Results 81 to 90 of about 12,199 (215)

La azarosa privatización de Aerolíneas Argentinas : paradigmático testimonio de un cambio de rumbo [PDF]

, 1993
Fil: Thwaites Rey, Mabel. Universidad de Buenos Aires. Facultad de Ciencias Económicas.
Thwaites Rey, Mabel
core  

Ocean access beneath the southwest tributary of Pine Island Glacier, West Antarctica

Annals of Glaciology, 2018
The catchments of Pine Island Glacier and Thwaites Glacier in the Amundsen Sea Embayment are two of the largest, most rapidly changing, and potentially unstable sectors of the West Antarctic Ice Sheet.
Dustin M. Schroeder, Andrew M. Hilger, John D. Paden, Duncan A. Young, Hugh F. J. Corr   +4 more
doaj   +1 more source

Thwaites, W P, VX4616

, 2017
This record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete.
Australian Red Cross Society, National Office
core  

Thwaites Basal Melt Calculations

Jakob, L., & Gourmelen, N. (2025). Thwaites Basal Melt Calculations (Version v1). Zenodo.
Jakob, Livia, School of GeoSciences, Gourmelen, Noel   +2 more
core   +1 more source

On Mr. Thwaites second inscrutable Cypher deciphered by C.

ON MR. THWAITES SECOND INSCRUTABLE CYPHER DECIPHERED BY C. On Mr. Thwaites second inscrutable Cypher deciphered by C. (-
Babbage, Charles
core   +1 more source

Modeling Ocean Heat Transport to the Grounding Lines of Pine Island, Thwaites, Smith, and Kohler Glaciers, West Antarctica

Geophysical Research Letters
Pine Island, Thwaites, Smith, and Kohler glaciers in the Amundsen Sea Embayment (ASE) sector of West Antarctica experience rapid mass loss and grounding line retreat due to enhanced ocean thermal forcing from Circumpolar Deep Water (CDW) reaching the ...
Andy Dinh, Eric Rignot, Matthew Mazloff, Ian Fenty   +3 more
doaj   +1 more source

Adaptively constraining radar attenuation and temperature across the Thwaites Glacier catchment using bed echoes

Journal of Glaciology, 2016
Englacial temperature is a major control on ice rheology and flow. However, it is difficult to measure at the glacier to ice-sheet scale. As a result, ice-sheet models must make assumptions about englacial temperature and rheology, which affect sea level
DUSTIN M. SCHROEDER, HELENE SEROUSSI, WINNIE CHU, DUNCAN A. YOUNG   +3 more
doaj   +1 more source

Direct Geologic Constraints on the Timing of Late Holocene Ice Thickening in the Amundsen Sea Embayment, Antarctica

Geophysical Research Letters
Constraining past West Antarctic Ice Sheet (WAIS) change helps validate numerical models simulating future ice sheet dynamics. Following rapid deglaciation during the mid‐Holocene, ice near Thwaites Glacier was ∼35 m thinner than present; however, the ...
Keir A. Nichols, Jonathan R. Adams, Katie Brown, Roger C. Creel, Marion A. McKenzie, Ryan A. Venturelli, Joanne S. Johnson, Dylan H. Rood, Klaus Wilcken, John Woodward, Stephen J. Roberts   +10 more
doaj   +1 more source

Retreat of Thwaites Glacier Triggered by its Neighbours

The Amundsen Sea Embayment in West Antarctica is experiencing the most rapid mass loss and grounding line retreat in Antarctica. Its glaciers are vulnerable to retreat through marine ice sheet instability.
Stephen Cornford, Suzanne Bevan
core   +1 more source

Recent Observations of Thwaites Glacier, West Antarctica Are Consistent With High Rates of Loss in Next 50 Years

Geophysical Research Letters
Thwaites Glacier has experienced accelerating mass loss, with rates increasing over fivefold since the 1990s. We apply transient calibration to two independent ice‐sheet models (STREAMICE and ISSM) using time‐varying velocity and surface elevation data ...
Daniel N. Goldberg, Mathieu Morlighem, Noel Gourmelen   +2 more
doaj   +1 more source