Contrasting Stratospheric Smoke Mass and Lifetime From 2017 Canadian and 2019/2020 Australian Megafires: Global Simulations and Satellite Observations DOI Creative Commons
Gennaro D’Angelo, Stephen R. Guimond, Jon Reisner

et al.

Journal of Geophysical Research Atmospheres, Journal Year: 2022, Volume and Issue: 127(10)

Published: May 4, 2022

Abstract Stratospheric injections of carbonaceous aerosols and combustion gases by extreme wildfires have become increasingly common. Recent “megafires,” particularly large intense fires, delivered particulate burdens to the lower stratosphere comparable those moderate volcanic eruptions. The 2017 Canadian megafire generated four Pyrocumulonimbi (pyroCbs), injecting up ≈0.3 Tg smoke in stratosphere. Even more extreme, 2019/2020 Australian event produced a pyroCb activity resulting stratospheric intrusions ≈1 Tg. To understand their contrasting behavior, we present global climate simulations atmospheric response these events, applying informed remote observations. Model outcomes, compared satellite data transport, reproduce reasonably well initial plume rise, at 0.2–0.3 km/day, attaining heights ≈20 km Canada above 30 Australia. Global dispersal occurs within about 3 weeks both cases, consistent with Smoke removal timescales, ≈5 months for megafire, agree measurements. During observations indicate three times as large, models predict comparatively longer lifetimes, ≈16 months. After latter event, optical depths radiative cooling achieved values close measured following Pinatubo eruption. Sensitivity tests model assumptions indicate, accord prior studies, that burden, injection heights, black carbon content can determine evolution possible impacts. An empirical relation between peak plumes lifetimes is derived help assess impacts on stratosphere, Earth system.

Language: Английский

Wildfire smoke destroys stratospheric ozone DOI
P. F. Bernath, C. D. Boone, Jeff Crouse

et al.

Science, Journal Year: 2022, Volume and Issue: 375(6586), P. 1292 - 1295

Published: March 17, 2022

Large wildfires inject smoke and biomass-burning products into the mid-latitude stratosphere, where they destroy ozone, which protects us from ultraviolet radiation. The infrared spectrometer on Atmospheric Chemistry Experiment satellite measured spectra of particles "Black Summer" fires in Australia late 2019 early 2020, revealing that contain oxygenated organic functional groups water adsorption surfaces. These injected have produced unexpected extreme perturbations stratospheric gases beyond any seen previous 15 years measurements, including increases formaldehyde, chlorine nitrate, monoxide, hypochlorous acid decreases nitrogen dioxide, hydrochloric acid. composition potential to affect ozone chemistry ways.

Language: Английский

Citations

94

Chlorine activation and enhanced ozone depletion induced by wildfire aerosol DOI

Susan Solomon,

Kane A. Stone, Pengfei Yu

et al.

Nature, Journal Year: 2023, Volume and Issue: 615(7951), P. 259 - 264

Published: March 8, 2023

Language: Английский

Citations

81

Stratospheric ozone, UV radiation, and climate interactions DOI Creative Commons
G. Bernhard, Alkiviadis Bais, P. J. Aucamp

et al.

Photochemical & Photobiological Sciences, Journal Year: 2023, Volume and Issue: 22(5), P. 937 - 989

Published: April 21, 2023

This assessment provides a comprehensive update of the effects changes in stratospheric ozone and other factors (aerosols, surface reflectivity, solar activity, climate) on intensity ultraviolet (UV) radiation at Earth's surface. The is performed context Montreal Protocol Substances that Deplete Ozone Layer its Amendments Adjustments. Changes UV low- mid-latitudes (0-60°) during last 25 years have generally been small (e.g., typically less than 4% per decade, increasing some sites decreasing others) were mostly driven by cloud cover atmospheric aerosol content, caused partly climate change measures to control tropospheric pollution. Without Protocol, erythemal (sunburning) irradiance northern southern latitudes 50° would increased 10-20% between 1996 2020. For exceeding 50°, Index (UVI) surged 25% (year-round tip South America) more 100% (South Pole spring). Variability Antarctica was very large four years. In spring 2019, minimum historical (1991-2018) range Pole, while near record-high values observed 2020, which up 80% above mean. Arctic, highest irradiances record measured March April example monthly average UVI over site Canadian Arctic 70% higher (2005-2019) average, often this mean three standard deviations. Under presumption all countries will adhere future concentrations remain constant, (30-60°) projected decrease 2015 2090 2-5% north 4-6% south due recovering ozone. for tropics are ≤ 3%. However, industrial regions currently affected air pollution, increase as reduce pollutants gradually restore intensities those cleaner atmosphere. Since most substances controlled also greenhouse gases, phase-out these may avoided warming 0.5-1.0 °C mid-latitude continents, 1.0 Arctic; however, uncertainty calculations large. We assess climate, focusing poleward shift zones, discuss role Antarctic hole 2019 devastating "Black Summer" fires Australia. Additional topics include advances measuring modeling radiation; methods determining personal exposure; effect management (stratospheric injections) relevant plants; possible revisions vitamin D action spectrum, describes wavelength dependence synthesis previtamin

