The snowpack conditions in New Mexico vary across different mountain ranges that contribute to the state's water supply. The Sangre de Cristo Mountains, located in the northern part of the state, receive the greatest snowfall. These mountains provide snow for the Rio Grande, Pecos, and Canadian River watersheds. The Jemez Mountains and San Juan Mountains also contribute to the state's snowpack.

Winter climate characteristics in New Mexico include cold temperatures, occasional heavy snowfall, and strong winds. The snowpack typically accumulates from November to April and serves as a vital water source during the dry summer months.

Interesting facts about snow science in New Mexico include the study of snow hydrology, which helps predict snowmelt runoff and manage water resources. Furthermore, snow surveys are conducted to measure snow depth and water content, providing critical data for water resource planning.

It is important to verify the accuracy of this information across multiple sources due to the ever-changing nature of snowpack conditions and scientific research.