Damage intensity increases ice mass loss from Thwaites Glacier, Antarctica [PDF]
Ice damage, which results from the formation and development of crevasses on glaciers, plays a critical role in ice-shelf stability, grounding-line retreat, and subsequent sea-level rise. Yet, few ice-sheet models explicitly account for ice damage or its
Y. Li +5 more
doaj +1 more source
Evaluación del árbol de clasificación y regresión de Thwaites
Objetivo. Evaluar el valor diagnóstico del arbol de clasificación y regresión de Thwaites para diferenciar, meningitis tuberculosa, de meningitis bacteriana. Materiales y métodos.
Andrea Llanos Mendoza +1 more
doaj +1 more source
Competing processes determine the long-term impact of basal friction parameterizations for Antarctic mass loss [PDF]
Previous studies do not agree on the magnitude of the influence of basal friction laws in sea-level projections. We use the Community Ice Sheet Model (CISM) to show that the sensitivity of the projected sea level rise to the choice of basal friction law ...
T. van den Akker +8 more
doaj +1 more source
Coupled ice–ocean interactions during future retreat of West Antarctic ice streams in the Amundsen Sea sector [PDF]
The Amundsen Sea sector has some of the fastest-thinning ice shelves in Antarctica, caused by high, ocean-driven basal melt rates, which can lead to increased ice streamflow, causing increased sea level rise (SLR) contributions. In this study, we present
D. T. Bett +6 more
doaj +1 more source
Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength
A weaker ocean gyre in the Pine Island Bay, suppressed by higher sea-ice concentration over the ocean near the Thwaites Eastern Ice Shelf, allows more meltwater to enter the sub-ice-shelf cavity. This increases the ocean temperature beneath the ice.
Tiago S. Dotto +16 more
doaj +1 more source
Calving Dynamics and the Potential Impact of Mélange Buttressing at the Western Calving Front of Thwaites Glacier, West Antarctica [PDF]
The western region of the wide Thwaites Glacier terminus is characterized by a near-vertical calving front. The grounding line at this western calving front (WCF) rests on a relatively high ridge, behind which exists a reverse-sloping bed; retreat of the
Luckman, Adrian +9 more
core +1 more source
Past water flow beneath Pine Island and Thwaites glaciers, West Antarctica [PDF]
Outburst floods from subglacial lakes beneath the Antarctic Ice Sheet modulate ice-flow velocities over periods of months to years. Although subglacial lake drainage events have been observed from satellite-altimetric data, little is known about their ...
J. D. Kirkham +7 more
doaj +1 more source
ABSTRACT For regenerative agricultural systems such as food forests to move from experimental niches to scalable market solutions, they must attract consumer acceptance and sufficient willingness to pay a price premium. This study examines the demand‐side drivers of consumers' willingness to pay for food forest produce, focusing on nature connectedness,
Ada Folques +3 more
wiley +1 more source
Model setup for simulations of melting beneath Thwaites Glacier
Model parameter and forcing files needed to simulate the ocean beneath Thwaites Glacier during the period 2011-2022 as described in the paper "Strong ocean melting feedback during the recent retreat of Thwaites Glacier" in Geophysical Research Letters by
Paul Holland +2 more
core +2 more sources
Learning in radiation oncology: 12‐month experience with a new incident learning system
Introduction of an incident learning incident (ILS) was shown to have had a positive impact on reporting and safety culture within a local health district (LHD). Survey findings correlate with existing literature that ILSs are effective tools for improving patient safety and departmental safety facilitating quality improvement.
Krystle Crouch +4 more
wiley +1 more source

