Abstract
Spells of cold (hot) days in winter (summer) were defined as sequences of days with minimum (maximum) temperature at least one standard deviation below (above) the mean daily minimum (maximum) temperature, as observed during 40 years (1930–40, 1946–74) at the Aristotelian University in Thessaloniki, Greece. Winter cold spells were best fitted by a geometric (Markov) model, summer hot spells by a logarithmic one. Skill scores were 0.42 to 0.80 for forecasting cold days, 0.24 to 0.77 for hot days, from the respective models.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Archives for Meteorology, Geophysics, and Bioclimatology Series A
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
