Editorial on the Research Topic Pan-Arctic snow researchSnowpacks are a key component of the Earth's environment and play a fundamental role in regulating both the Earth's energy budget and the Arctic hydrological cycle (Bolibar et al., 2022). Polar snowpacks constitute the largest interface between the atmosphere and the Earth's surface during winter (Bennett et al., 2022) and cover between 40% and 50% of the land surface during winter in the northern hemisphere (excluding the snow over sea ice). Although the seasonal snow cover represents a crucial component of the cryosphere (van Pelt et al., 2019), it is also the most variable and short-lived. Snow deposited on land or ice surfaces is thermodynamically unstable and is in constant change due to snow metamorphism, which is mainly controlled by temperature gradients (Pinzer and Schneebeli, 2009;Gallet et al., 2018;Domine et al., 2019). Snowpack affects the hydrological cycle by acting as a water reservoir during the wintertime while it contributes to the replenishment of water tables and rivers during the spring and summer melt periods (Bennett et al., 2022). The annual snowpacks are also critical for the mass balance of glaciers, providing them with water mass input (in the solid form) required for their growth, or at least helping to decelerate the speed at which they are disappearing by protecting the ice surface from solar radiation and melting (Bolibar et al., 2022). Snowpacks are not only reservoirs, but they are also ecosystems too, harboring a variety of microorganisms, such as prokaryotes, fungi, algae, protists, and viruses, that vary in abundance, physiological characteristics, community composition and diversity depending on both season and location (Maccario et al., 2015). These snow microbial communities are not only active at temperatures below 0 °C, but also dynamic and interact with their chemical environment (Maccario et al., 2015). Therefore, the biotic compartment of snow in the Arctic has a crucial role in the production, degradation, and transformation of contaminants and nutrients and is a key player in biogeochemical cycles.The main Research Topic of this Research Topic was to collect research proposing new and improved methodologies and techniques for physical, chemical, and biological snowpack observations. Since the snowpack is the most dynamic portion of the