Neglecting future sporadic volcanic eruptions underestimates climate uncertainty DOI Creative Commons
Man Mei Chim, Thomas J. Aubry, Chris Smith

et al.

Communications Earth & Environment, Journal Year: 2025, Volume and Issue: 6(1)

Published: March 25, 2025

Language: Английский

Trends and variability in the ocean carbon sink DOI
Nicolas Gruber, Dorothée C. E. Bakker, Tim DeVries

et al.

Nature Reviews Earth & Environment, Journal Year: 2023, Volume and Issue: 4(2), P. 119 - 134

Published: Jan. 24, 2023

Language: Английский

Citations

153

The unexpected radiative impact of the Hunga Tonga eruption of 15th January 2022 DOI Creative Commons
Pasquale Sellitto, Aurélien Podglajen, Redha Belhadji

et al.

Communications Earth & Environment, Journal Year: 2022, Volume and Issue: 3(1)

Published: Nov. 19, 2022

Abstract The underwater Hunga Tonga-Hunga Ha-apai volcano erupted in the early hours of 15th January 2022, and injected volcanic gases aerosols to over 50 km altitude. Here we synthesise satellite, ground-based, situ radiosonde observations eruption investigate strength stratospheric aerosol water vapour perturbations initial weeks after quantify net radiative impact across two species using offline transfer modelling. We find that produced largest global perturbation since Pinatubo 1991 observed satellite era. Immediately eruption, cooling dominated local heating/cooling rates, while at top-of-the-atmosphere surface, forcing. However, weeks, due dispersion/dilution, heating started dominate forcing, leading a warming climate system.

Language: Английский

Citations

122

Climate change: Strategies for mitigation and adaptation DOI Open Access
Fang Wang, Jean Damascene Harindintwali, Ke Wei

et al.

The Innovation Geoscience, Journal Year: 2023, Volume and Issue: 1(1), P. 100015 - 100015

Published: Jan. 1, 2023

<p>The sustainability of life on Earth is under increasing threat due to human-induced climate change. This perilous change in the Earth's caused by increases carbon dioxide and other greenhouse gases atmosphere, primarily emissions associated with burning fossil fuels. Over next two three decades, effects change, such as heatwaves, wildfires, droughts, storms, floods, are expected worsen, posing greater risks human health global stability. These trends call for implementation mitigation adaptation strategies. Pollution environmental degradation exacerbate existing problems make people nature more susceptible In this review, we examine current state from different perspectives. We summarize evidence Earth’s spheres, discuss emission pathways drivers analyze impact health. also explore strategies highlight key challenges reversing adapting change.</p>

Language: Английский

Citations

119

Interactive stratospheric aerosol models' response to different amounts and altitudes of SO2 injection during the 1991 Pinatubo eruption DOI Creative Commons
Ilaria Quaglia, Claudia Timmreck, Ulrike Niemeier

et al.

Atmospheric chemistry and physics, Journal Year: 2023, Volume and Issue: 23(2), P. 921 - 948

Published: Jan. 19, 2023

Abstract. A previous model intercomparison of the Tambora aerosol cloud has highlighted substantial differences among simulated volcanic properties in pre-industrial stratosphere and led to questions about applicability global models for large-magnitude explosive eruptions prior observational period. Here, we compare evolution stratospheric following well-observed June 1991 Mt. Pinatubo eruption with six interactive microphysics a range data sets. Our primary focus is on uncertainties regarding initial SO2 emission eruption, as prescribed Historical Eruptions Emission Assessment experiments (HErSEA), framework Interactive Stratospheric Aerosol Model Intercomparison Project (ISA-MIP). Six took part this study: ECHAM6-SALSA, EMAC, ECHAM5-HAM, SOCOL-AERv2, ULAQ-CCM, UM-UKCA. simulations are performed by varying injection amount (ranging between 5 10 Tg S) altitude (between 18–25 km). The comparisons show that all consistently demonstrate faster reduction from peak sulfate mass burden tropical stratosphere. Most also stronger transport towards extratropics Northern Hemisphere, at expense observed confinement, suggesting much weaker subtropical barrier models, which results shorter e-folding time compared observations. Furthermore, more than S form injected an overestimation tropics and, some Hemisphere large surface area density few months after values measured situ measurements over Laramie. This draws attention importance including processes such ash removal lofting through local heating.

Language: Английский

Citations

50

A robust reduction in near-surface wind speed after volcanic eruptions: Implications for wind energy generation DOI Creative Commons
Cheng Shen, Zhibo Li, Fei Liu

et al.

The Innovation, Journal Year: 2025, Volume and Issue: 6(1), P. 100734 - 100734

Published: Jan. 1, 2025

Public summary•Volcanic eruptions and geoengineering aerosol injections could significantly reduce wind speeds, impacting energy.•Simulations reveal a consistent 2-year global speed reduction after volcanic eruptions.•The is linked to decrease in downward momentum flux, triggered by forcing.•The 1815 Tambora eruption led ∼9.2% power density the following 2 years.AbstractNear-surface (NSWS), determinant of energy, influenced both natural anthropogenic factors. However, specific impacts on NSWS, remain unexplored. Our simulations spanning last millennium NSWS 10 major historical eruptions. This equates an approximately two inter-annual standard deviations from AD 851 1849. weakening subtropical descending air forcing. The eruption, one most powerful recent history, subsequent years. research fills knowledge gap, establishes theoretical foundation for empirical studies, highlights potential energy risks large atmospheric injections, including eruptions, nuclear warfare, climate intervention.Graphical abstract

Language: Английский

Citations

1

Past hydroclimate extremes in Europe driven by Atlantic jet stream and recurrent weather patterns DOI Creative Commons
Stefan Brönnimann, Jörg Franke, Veronika Valler

et al.

