Abstract
Central England temperature fluctuations are found to be monoscaling with long-range dependence. Monoscaling can be explained in terms of the dominance of Gaussian temperature advection. Simulations of the UK Meteorological Office Hadley Centre general circulation model do not capture many of these features.
Sign-in/Register to access full text options 
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 callDisclaimer: 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.
