the model predicts a volume loss of 20 % to 30 % by the year 2100 (relative to the 2017 volume). For a ∼ 4 m a −1 rise in the ELA this is 30 % to 40 %. However, much of the response to 21st century warming will still come after 2100.

Modelling the mass budget and future evolution of Tunabreen, central Spitsbergen

“…Although a surge initiates a negative perturbation of the mass budget for some years and reduces the glacier volume slightly, this apparently has no lasting effect. The same conclusion was reached in earlier studies of Abrahamsenbreen (Oerlemans and van Pelt, 2015) and Monacobreen (Oerlemans, 2018), and it probably applies to most long glaciers on Svalbard. However, with respect to ice caps that have surging parts (like Austfonna), the situation may be different.…”

“…However, the most important mechanical effect, namely that glaciers are thicker when they are longer and/or rest on a bed with a smaller slope, should always be accounted for. We note that the model version em-ployed here is similar to the one used in a study of Monacobreen in northern Spitsbergen (Oerlemans, 2018).…”

On the Imbalance and Response Time of Glaciers in the European Alps

“…The glacier response time from numerical experiments can be expressed through an e‐folding timescale, in which the response time corresponds to the time needed to complete 1 − e −1 (= 63.2%) of the total change (e.g., Leysinger Vieli & Gudmundsson, ; Oerlemans, ). For the committed experiments (Figure ), the above approach results in response times decreasing from 42 years in 2001 to 33 years in 2018 (Figure S5).…”