Temperature lag
Temperature lag is when change in temperature lags change in radiation (heating or cooling). Meteorological examples include:
- Diurnal temperature variation – e.g., peak daily temperature typically occurs after noon
- Seasonal lag – e.g., peak annual temperature typically occurs after the summer solstice
This article is issued from Wikipedia - version of the Saturday, November 29, 2014. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.