Mass loss from the Greenland Ice Sheet (GrIS) has accelerated over the past two decades,
coincident with rapid Arctic warming and increasing moisture transport over Greenland by …

Greenland Ice Sheet surface temperatures are controlled by an exchange of energy at the
surface, which includes radiative, turbulent, and ground heat fluxes. Data collected by …

Abstract The Greenland Ice Sheet (GrIS) is losing mass at an increasing rate yet mass gain
from snowfall still exceeds the loss attributed to surface melt processes on an annual basis …

A novel method for classifying Arctic precipitation using ground based remote sensors is
presented. Using differences in the spectral variation of microwave absorption and …

The mass of the Greenland Ice Sheet (GrIS) is decreasing due to increasing surface melt
and ice dynamics. Snowfall both adds mass to the GrIS and has the capacity to reduce …

The polarization of the atmosphere has been a long-standing concern for ground-based
experiments targeting cosmic microwave background (CMB) polarization. Ice crystals in …

The unambiguous retrieval of cloud phase from polarimetric lidar observations is dependent
on the assumption that only cloud scattering processes affect polarization measurements. A …

Energy exchange at the Greenland Ice Sheet surface governs surface temperature
variability, a factor critical for representing increasing surface melt extent, which portends a …

Clouds are the primary modulator of radiation and moisture received by the Arctic surface.
Long term, large scale, and detailed observations of Arctic clouds are required to connect …

Greenland Ice Sheet surface temperatures are controlled by an exchange of energy at the
surface, which includes radiative, turbulent, and ground heat fluxes. Data collected by …