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Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Surface mass balance of Pine Island Glacier, West Antarctica over the period ...
Airborne radar soundings of internal reflection layers were collected across the Pine Island (PIG) catchment area, West Antarctica, aboard the Polar 5 aircraft between 01 and 03... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal Reflection Horizon (IRH) in western Dronning Maud Land, East Antarct...
We present internal reflection horizons (IRHs) from airborne radar data in western Dronning Maud Land, East Antarctica. The IRHs were dated at the EDML ice core and IRH ages... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
ASIRAS Level 1b radargrams of Pine Island Glacier
Elevation in NetCDF files bases on WGS84 -
Picked reflection layer data, ASIRAS Flight Profile: 20156102
This dataset has no description
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Gridded SMB and error maps of Pine Island Glacier
WGS84/Polar Stereographic Projection, Centre Latitude = -71 deg, Centre Longitude = 0 deg. -
Smoothed alongtrack SMB estimates considered for krige estimation, which yiel...
This dataset has no description
