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micrometeorology

American  
[mahy-kroh-mee-tee-uh-rol-uh-jee] / ˌmaɪ kroʊˌmi ti əˈrɒl ə dʒi /

noun

  1. the study of local and small-scale atmospheric phenomena, usually confined to the physical and dynamic occurrences within a shallow stratum of air adjacent to the ground.


micrometeorology British  
/ ˌmaɪkrəʊˌmiːtɪəˈrɒlədʒɪ /

noun

  1. the study of the layer of air immediately above the earth and of small-scale meteorological processes

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

micrometeorology Scientific  
/ mī′krō-mē′tē-ə-rŏlə-jē /
  1. The branch of meteorology that deals with weather conditions on a small scale, both in terms of space and time. For example, weather conditions lasting less than a day in the area immediately surrounding a smokestack, a building, or a mountain are studied in micrometeorology.


Other Word Forms

Derived Forms

Etymology

Origin of micrometeorology

First recorded in 1925–30; micro- + meteorology

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