Index
- Alaska Climate Divisions FAQs
- Anomalies vs. Temperature
- Arctic Sea Ice Measurements
- Billion-Dollar Disasters: Calculating the Costs
- Binomial Filter
- Climate Division Dataset Transition
- Climate Extremes Index
- CLIMAT Messages
- Climatological Rankings
- Coral Reef Bleaching
- Dead Fuel Moisture
- Definition of Drought
- Drought Indicators
- Drought in the Colorado River Basin
- Drought vs. Aridity
- El Niño: A Historical Perspective
- Explanation of the 500 mb Flow
- Future Drought
- Global Precipitation Percentile Maps
- Global Regions Definitions
- Global Temperature Anomaly Percentile Maps
- Global Temperature Uncertainty
- Groundwater Drought Indicators
- Hawaiʻi Climate Divisions FAQs
- LOESS
- Measuring Drought
- Monthly Releases
- Monthly Report RSS Feed
- nClimDiv Maximum and Minimum Temperatures
- Palmer Drought Index
- Potential Evapotranspiration
- Reforestation of Bastrop Lost Pines
- Regional Climate Centers
- Regional Snowfall Index (RSI)
- Satellite-Based Drought Indicators
- Soil Moisture Water Balance Models
- Southern Hemisphere Snow Cover Extent
- Standardized Precipitation Index
- Streamflow Drought Indicators
- Subtropical Highs
- Tornado Count
- U.S. Climate Divisions
- U.S. Climate Normals
- U.S. Drought Monitor Scale
- USHCN Version 2.5 Transition
- Water Supply vs. Water Demand
Southern Hemisphere Snow Cover Extent
As part of its monthly State of the Climate Global Snow & Ice report, the National Centers for Environmental Information monitors monthly and seasonal snow cover extent across the Northern Hemisphere's major land areas — North America and Eurasia — using data from the Rutgers Global Snow Lab. Snow cover extent is sensitive to both regional temperatures and precipitation patterns across the mid and high latitudes, providing an important metric to measure the earth's climate system. By utilizing NOAA satellites, snow cover can be observed over all land areas, not just locations with surface-based observations, which can be sparse in non-developed areas of the globe.
Snow cover extent in the Southern Hemisphere is not currently examined for several reasons:
- Snow cover can only be measured over land areas, and not the ocean surface. Most of the surface area of the Southern Hemisphere is covered by ocean.
- The Southern Hemisphere land area located in the mid and high latitudes is very small, excluding Antarctica, when compared to the land area of the Northern Hemisphere at the same latitudes.
- The Antarctic continent is generally snow covered year round, with very little annual variation.
- Snow cover is difficult to measure across Antarctica and the high elevations of South America. These land areas are mostly covered by glaciers, and it is nearly impossible to distinguish snow cover from glacial ice using current satellite technology.