Related Experiment Video
Updated: Sep 30, 2025

08:17
Generation of a Chronic Obstructive Pulmonary Disease Model in Mice by Repeated Ozone Exposure
Published on: August 25, 2017
11.1K
Wildfire smoke destroys stratospheric ozone
Peter Bernath1,2,3, Chris Boone2, Jeff Crouse2
1Department of Chemistry and Biochemistry, Old Dominion University, Norfolk, VA, USA.
Summary
Large Australian wildfires sent smoke into the stratosphere, damaging ozone. The Atmospheric Chemistry Experiment satellite found smoke particles altered stratospheric gases, impacting ozone chemistry.
Area of Science:
- Atmospheric Chemistry
- Stratospheric Science
- Wildfire Smoke Impacts
Background:
- Large wildfires release smoke and biomass-burning products into the stratosphere.
- Stratospheric ozone protects Earth from harmful ultraviolet radiation.
- Previous understanding of wildfire smoke's stratospheric impact was limited.
Purpose of the Study:
- To analyze the composition of smoke particles from Australia's "Black Summer" fires.
- To investigate the impact of these smoke particles on stratospheric gas composition.
- To understand the potential effects on ozone chemistry.
Main Methods:
- Utilized the infrared spectrometer on the Atmospheric Chemistry Experiment (ACE) satellite.
- Measured spectra of smoke particles injected into the stratosphere.
- Analyzed changes in various stratospheric gases following smoke injection.
Main Results:
- Smoke particles contained oxygenated organic functional groups and adsorbed water.
- Observed unprecedented perturbations in stratospheric gases, including increases in formaldehyde, chlorine nitrate, chlorine monoxide, and hypochlorous acid.
- Measured significant decreases in ozone, nitrogen dioxide, and hydrochloric acid.
Conclusions:
- Wildfire smoke significantly alters stratospheric composition.
- These alterations have led to extreme and unexpected changes in key stratospheric gases.
- The observed perturbations pose potential risks to stratospheric ozone and chemistry.
Related Concept Videos
Global Climate Change
24.9K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.9K
Mutations
40.8K
Mutations are changes in the sequence of DNA. These changes can occur spontaneously or they can be induced by exposure to environmental factors. Mutations can be characterized in a number of different ways: whether and how they alter the amino acid sequence of the protein, whether they occur over a small or large area of DNA, and whether they occur in somatic cells or germline cells.
Chromosomal Alterations Are Large-Scale Mutations
While point mutations are changes in a single nucleotide in...
Chromosomal Alterations Are Large-Scale Mutations
While point mutations are changes in a single nucleotide in...
40.8K
Threats to Biodiversity
23.1K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
23.1K
Oxidative Cleavage of Alkenes: Ozonolysis
11.3K
In ozonolysis, ozone is used to cleave a carbon–carbon double bond to form aldehydes and ketones, or carboxylic acids, depending on the work-up.
Ozone is a symmetrical bent molecule stabilized by a resonance structure.
Ozone is a symmetrical bent molecule stabilized by a resonance structure.
11.3K
Chronic Obstructive Pulmonary Disease-II: Pathophysiology
3.2K
Chronic Obstructive Pulmonary Disease (COPD) pathophysiology is intricate and multifaceted, involving a complex interplay of physiological processes. Understanding these mechanisms is crucial for effectively managing and treating COPD. Here is an in-depth look at the critical elements in the pathophysiology of COPD:
Chronic Inflammation
Chronic Inflammation
3.2K
Radical Autoxidation
2.4K
The oxidation of an organic compound in the presence of air or oxygen is called autoxidation. For example, cumene reacts with oxygen to form hydroperoxide. Autoxidation involves initiation, propagation, and termination steps. Many organic compounds are susceptible to autoxidation—especially ethers in the presence of oxygen, which form hydroperoxides. Even though this reaction is slow, old ether bottles contain small amounts of peroxide, which leads to laboratory explosions during ether...
2.4K

