EGU22-6841, updated on 18 Jan 2023
https://doi.org/10.5194/egusphere-egu22-6841
EGU General Assembly 2022
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Rise in the frequency and intensity of extreme temperature events over New Zealand in connection to synoptic circulation features

Anjali Thomas1, Adrian McDonald1, James Renwick2, Jordis Tradowsky3,4, and Greg Bodeker2,3
Anjali Thomas et al.
  • 1University of Canterbury, School of Physical and Chemical Sciences, Christchurch, New Zealand (anjali.thomas@pg.canterbury.ac.nz)
  • 2Victoria University of Wellington, School of Geography, Environment and Earth Science, New Zealand(james.renwick@vuw.ac.nz, greg@bodekerscientific.com)
  • 3Bodeker Scientific, Alexandra, New Zealand (jordis@bodekerscientific.com, greg@bodekerscientific.com)
  • 4Deutscher Wetterdienst, Regional Climate Office Potsdam, Stahnsdorf, Germany (jordis@bodekerscientific.com,)

Extreme temperature events (ETEs) have evolved alongside the warming climate over most parts of the world. This study provides a statistical quantification of how human influences have increased the likelihood and frequencies of ETEs in New Zealand, depending on the synoptic weather type. We use the simulation under pre-industrial conditions (natural scenarios with no rise in greenhouse gases (GHGs)) and present-day conditions (anthropogenic scenarios) from the weather@home regional climate model. The ensembles of simulations under these two scenarios are used to identify how increases in GHG concentrations have impacted the frequency and intensity of ETEs based on their connection to different large-scale circulation patterns derived using Self Organizing Maps (SOMs). Over New Zealand, an average 2-3 fold rise in frequencies of extremes occurs irrespective of seasons due to elevated GHG concentrations with a mean temperature increase close to 1℃. For some synoptic situations, the frequency and intensity of ETEs are enhanced. In particular, for low-pressure centers to the northeast of New Zealand, the frequency of occurrence of daily temperature extremes has increased by a factor of 7 between anthropogenic and natural simulations for the winter season, though these synoptic patterns rarely occur. For low-pressure centers to the northwest of New Zealand, we observe extreme temperatures frequently in both anthropogenic and natural simulations which we attribute to warm air advection from the tropics. The frequency of occurrence of these synoptic patterns has also increased by a factor of 2 between the natural and anthropogenic simulations. For these synoptic states, the extremes are observed in the North Island and along the east coast of the country with the highest temperature along the Canterbury coast and Northland. However, the change between the natural and anthropogenic simulations is largest on the west coast along the Southern Alps.

How to cite: Thomas, A., McDonald, A., Renwick, J., Tradowsky, J., and Bodeker, G.: Rise in the frequency and intensity of extreme temperature events over New Zealand in connection to synoptic circulation features, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-6841, https://doi.org/10.5194/egusphere-egu22-6841, 2022.

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