Abstract
AbstractThis study compares two methods of multimodel averaging for the future projection of precipitation based on the classically defined absolute and relative climate changes. In the relative change scheme, the multimodel average of the percentage changes in precipitation is multiplied by the observed present climate to form the future projection; this method is equivalent to applying unequal weighting to the absolute change scheme which potentially implies a bias correction. The new scheme and the classical equal weight scheme for the absolute change do not produce radically different large‐scale patterns of the trend in precipitation. Nevertheless, notable differences emerge in regional scales. Copyright © 2012 Royal Meteorological Society
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
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.