Abstract

Abstract. Records of Neoglacial glacier activity in the Arctic constructed from moraines are often incomplete due to a preservation bias toward the most extensive advance, often the Little Ice Age. Recent warming in the Arctic has caused extensive retreat of glaciers over the past several decades, exposing preserved landscapes complete with in situ tundra plants previously entombed by ice. The radiocarbon ages of these plants define the timing of snowline depression and glacier advance across the site, in response to local summer cooling. Erosion rapidly removes most dead plants that have been recently exposed by ice retreat, but where erosive processes are unusually weak, dead plants may remain preserved on the landscape for decades. In such settings, a transect of plant radiocarbon ages can be used to construct a near-continuous chronology of past ice margin advance. Here we present radiocarbon dates from the first such transect on Baffin Island, which directly dates the advance of a small ice cap over the past two millennia. The nature of ice expansion between 20 BCE and ∼ 1000 CE is still uncertain, but episodic advances at ∼ 1000 CE, ∼ 1200, and ∼ 1500 led to the maximum Neoglacial dimensions ~ 1900 CE. We employ a two-dimensional numerical glacier model calibrated using the plant radiocarbon ages ice margin chronology to assess the sensitivity of the ice cap to temperature change. Model experiments show that at least ∼ 0.44 °C of cooling over the past 2 kyr is required for the ice cap to reach its 1900 CE margin, and that the period from ∼ 1000 to 1900 CE must have been at least 0.25° C cooler than the previous millennium, results that agree with regional temperature reconstructions and climate model simulations. However, significant warming since 1900 CE is required to explain retreat to its present position, and, at the same rate of warming, the ice cap will disappear before 2100 CE.

Highlights

  • Summer insolation in the Northern Hemisphere has declined steadily through the Holocene, favoring cryosphere expansion, glaciers worldwide are currently losing mass (Stocker et al, 2013)

  • Model experiments show that at least ∼ 0.44 ◦C of cooling over the past 2 kyr is required for the ice cap to reach its 1900 CE margin, and that the period from ∼1000 to 1900 CE must have been at least 0.25◦ C cooler than the previous millennium, results that agree with regional temperature reconstructions and climate model simulations

  • We present a chronology of ice-margin advance from Divide Ice Cap, a small mountain ice cap in southeastern Baffin Island, derived from radiocarbondated dead plants, and utilize numerical modeling to estimate the changes in summer temperature required to reproduce the observed record of ice margin advance

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Summary

Introduction

Summer insolation in the Northern Hemisphere has declined steadily through the Holocene, favoring cryosphere expansion, glaciers worldwide are currently losing mass (Stocker et al, 2013). Since summer temperatures are the dominant control on glacier mass balance in the Canadian Arctic (Koerner, 2005), the reversal of late Holocene cooling (Kaufman et al, 2009) has caused recent retreat of ice caps and glaciers in the region. This continued shrinkage of the cryosphere reinforces the need for records of past glacier and climate change to provide context for contemporary warming. Moraines can be difficult to date precisely, and moraine records by nature are discontinuous

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