Atmospheric phenomena generally current an altered visible spectrum, dominated by darkish, sooty tones contrasted sharply with vibrant crimson hues. These occurrences usually end result from particular environmental circumstances, corresponding to volcanic ash dispersion, intensive wildfires releasing particulate matter, or distinctive interactions of daylight with aerosols within the higher environment. As an illustration, following important volcanic eruptions, advantageous ash particles suspended excessive within the air can selectively scatter daylight, resulting in the notion of darkened skies punctuated by deep crimson sunsets and sunrises.
The presence of such a dramatically coloured horizon can function a visible indicator of great environmental occasions and potential dangers to air high quality. Traditionally, these intense chromatic shows have been documented in reference to durations of main geological upheaval and large-scale conflagrations. Observations of those phenomena can present helpful knowledge for atmospheric scientists learning particle dispersion, radiative switch, and the general affect of such occasions on world local weather patterns. Moreover, analyzing the frequency and depth of those occasions helps to evaluate the well being of the environment.
Understanding the components that contribute to this uncommon celestial show is due to this fact essential. The rest of this text explores the precise causes, contributing atmospheric circumstances, and scientific significance behind this putting manifestation within the setting.
1. Volcanic ash
Volcanic ash is a big contributor to the phenomenon. Throughout explosive volcanic eruptions, huge portions of advantageous particulate matter, together with ash, are ejected into the environment. This ash can ascend to appreciable altitudes, generally reaching the stratosphere. The presence of such widespread ash clouds immediately impacts the transmission of daylight, ensuing within the attenuation of shorter wavelengths, corresponding to blue and inexperienced gentle, whereas permitting longer wavelengths, primarily crimson, to penetrate. This selective scattering and absorption result in a sky that seems darkened and reddened, creating the impact. The dimensions of the chromatic alteration depends upon the amount of ash emitted, its particle dimension distribution, and the altitude of the ash cloud.
A pertinent instance of this impact occurred following the eruption of Mount Pinatubo in 1991. The huge quantities of volcanic ash launched into the environment induced a world dimming impact and produced exceptionally vivid crimson sunsets and sunrises for a number of years. The ash acted as a scattering agent, preferentially diminishing blue gentle and permitting crimson gentle to dominate the visible spectrum. Moreover, the ash particles supplied surfaces for the condensation of sulfuric acid aerosols, which additional enhanced the scattering impact. This occasion underscored the power of volcanic ash to considerably alter the environment’s optical properties and produce dramatic visible results.
In abstract, volcanic ash is a main driver behind altered celestial appearances due to its capability to scatter and soak up daylight selectively. The magnitude of the chromatic alteration is immediately proportional to the size and depth of the volcanic occasion. Understanding the function of volcanic ash is essential for comprehending atmospheric optics and the potential environmental impacts of volcanic eruptions. Moreover, observing sky coloration can function a helpful, although oblique, technique of monitoring the dispersal of volcanic plumes and assessing potential aviation hazards.
2. Wildfire smoke
Wildfire smoke is a considerable contributor to the phenomenon, significantly in areas liable to seasonal wildfires. The smoke generated from burning vegetation incorporates a fancy combination of particulate matter, together with black carbon, natural carbon, and ash. These particles, sometimes smaller than these produced by volcanic eruptions, are extremely efficient at scattering and absorbing daylight. When wildfire smoke is current in ample concentrations, it may possibly attenuate the transmission of daylight, making a darkened impact. Concurrently, the crimson and orange wavelengths are much less vulnerable to scattering by these smaller particles, resulting in a sky dominated by these colours. The depth of the impact immediately correlates with the density of the smoke plume and the dimensions distribution of the particles inside it. A living proof is the intensive wildfires skilled in Australia through the 2019-2020 season. The smoke plumes from these fires traveled huge distances, darkening skies and producing vivid crimson sunsets in areas far faraway from the precise fires. This occasion served as a stark reminder of the wide-ranging atmospheric impacts of large-scale wildfires. Understanding this connection is essential for predicting air high quality impacts and issuing public well being advisories during times of intense wildfire exercise.
