Arctic amplification (AA)—referring to the enhancement of near-surface air temperature
change over the Arctic relative to lower latitudes—is a prominent feature of climate change …

Recent satellite observations confirm that the Arctic is absorbing more solar radiation now
than at the start of this century in response to declining Arctic sea ice and snow covers …

The zero emissions commitment (ZEC) is the expected temperature change following the
cessation of anthropogenic emissions of climate altering gases and aerosols. Recent model …

The rapid Arctic sea ice retreat in the early 21st century is believed to be driven by several
dynamic and thermodynamic feedbacks, such as ice-albedo feedback and water vapor …

This study analyses the cloud radiative effect (CRE) obtained from near-surface
observations of three airborne campaigns in the Arctic north-west of Svalbard: Airborne …

This study employs ERA5 reanalysis and CERES/EBAF Ed4. 1 data to evaluate the
dominant features of summer shortwave cloud radiative effect (SWCRE) variability and …

Over the past 30 years, the Arctic Dipole Anomaly (DA) has repeatedly led to record lows in
summer sea ice extent, with cloud radiative effects (CRE) playing a crucial regulatory role …

Approximations in the moist thermodynamics of atmospheric models can often be
inconsistent; different parts of numerical models may handle the thermodynamics in different …

The Arctic atmosphere–surface system transmits visible light from the Sun to the ocean,
determining the annual cycle of light available to microalgae. This light is referred to as …

Abstract The Ross-Amundsen sector is experiencing an accelerating warming trend and a
more intensive advective influx of marine air streams. As a result, massive surface melting …