Language: Английский

Citations

70

Interactive effects of changes in UV radiation and climate on terrestrial ecosystems, biogeochemical cycles, and feedbacks to the climate system DOI Creative Commons
Paul W. Barnes,

T. Matthew Robson,

Richard G. Zepp

et al.

Photochemical & Photobiological Sciences, Journal Year: 2023, Volume and Issue: 22(5), P. 1049 - 1091

Published: Feb. 1, 2023

Terrestrial organisms and ecosystems are being exposed to new rapidly changing combinations of solar UV radiation other environmental factors because ongoing changes in stratospheric ozone climate. In this Quadrennial Assessment, we examine the interactive effects ozone, climate on terrestrial biogeochemical cycles context Montreal Protocol. We specifically assess organisms, agriculture food supply, biodiversity, ecosystem services feedbacks system. Emphasis is placed role extreme events altering exposure potential biodiversity. also address responses plants increased temporal variability radiation, change (e.g. drought, temperature) crops, driving breakdown organic matter from dead plant material (i.e. litter) biocides (pesticides herbicides). Our assessment indicates that interact various ways affect structure function ecosystems, by protecting layer, Protocol continues play a vital maintaining healthy, diverse land sustain life Earth. Furthermore, its Kigali Amendment mitigating some negative consequences limiting emissions greenhouse gases carbon sequestration vegetation pool.

Language: Английский

Citations

63

Understanding the critical elements of the pyrocumulonimbus storm sparked by high-intensity wildland fire DOI Creative Commons
Michael Fromm, R. Servranckx,

B. J. Stocks

et al.

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

Published: Oct. 17, 2022

Abstract High-intensity wildland fires can produce extreme flaming and smoke emissions that develop into a fire-cloud chimney, reaching the upper troposphere or lower stratosphere. Termed pyrocumulonimbus, these storms are both conventional counterintuitive. They have been observed to lightning, hail, downdraft wind hazards, tornadoes as expected with severe convective storms, but counterintuitively, they not associated significant precipitation. Pyrocumulonimbus noticed outside wildfire expert circles following Australia’s Black Summer in 2019/20, since repeatedly made headlines United States. However, much is unknown about their behavior, energetics, history, impact on Earth/atmosphere system. We address several questions science challenges related unknowns. Our worldwide record of pyrocumulonimbus events from 2013 2021 shows phenomenon neither new nor rare. Despite high occurrences 2019 2021, data do support identification trend. Future studies require an expansive occurrence globally regionally, historically continuously forward time.

Language: Английский

Citations

48

Radiative impacts of the Australian bushfires 2019–2020 – Part 1: Large-scale radiative forcing DOI Creative Commons
Pasquale Sellitto, Redha Belhadji, Corinna Kloss

et al.

Atmospheric chemistry and physics, Journal Year: 2022, Volume and Issue: 22(14), P. 9299 - 9311

Published: July 20, 2022

Abstract. As a consequence of extreme heat and drought, record-breaking wildfires developed ravaged south-eastern Australia during the fire season 2019–2020. The strength reached its paroxysmal phase at turn year During this phase, pyrocumulonimbus clouds (pyroCb) injected biomass burning aerosols gases into upper troposphere lower stratosphere (UTLS). UTLS aerosol layer was massively perturbed by these fires, with extinction increased factor 3 in visible spectral range Southern Hemisphere, respect to background atmosphere, stratospheric optical depth reaching values as large 0.015 February 2020. Using best available description event observations, we estimate radiative forcing (RF) such perturbations Hemispheric layer. We use offline transfer modelling driven observed information perturbation variability obtained from limb satellite measurements. Based on hypotheses absorptivity angular scattering properties layer, regional (at three latitude bands Hemisphere) clear-sky TOA (top-of-atmosphere) RF is found varying small positive relatively negative (up −2.0 W m−2), surface be consistently −4.5 m−2). argue that are unlikely for event, if ageing/mixing plume mirrored evolution properties. Our area-weighted global-equivalent -0.35±0.21 (TOA RF) -0.94±0.26 m−2 (surface RF), thus strongest documented comparable magnitude volcanic eruptions post-Pinatubo era. surplus surface, TOA, due absorption within has contributed generation ascending smoke vortices stratosphere. Highly reflective underlying surfaces, like clouds, can nevertheless swap RF, global average high +1.0 assuming highly absorbing particles.

