Fig. 7: Differences between standalone ARs and foehn winds.
From: Intense atmospheric rivers can weaken ice shelf stability at the Antarctic Peninsula
The difference between anomalies associated with AR landfalls with an IVT above 400 kg m−1 s–1 and foehn events according to the foehn detection algorithm11 for MAR a 2 m temperature, b surface melting, c sensible heat flux, and d downward longwave radiation from 2009 to 2012.
