The Independent writes on the intensification of melting on the Antarctic peninsula. Last year's melt season was the highest in forty years of satellite records.
Antarctica’s Larsen C Ice Shelf experienced its highest rate of melting since records began 40 years ago from 2019-2020, a new study has found.
The unprecedented melt at Larsen C, which is Antarctica’s fourth-largest ice shelf, coincided with record-breaking summer temperatures at a weather station in the Antarctic Peninsula, the research says.
The melting was primarily driven by a series of rare weather events that brought additional heat towards the ice shelf, causing it to melt from above, the study says.
The effects of such meteorological events can combine with human-caused global heating to create a “perfect storm” for Antarctica’s ice shelves, a climate scientist told The Independent.
In mid-November, about a month before the start of summer in the southern hemisphere, the Antarctic melting season is usually just starting. By that time this year, vast areas along the Antarctic Peninsula were already painted blue with meltwater.
By the end of November 2020, much of the meltwater on the ice had refrozen. But scientists want to know if this event was similar to a strong early season melt that launched the 2019-2020 melt season. Last year, unusually warm air and water led to record-breaking melting across the Larsen C Ice Shelf. It is the largest remaining ice shelf along the Antarctic Peninsula, even though it lost a Delaware-sized iceberg in 2017.
Widespread melting on Larsen C, located just south of this image, was not apparent in natural-color satellite images. But scientists are watching how this season progresses. The ice shelf surface on the Larsen A was full of ponded meltwater just before its complete collapse in 1995; the same thing occurred before the near-complete collapse of Larsen B in 2002.
Surface melt and ponding on Antarctic Peninsula (AP) ice shelves has been linked to firn densification (Holland et al., 2011), surface lowering (Paolo et al., 2015), hydrofracture (Banwell et al., 2013), and eventual collapse (Scambos et al., 2000; van den Broeke, 2005). Following collapse the glaciers that feed the ice shelves have been observed to speed up (Gudmundsson, 2013), discharging more land ice to the oceans and increasing the rate of sea-level rise. Larsen C Ice Shelf (LCIS, Fig. 1) is the largest remaining ice shelf on the AP, and surface melt and ponding have led to surface lowering, concentrated in the inlets and the northern parts of the shelf, and to the formation of a large subsurface mass of ice (Hubbard et al., 2016). If LCIS were to disintegrate, in the same way as Prince Gustav and Larsen A ice shelves in 1995 (Rott et al., 1996) and Larsen B ice shelf in 2002 (Rott et al., 2002), modelling studies suggest that the dynamic response of the inland ice might be limited owing to the small amount of buttressing generated by LCIS (Furst et al., 2016). The potential sea-level contribution might only be of the order of millimetres over the next two centuries (Schannwell et al., 2018). However, removal of ice shelves has consequences other than sea-level rise with potential impacts on ocean circulation and biodiversity (Siegert et al., 2019).
Iceberg A68 was twelve percent of the marine extension of land ice on the Antarctic Peninsula before the calving from the Larsen C ice shelf in 2017. The iceberg will reach the South Atlantic islands of S Sandwich and South Georgia, also known as the iceberg graveyard, within a couple of weeks.