Language: Английский

Citations

41

Climate Impacts and Potential Drivers of the Unprecedented Antarctic Ozone Holes of 2020 and 2021 DOI
Simchan Yook, David W. J. Thompson,

Susan Solomon

et al.

Geophysical Research Letters, Journal Year: 2022, Volume and Issue: 49(10)

Published: May 21, 2022

Abstract The latter months of 2020 and 2021 were marked by two the largest Antarctic ozone holes on record. That such large occurred despite ongoing recovery raises questions about their origins climate impacts. Here we provide novel evidence that supports hypothesis influenced distinct extraordinary events: Australian wildfires early eruption La Soufriere in 2021. We further reveal both associated with widespread changes Southern Hemisphere are consistent established impacts depletion, including a strengthening polar stratospheric vortex, enhanced surface westerlies over Ocean, temperature Antarctica Australia. results thus suggestive injections wildfire smoke volcanic emissions into stratosphere can lead to hemispheric‐scale climate.

Language: Английский

Citations

40

Can southern Australian rainfall decline be explained? A review of possible drivers DOI Creative Commons
Roseanna C. McKay, Ghyslaine Boschat, Irina Rudeva

et al.

Wiley Interdisciplinary Reviews Climate Change, Journal Year: 2023, Volume and Issue: 14(2)

Published: Jan. 20, 2023

Abstract Southern Australia's rainfall is highly variable and influenced by factors across scales from synoptic weather to large‐scale circulation remote climate modes of variability. Anthropogenic change natural variability modulate these their interactions. However, studies often focus on changes in selected parts the system with less emphasis as a whole. As such, it difficult gain complete understanding how southern responds broad‐scale system. We step through existing literature long‐term synoptic‐to‐large‐scale atmospheric drivers form more story Australia. This process reveals that most robust observed winter decline consistent several changing climatic factors: decreasing systems, strengthening subtropical ridge, poleward shifts Hadley Cell Annular Mode, increasing frequency positive Indian Ocean Dipole events. In other seasons, particularly summer, may not agree changes, highlighting gaps our knowledge dynamics processes. Future work should research temporal‐ spatial‐scales, better jet interactions, influence stratospheric processes troposphere, instances contrasting trends Australian changes. article categorized under: Paleoclimates Current Trends > Modern Climate Change Detection Attribution Assessing Impacts Observed

Language: Английский

Citations

37

Rapid ozone depletion after humidification of the stratosphere by the Hunga Tonga Eruption DOI
Stéphanie Evan, J. Brioude, K. H. Rosenlof

et al.

Science, Journal Year: 2023, Volume and Issue: 382(6668)

Published: Oct. 19, 2023

The eruption of the Hunga Tonga-Hunga Ha'apai volcano on 15 January 2022 offered a good opportunity to explore early impacts tropical volcanic eruptions stratospheric composition. Balloon-borne observations near Réunion Island revealed unprecedented amount water vapor injected by volcano. enhanced humidity, radiative cooling, and expanded aerosol surface area in plume created ideal conditions for swift ozone depletion 5% stratosphere just 1 week. decrease hydrogen chloride 0.4 parts per million volume (ppbv) increase chlorine monoxide ppbv provided compelling evidence activation within plume. This study enhances our understanding effect this unusual chemistry provides insights into possible changes that may occur changing climate.

Language: Английский

Citations

36

Tomographic Retrievals of Hunga Tonga‐Hunga Ha'apai Volcanic Aerosol DOI Creative Commons
Adam Bourassa, Daniel Zawada, Landon Rieger

et al.

Geophysical Research Letters, Journal Year: 2023, Volume and Issue: 50(3)

Published: Feb. 1, 2023

Abstract The 2022 eruption of the Hunga Tonga‐Hunga Ha'apai volcano caused substantial impacts on atmosphere, including a massive injection water vapor, and largest increase in stratospheric aerosol for 30 years. Ozone Mapping Profiler Suite (OMPS) Limb instrument has been critical monitoring amount spread volcanic stratosphere. We show that rapid imagery from OMPS enables tomographic retrieval extinction reduces bias up to factor two, improves vertical structure agreement with coincident lidar occultation observations. Due vertically thin heterogeneous nature aerosol, this integrated values across latitude, altitude, time several months. also investigate systematic impact uncertainty assumed particle size result an underestimation at peak layer.

Language: Английский

Citations

32