TY - JOUR
T1 - Tonga eruption increases chance of temporary surface temperature anomaly above 1.5 °C
AU - Jenkins, Stuart
AU - Smith, Chris
AU - Allen, Myles
AU - Grainger, Roy
N1 - Funding Information:
S.J. acknowledges NERC grant NE/L002612/1 and support from the European Space Agency’s Climate Change Initiative. S.J. and M.A. acknowledge funding from the European Union’s Horizon 2020 research programme with grant agreement no. 821205 (FORCeS). R.G. acknowledges support of the National Centre for Earth Observation, contract no. PR140015. C.S. acknowledges the NERC/IIASA collaborative research fellowship scheme with grant no. NE/T009381/1.
Publisher Copyright:
© 2023, The Author(s), under exclusive licence to Springer Nature Limited.
PY - 2023/2
Y1 - 2023/2
N2 - On 15 January 2022, the Hunga Tonga–Hunga Ha’apai (HTHH) eruption injected 146 MtH2O and 0.42 MtSO2 into the stratosphere. This large water vapour perturbation means that HTHH will probably increase the net radiative forcing, unusual for a large volcanic eruption, increasing the chance of the global surface temperature anomaly temporarily exceeding 1.5 °C over the coming decade. Here we estimate the radiative response to the HTHH eruption and derive the increased risk that the global mean surface temperature anomaly shortly exceeds 1.5 °C following the eruption. We show that HTHH has a tangible impact of the chance of imminent 1.5 °C exceedance (increasing the chance of at least one of the next 5 years exceeding 1.5 °C by 7%), but the level of climate policy ambition, particularly the mitigation of short-lived climate pollutants, dominates the 1.5 °C exceedance outlook over decadal timescales.
AB - On 15 January 2022, the Hunga Tonga–Hunga Ha’apai (HTHH) eruption injected 146 MtH2O and 0.42 MtSO2 into the stratosphere. This large water vapour perturbation means that HTHH will probably increase the net radiative forcing, unusual for a large volcanic eruption, increasing the chance of the global surface temperature anomaly temporarily exceeding 1.5 °C over the coming decade. Here we estimate the radiative response to the HTHH eruption and derive the increased risk that the global mean surface temperature anomaly shortly exceeds 1.5 °C following the eruption. We show that HTHH has a tangible impact of the chance of imminent 1.5 °C exceedance (increasing the chance of at least one of the next 5 years exceeding 1.5 °C by 7%), but the level of climate policy ambition, particularly the mitigation of short-lived climate pollutants, dominates the 1.5 °C exceedance outlook over decadal timescales.
UR - https://doi.org/10.1038/s41558-022-01568-2
UR - http://www.scopus.com/inward/record.url?scp=85146165604&partnerID=8YFLogxK
U2 - 10.1038/s41558-022-01568-2
DO - 10.1038/s41558-022-01568-2
M3 - Article
SN - 1758-678X
VL - 13
SP - 127
EP - 129
JO - Nature Climate Change
JF - Nature Climate Change
M1 - 13
ER -