Additional evaluation reveals that the composition of wildfire smoke varies relying on the kind of vegetation being burned and the combustion circumstances. Incomplete combustion processes, widespread in wildfires, lead to the next proportion of black carbon particles, that are significantly efficient at absorbing daylight throughout all the spectrum. This absorption contributes to the general darkening impact whereas additionally influencing atmospheric heating and cloud formation processes. The presence of natural carbon particles, alternatively, can have an effect on the scattering of sunshine and the formation of secondary natural aerosols. Satellite tv for pc observations and ground-based measurements are essential for monitoring the distribution and composition of wildfire smoke plumes. These observations permit for the event of refined fashions that may predict the transport and dispersion of smoke, in addition to its affect on radiative switch and air high quality. For instance, devices corresponding to LIDAR (Mild Detection and Ranging) can present detailed vertical profiles of smoke plumes, enabling a greater understanding of their construction and evolution.
In conclusion, wildfire smoke performs a pivotal function in altering the colour of the sky on account of its composition and particle dimension distribution. The understanding of this connection has sensible implications for monitoring air high quality, predicting smoke transport, and issuing public well being alerts. Challenges stay in precisely characterizing the complicated chemical and bodily processes that happen inside wildfire smoke plumes, in addition to in predicting the long-term impacts of wildfire smoke on local weather and human well being. Continued analysis and monitoring efforts are important for mitigating the antagonistic results of wildfires on the setting and society.
3. Rayleigh scattering
Rayleigh scattering, whereas a basic atmospheric course of, doesn’t immediately trigger a “black” sky. As a substitute, it’s primarily liable for the blue coloration of the sky below regular circumstances. Rayleigh scattering happens when electromagnetic radiation, corresponding to daylight, is scattered by particles of a a lot smaller wavelength. In Earth’s environment, these particles are primarily nitrogen and oxygen molecules. As a result of the scattering effectivity is inversely proportional to the fourth energy of the wavelength, shorter wavelengths (blue and violet) are scattered way more successfully than longer wavelengths (crimson and orange). This explains why we understand the sky as blue. Subsequently, the presence of a darkish or blackened sky signifies a disruption of regular Rayleigh scattering processes, sometimes attributable to the presence of bigger particles, corresponding to these present in volcanic ash or wildfire smoke. These bigger particles interact in Mie scattering, which is much less wavelength-dependent and scatters gentle extra evenly, resulting in a discount within the depth of blue gentle and an total darkening impact. The simultaneous presence of crimson hues implies that these bigger particles are selectively absorbing or scattering shorter wavelengths, permitting crimson gentle to dominate the visible spectrum.
The importance of Rayleigh scattering as a element of the usual atmospheric gentle regime underscores its absence or modification in conditions exhibiting uncommon coloration. As an illustration, during times of intense volcanic exercise or widespread wildfires, the abundance of particulate matter overwhelms the consequences of Rayleigh scattering. Actual-world examples abound: the darkened skies noticed after main volcanic eruptions, corresponding to Mount Pinatubo in 1991, illustrate the diminished function of Rayleigh scattering because of the dominance of ash particles. Equally, the reddish skies seen throughout extreme wildfires, as skilled in Australia in 2019-2020 and the Western United States, spotlight the affect of smoke aerosols on gentle scattering. In these cases, the particulate matter not solely reduces the depth of the blue gentle scattered by air molecules but additionally selectively absorbs or scatters it, permitting redder wavelengths to change into extra distinguished. Thus, fairly than contributing to a “black and crimson sky,” Rayleigh scattering is successfully suppressed or masked by different scattering mechanisms.
In conclusion, whereas Rayleigh scattering is crucial for the blue coloration of the sky below regular circumstances, it doesn’t immediately contribute to a “black and crimson sky.” The presence of darkened and reddish skies signifies a shift within the dominant scattering mechanisms, sometimes because of the introduction of bigger particulate matter from volcanic eruptions or wildfires. Understanding the interaction between Rayleigh scattering, Mie scattering, and absorption processes is essential for decoding atmospheric optical phenomena and assessing the environmental impacts of such occasions. Challenges stay in precisely modeling the complicated interactions of sunshine with numerous atmospheric aerosols and in predicting the visible results of large-scale environmental occasions.
