Honors (Bachelor's)Atmospheric, Oceanic, and Space ScienceEarth and Environmental SciencesUniversity of Michiganhttp://deepblue.lib.umich.edu/bitstream/2027.42/96848/1/robincz.pd
Despite the potentially detrimental impact of large-scale calving events on the geometry and ice flo...
The Larsen C ice shelf is the most northerly of the remaining major Antarctic Peninsula ice shelves ...
Calving is a complex process subject to several cooperating atmospheric, oceanographic and glaciolog...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/102662/1/jgrf20163.pdfhttp://deepblue.l...
ABSTRACT. For three field seasons (2002/03, 2004/05, 2005/06) we have deployed a network of GPS rec...
We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in Dec...
We use satellite imagery from four sensors (Multi-angle Imaging SpectroRadiometer (MISR), Enhanced T...
Iceberg calving accounts for two thirds of the mass discharged from the cryosphere to the ocean. Des...
[1] We investigate ice shelf rift propagation using a combination of GPS and seismic measurements ne...
The calving of icebergs from large Antarctic ice shelves is controlled mainly by the formation and p...
Iceberg calving is a dominant mass loss mechanism for Antarctic ice shelves, second only to basal me...
The rate and direction of rift propagation through ice shelves depend on both the stress field and ...
Mass loss from the Antarctic ice sheet predominantly occurs at the fringing ice shelves via iceberg ...
The majority of mass lost from the Antarctic ice sheet takes place at the fringing ice shelves via ...
Ice shelves are important components of the Antarctic ice sheet due to their ice-ocean-atmosphere in...
Despite the potentially detrimental impact of large-scale calving events on the geometry and ice flo...
The Larsen C ice shelf is the most northerly of the remaining major Antarctic Peninsula ice shelves ...
Calving is a complex process subject to several cooperating atmospheric, oceanographic and glaciolog...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/102662/1/jgrf20163.pdfhttp://deepblue.l...
ABSTRACT. For three field seasons (2002/03, 2004/05, 2005/06) we have deployed a network of GPS rec...
We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in Dec...
We use satellite imagery from four sensors (Multi-angle Imaging SpectroRadiometer (MISR), Enhanced T...
Iceberg calving accounts for two thirds of the mass discharged from the cryosphere to the ocean. Des...
[1] We investigate ice shelf rift propagation using a combination of GPS and seismic measurements ne...
The calving of icebergs from large Antarctic ice shelves is controlled mainly by the formation and p...
Iceberg calving is a dominant mass loss mechanism for Antarctic ice shelves, second only to basal me...
The rate and direction of rift propagation through ice shelves depend on both the stress field and ...
Mass loss from the Antarctic ice sheet predominantly occurs at the fringing ice shelves via iceberg ...
The majority of mass lost from the Antarctic ice sheet takes place at the fringing ice shelves via ...
Ice shelves are important components of the Antarctic ice sheet due to their ice-ocean-atmosphere in...
Despite the potentially detrimental impact of large-scale calving events on the geometry and ice flo...
The Larsen C ice shelf is the most northerly of the remaining major Antarctic Peninsula ice shelves ...
Calving is a complex process subject to several cooperating atmospheric, oceanographic and glaciolog...
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