The Arctic Surface Climate in CMIP6: Status and Developments since CMIP5 in: Journal of
Climate Volume 33 Issue 18 (2020) Jump to Content Jump to Main Navigation Logo Logo Logo …

As the Arctic continues to warm faster than the rest of the planet, evidence mounts that the
region is experiencing unprecedented environmental change. The hydrological cycle is …

In recent decades, surface air temperature (SAT) data from Global reanalyses points to
maximum warming over the northern Barents area. However, a scarcity of observations …

Year-round observations of the physical snow and ice properties and processes that govern
the ice pack evolution and its interaction with the atmosphere and the ocean were …

This study presents a comprehensive inter-comparison between two widely used rainfall
datasets–the Global Precipitation Climatology Project (GPCP) and the ERA-Interim …

Streamflow in high-mountain Asia is influenced by meltwater from snow and glaciers, and
determining impacts of climate change on the region's cryosphere is essential to understand …

As a step towards understanding the fundamental drivers of polar climate change, we
evaluate contributions to polar warming and its seasonal and hemispheric asymmetries in …

Reanalysis precipitation estimates are widely used in the fields of meteorology and
hydrology because they can provide physical, spatial, and temporal coherent long time …

A Lagrangian snow‐evolution model (SnowModel‐LG) was used to produce daily, pan‐
Arctic, snow‐on‐sea‐ice, snow property distributions on a 25× 25‐km grid, from 1 August …

We present a first examination of Arctic sea ice snow depth estimates from differencing
satellite lidar (ICESat‐2) and radar (CryoSat‐2) freeboards. These estimates cover the …