Close

Service Interruption

The Cryosphere: Where the World is Frozen
Arctic Climatology and Meteorology navigation Arctic Meteorology Home Arctic Meteorology Home Arctic Meteorology Introduction Arctic Meteorology Factors Arctic Meteorology Patterns Arctic Meteorology Glossary Arctic Meteorology Gallery Arctic Map the Cryosphere

Basics

Arctic Climatology and Meteorology Basics navigation What is the Arctic Weather vs. Climate Synoptic Meteorology Arctic Climate Optical and Acoustic Phenomena

Optical Haze

Also called shimmer, optical haze occurs in a layer of air next to the ground where small-scale convective currents develop. In this layer warmer air ascends and colder air descends. The difference in how the warm and cold air refract light causes a blurring of objects seen though the layer. Optical haze occurs quite frequently in the Arctic in the same meteorological conditions as the inferior mirage, and often makes it difficult to identify details in the landscape.

Contact Us | NSIDC Web Policy | Use & Copyright | Our Sponsors

The National Snow and Ice Data Center

Supporting Cryospheric Research Since 1976
449 UCB  University of Colorado  Boulder, CO 80309-0449

Cooperative Institute for Research in Environmental Sciences (CIRES)    University of Colorado Boulder