Nature Geoscience, Journal Year: 2025, Volume and Issue: 18(3), P. 246 - 253

Published: Feb. 27, 2025

Abstract The jet stream over the Atlantic–European sector is relevant for weather and climate in Europe. It generates temperature extremes steers moisture flood-propelling systems to Europe or facilitates development of atmospheric blocks, which can lead drought. Ongoing change may alter characteristics, affecting extremes. However, little known about past interannual-to-decadal variability stream. Here we analyse strength, tilt latitude from 1421 2023 an ensemble monthly daily reconstructions fields. We compare these indices with blocking frequency cyclonic activity data drought flood Summer enhanced Central periods a poleward-shifted jet. An equatorward-shifted associated decreased leads frequent floods Western Alps, particularly winter. Recurrent patterns causing often characterize entire season, such that association between peak discharge seen on seasonal even annual scales. Jet strength are significantly influenced by volcanic eruptions. Our 600-year perspective shows recent changes within cannot be drivers increasing frequency.

Language: Английский

Citations

1

Climate Projections Very Likely Underestimate Future Volcanic Forcing and Its Climatic Effects DOI Creative Commons
Man Mei Chim, Thomas J. Aubry, N. Luke Abraham

et al.

Geophysical Research Letters, Journal Year: 2023, Volume and Issue: 50(12)

Published: June 13, 2023

Abstract Standard climate projections represent future volcanic eruptions by a constant forcing inferred from 1850 to 2014 forcing. Using the latest ice‐core and satellite records design stochastic eruption scenarios, we show that there is 95% probability explosive could emit more sulfur dioxide (SO 2 ) into stratosphere over 2015–2100 than current standard (i.e., ScenarioMIP). Our simulations using UK Earth System Model with interactive stratospheric aerosols for median scenario, average global‐mean aerosol optical depth (SAOD) double used in ScenarioMIP, small‐magnitude (<3 Tg of SO contributing 50% SAOD perturbations. We effects on large‐scale indicators, including global surface temperature, sea level ice extent, are underestimated ScenarioMIP because do not fully account recurrent frequency different magnitudes.

Language: Английский

Citations

23

Spatial and Temporal Quantification of Subaerial Volcanism From 1980 to 2019: Solid Products, Masses, and Average Eruptive Rates DOI Creative Commons
Federico Galetto, M. E. Pritchard, Adrian Hornby

et al.

Reviews of Geophysics, Journal Year: 2023, Volume and Issue: 61(1)

Published: Feb. 10, 2023

Abstract Volcanism is one of the main mechanisms transferring mass and energy between interior Earth Earth's surface. However, global flux lava, volcanic ash explosive pyroclastic deposits not well constrained. Here we review published estimates erupted products from 1980 to 2019 by a compilation. We identified 1,064 magmatic eruptions that occurred Smithsonian Global Program database. For each eruption, reported both total its partitioning into different products. Using this data set, quantified temporal spatial evolution subaerial volcanism at regional scale. The magma in analyzed decade ranged 1.1–4.9 × 10 13 kg. Lava product representing ∼57% magma. related biggest (Magnitude ≥6), with long recurrence times, can temporarily make more abundant than lava (e.g., 1990–1999). Twenty‐three volcanoes produced ∼72% mass, while two sets 15 >70% either effusive or At scale, 40‐year average eruptive rates calculated have same magnitude as long‐term (from thousand millions years), because cases are scaled for times comparable time occurred.

Language: Английский

Citations

18

Immediate and Long‐Lasting Impacts of the Mt. Pinatubo Eruption on Ocean Oxygen and Carbon Inventories DOI Creative Commons
Amanda R. Fay, Galen A. McKinley, Nicole S. Lovenduski

et al.

Global Biogeochemical Cycles, Journal Year: 2023, Volume and Issue: 37(2)

Published: Jan. 24, 2023

Abstract Large volcanic eruptions drive significant climate perturbations through major anomalies in radiative fluxes and the resulting widespread cooling of surface upper ocean. Recent studies suggest that these also important variability air‐sea carbon oxygen fluxes. By simulating Earth system using two initial‐condition large ensembles, with without aerosol forcing associated Mt. Pinatubo eruption June 1991, we isolate impact this event on physical biogeochemical properties The forced ocean interior inventories heat, oxygen, carbon. Pinatubo‐driven changes persist for multiple years permanently modify ocean's inventories. Positive concentrations emerge immediately post‐eruption penetrate into deep In contrast, intensify over several post‐eruption, are largely confined to 150 m. tropics northern high latitudes, change is dominated by subsequent ventilation mid‐depths, while anomaly solubility eruption‐generated El Niño—Southern Oscillation variability. We do not find or Southern Ocean; but may be due Hemisphere being underestimated Community System Model 1 simulations.

Language: Английский

Citations

16

A review on vulnerable atmospheric aerosol nanoparticles: Sources, impact on the health, ecosystem and management strategies DOI

S. Karthick Raja Namasivayam,

S. Priyanka,

M. Lavanya

et al.

Journal of Environmental Management, Journal Year: 2024, Volume and Issue: 365, P. 121644 - 121644

Published: July 3, 2024

Language: Английский

Citations

6