Introduction to the SPARC Reanalysis Intercomparison Project (S-RIP) and overview of the reanalysis systems

Authors:

Masatomo Fujiwara, Jonathon S Wright, Gloria L Manney, Lesley J Gray, James Anstey, Thomas Birner, Sean Davis, Edwin P Gerber, V Lynn Harvey, Michaela I Hegglin, Cameron R Homeyer, John A Knox, Kirstin Krüger, Alyn Lambert, Craig S Long, Patrick Martineau, Beatriz M Monge-Sanz, Michelle L Santee, Susann Tegtmeier, Simon Chabrillat, David GH Tan, David R Jackson, Saroja Polavarapu, Gilbert P Compo, Rossana Dragani, Wesley Ebisuzaki, Yayoi Harada, Chiaki Kobayashi, Will McCarty, Kazutoshi Onogi, Steven Pawson, Adrian Simmons, Krzysztof Wargan, Jeffrey S Whitaker, Cheng-Zhi Zou

Isolating the boreal winter response to the Pinatubo and Krakatoa eruptions using large-ensemble single-forcing simulations

Authors:

Chaim I Garfinkel, David Avisar, Wenjuan Huo, Ales Kuchar, Shoshiro Minobe, Scott Osprey, Katharina Perny, Jonathon S Wright

Key drivers of large scale changes in North Atlantic atmospheric and oceanic circulations and their predictability

Authors:

Buwen Dong, Yevgeny Yevgeny Aksenov, Ioana Colfescu, Ben Harvey, Joël Hirschi, Simon Josey, Hua Lu, Jenny Mecking, Marilena Oltmanns, Scott Osprey, Jon Robson, Stefanie Rynders, Len Shaffrey, Bablu Sinha, Rowan Sutton, Antje Weisheimer

Major volcanic eruptions episodically disrupted the continuity of polar warming through aerosol forcing

npj Clean Air Springer Nature

Authors:

Roy Grainger, Basudev Swain, Scott Osprey, Rui Song, Marco Vountas

Abstract:

The polar regions are warming rapidly, exceeding the global average due to greenhouse gas emissionsfrom human activities. Using CMIP6 simulations, HadCRUT5 data, and MERRA-2 aerosol records, thisstudy shows that major 20th-century volcanic eruptions, Agung (1963), El Chicho´n (1982), and Pinatubo(1991) temporarily offset polar warming through sulfate-induced cooling. The Agung eruption suppressedArctic surface air temperature anomalies for approximately 4-5 years (1964–1968), El Chicho´n for asimilar duration (1983–1987), and Pinatubo for about 4-5 years (1992–1996), demonstrating a consistentmulti-year cooling response following each event.Without these eruptions, Arctic surface air temperatureanomalies would have increased by up to 0.5 °C, whereas volcanic activity caused short-term coolingranging from –0.07 °C to –0.4 °C. Arctic minimum temperatures (Tmin) are rising faster than maximumtemperatures (Tmax), indicating asymmetric warming. In contrast, Antarctic responses were weaker,moderated by oceanic and atmospheric dynamics. Collectively, these eruptions produced episodic multi-year cooling that temporarily interrupted the ongoing Arctic warming trajectory, with warming resumingas volcanic aerosol forcing diminished. Spatial patterns reveal pronounced warming in the central Arctic,Greenland, and Siberia in the absence of volcanic forcing, highlighting the role of eruptions in modulating polar warming and providing insights relevant to future geoengineering considerations.

Multi-decadal variability in skill of predicting ENSO spatial pattern

Geophysical Research Letters American Geophysical Union

Authors:

Matthew Wright, Antje WEISHEIMER, Tim WOOLLINGS