// lecture 28 Flashcards
there are two ice sheets in the world:
- Greenland: 7 m sea level equivalent
- Antarctica: 61 m sea level equivalent
ice sheets gains
mass from snow on top and loses mass from melting and calving of icebergs.
- both loss and gain are increasing (increased precipitation at high latitudes).
- Greenland is losing mass though.
overall, ice sheet losses
are exceeding gains in Greenland. Also losses from calving have accelerated in the last 10 years.
Greenland is very big though -
it took tens of thousands of years to grow and at the current rates it would take many thousands of years to melt.
- now it’s contributing less than 10% of the sea level rise.
Could Greenland ice loss accelerate?
maybe because more melting causes larger melt ponds meltwater can fall through the cracks and make it to the bedrock below.
- water dripping through could cause it to stick to the bottom less and flow faster (moulin - hole in ice).
- still unclear how relevant this is in causing recent accelerations of calving.
A 2 C temp. rise would almost certainly
melt Greenland (eventually). this would likely take centuries though.
Currently, Greenland melting is a
small contribution to sea level rise. this is likely to become a larger percentage in the future though.
Antarctica has two giant
and many smaller, ice shelves.
ice shelves
float, but are connected to the sheet.
acceleration of melt has occurred in
w. antarctica recently. even more acceleration than in greenland.
glaciers along W. Antarctica’s Amundsen Sea would
raise sea levels by 1.2 m if they melted.
Antarctica has experienced relatively
small warming to this point, except the bits near South America.
- this was long ago forecast by climate models.
- strong jet stream keeps warmer air out of high latitudes.
- also ocean nearby takes up a lot of heat.
- no sea ice decrease has happened in Antarctica either. although, nearly all Antarctic sea ice melts each summer anyways.
East Antarctic is not
warming, but West Antarctic is warming.
Ice shelves reduce
calving by buttressing the ice.
Antarctica’s icy surfaces are
very cold, but warming in the surrounding ocean is a problem for the shelf base.
Ice shelf collapse can
then lead to acceleration of calving.