Remote Sensing Mass Loss of Ice Sheet Outlet Glaciers: Comparing Greenland and Antarctic Outlet Glaciers
Conference Year
January 2021
Abstract
The world’s ice sheets hold 69% of the world’s freshwater, and polar regions are warming at an accelerated rate threatening sea level rise that will affect millions over the 21st century. According to the 2019 International Panel on Climate Change, combined ice sheet mass loss is around 450 gigatons per year, increased from previous decades. Therefore, it is crucial to accurately track ice mass loss, and refine the errors within these studies to understand the rates at which climate change will affect sea level rise. High spatial and temporal resolution satellite imagery has enabled large scale projects analyzing glacier flow and mass balance. Patterns emerged, such as a 2020 finding of consistent retreat of Greenland outlet glaciers based upon normalized discharge values, unlike in Antarctica where ice shelves buttress the flow of ice. This project measures the ice discharge in the Larson B embayment, Antarctica, where a buttressing ice shelf collapsed near the turn of the century. By incorporating Landsat ice velocity measurements, subglacial topography, and satellite laser altimetry across multiple platforms, ice flux from the primary tidewater glaciers of the Larsen B embayment are compared with published analysis of Greenland tidewater glaciers at approximately the same latitudes. This yields insight onto the main controls of non-buttressed ice sheet glacial retreat.
Primary Faculty Mentor Name
Dr. Keith Klepeis
Status
Undergraduate
Student College
College of Arts and Sciences
Program/Major
Geology
Primary Research Category
Engineering & Physical Sciences
Remote Sensing Mass Loss of Ice Sheet Outlet Glaciers: Comparing Greenland and Antarctic Outlet Glaciers
The world’s ice sheets hold 69% of the world’s freshwater, and polar regions are warming at an accelerated rate threatening sea level rise that will affect millions over the 21st century. According to the 2019 International Panel on Climate Change, combined ice sheet mass loss is around 450 gigatons per year, increased from previous decades. Therefore, it is crucial to accurately track ice mass loss, and refine the errors within these studies to understand the rates at which climate change will affect sea level rise. High spatial and temporal resolution satellite imagery has enabled large scale projects analyzing glacier flow and mass balance. Patterns emerged, such as a 2020 finding of consistent retreat of Greenland outlet glaciers based upon normalized discharge values, unlike in Antarctica where ice shelves buttress the flow of ice. This project measures the ice discharge in the Larson B embayment, Antarctica, where a buttressing ice shelf collapsed near the turn of the century. By incorporating Landsat ice velocity measurements, subglacial topography, and satellite laser altimetry across multiple platforms, ice flux from the primary tidewater glaciers of the Larsen B embayment are compared with published analysis of Greenland tidewater glaciers at approximately the same latitudes. This yields insight onto the main controls of non-buttressed ice sheet glacial retreat.