Results 231 to 240 of about 190,113 (342)
A comparison of shipborne and airborne electromagnetic methods for Antarctic sea ice thickness measurements [PDF]
James Reid+2 more
openalex +1 more source
Energy balance in women during polar trekking—The POWER study
Polar trekking is characterized by a negative energy balance. While it can be sustained during a few days, prolonged periods of energy deficiency can lead to adverse health effects. Abstract Polar expeditions pose a significant challenge, contributing to a substantial energy deficit.
Pierre Bourdier+8 more
wiley +1 more source
Antarctic ice volume and deep-sea temperature during the last 50 Myr: a model study [PDF]
J. Oerlemans
openalex +1 more source
Abstract Antarctic ice shelves control the flow of ice into the ocean, affecting the rate of sea level rise. This flow is regulated by ice‐shelf thickness, which depends on tributary flux across the grounding line and the balance between surface accumulation and ocean‐induced melting.
Vjeran Višnjević+5 more
wiley +1 more source
An Assessment of Subseasonal Prediction Skill of the Antarctic Sea Ice Edge. [PDF]
Gao Y+7 more
europepmc +1 more source
Impact of the Madden-Julian oscillation on Antarctic sea ice and its dynamical mechanism. [PDF]
Lee HJ, Seo KH.
europepmc +1 more source
Studies of Antarctic sea ice concentrations from satellite data and their applications
Josefino C. Comiso, Konrad Steffen
openalex +1 more source
The First Firn Core From the Cordillera Darwin Icefield: Implications for Future Ice Core Research
Abstract The Southern Hemisphere westerly winds (SHWWs) (45–65°S) are important regulators of the Southern Hemisphere climate. The scarcity of observational records at the core of the wind belt hinders our understanding of the environmental impact and long‐term variability of the westerly winds.
Dieter R. Tetzner+13 more
wiley +1 more source
Role of anthropogenic forcing in Antarctic sea ice variability simulated in climate models. [PDF]
Morioka Y+5 more
europepmc +1 more source
Abstract Present‐day ice‐mass changes in Antarctica typically deform the solid Earth elastically, and this signal needs removing from Global Positioning System (GPS) observations of displacement before they can be used to constrain models of glacial isostatic adjustment.
Grace A. Nield+6 more
wiley +1 more source