Abstract
AbstractA change from negative to positive circulation anomalies over New South Wales (NSW) during the 1970s resulted in a decrease in east coastal low‐pressure systems and accompanying rain. Negative pressure anomalies over eastern Australia, anomalous onshore low‐level winds and larger NSW rainfall totals since 1950, occur in the cool phase of the IPO rather than the warm phase (post‐1976). Larger NSW extreme annual rainfall totals occurred prior to 1977 and were characterized by negative mean sea level pressure (MSLP) anomalies over eastern Australia. In contrast, extreme annual rainfall totals from 1977 were smaller and characterized by positive MSLP anomalies. Copyright © 2008 Royal Meteorological Society
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.