4. Aerosol focus
The focus of aerosols within the environment is a main determinant within the prevalence of considerably altered sky coloration. Aerosols, outlined as suspensions of advantageous stable particles or liquid droplets within the air, affect the scattering and absorption of daylight. When aerosol concentrations are elevated, significantly on account of occasions corresponding to volcanic eruptions, wildfires, or industrial air pollution, the conventional processes of atmospheric gentle scattering are disrupted. Elevated aerosol loading can result in the attenuation of shorter wavelengths of sunshine, corresponding to blue and inexperienced, whereas permitting longer wavelengths, notably crimson, to dominate. This preferential scattering and absorption end result within the commentary of a darkened sky punctuated by crimson or orange hues. A direct instance is the commentary of vividly coloured sunsets after main volcanic eruptions, whereby the dispersal of volcanic ash aerosols results in considerably enhanced scattering of crimson gentle. Equally, excessive aerosol concentrations from industrial smog in closely polluted areas can produce comparable results, albeit usually with a brownish or greyish forged along with the crimson tones.
Additional examination reveals that the precise composition, dimension, and refractive index of the aerosols current play an important function within the noticed optical results. Bigger aerosol particles, for example, are likely to scatter gentle extra uniformly throughout the spectrum, resulting in a common discount in sky brightness. Nonetheless, smaller particles exhibit higher selectivity of their scattering habits, enhancing the prominence of crimson wavelengths. The interaction between aerosol focus, composition, and particle dimension distribution determines the general coloration and depth of the altered sky. Sensible functions of this understanding prolong to distant sensing and air high quality monitoring. By analyzing the spectral traits of scattered daylight, scientists can infer details about aerosol concentrations and properties. This info is essential for assessing air high quality, monitoring the dispersion of pollution, and understanding the radiative results of aerosols on local weather. For instance, satellite-based devices such because the Aerosol Robotic Community (AERONET) measure the aerosol optical depth and different parameters, offering helpful knowledge for atmospheric analysis and environmental administration.
In abstract, aerosol focus is a essential issue driving the formation of a phenomenon. Elevated aerosol ranges, usually related to particular environmental occasions, disrupt regular gentle scattering processes, resulting in the attenuation of shorter wavelengths and the improved visibility of crimson and orange wavelengths. This understanding has sensible implications for air high quality monitoring, distant sensing, and local weather modeling. Challenges stay in precisely characterizing the complicated interactions of sunshine with numerous aerosol sorts and in predicting the long-term impacts of aerosol emissions on atmospheric optics and local weather. Continued analysis and monitoring efforts are important for mitigating the antagonistic results of aerosol air pollution and for enhancing our understanding of atmospheric processes.
5. Atmospheric absorption
Atmospheric absorption performs a big, although usually oblique, function within the formation of dramatic coloration. Absorption refers back to the course of by which sure gases and particles within the environment take away particular wavelengths of sunshine from the photo voltaic spectrum. Whereas scattering is often the dominant consider sky coloration, absorption contributes by selectively diminishing sure wavelengths, thereby influencing the ultimate perceived coloration.
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Ozone Absorption
Ozone (O3) primarily absorbs ultraviolet (UV) radiation, and to a lesser extent, some seen gentle. Whereas indirectly liable for making the sky seem black or crimson, ozone absorption reduces the general depth of sunshine reaching the decrease environment. This discount not directly enhances the distinction of different colours. Throughout circumstances the place particulate matter is excessive, corresponding to after volcanic eruptions or throughout wildfires, ozone absorption can subtly contribute to the general darkening of the sky by lowering the quantity of scattered blue gentle, which is often considerable.
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Water Vapor Absorption
Water vapor (H2O) absorbs infrared radiation, but it surely additionally has some absorption bands within the seen spectrum, significantly within the crimson and yellow parts. Elevated water vapor within the environment can result in a slight discount within the depth of those colours. Nonetheless, the first impact of water vapor is its function in cloud formation, which might each scatter and soak up daylight. In eventualities that produce “black and crimson sky,” water vapor might contribute to the general dimming if cloud cowl is current, additional lowering the quantity of accessible gentle for scattering.
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Aerosol Absorption
Aerosols, corresponding to black carbon from wildfires and mud particles from desert storms, are efficient absorbers of daylight throughout a broad spectrum. Black carbon, specifically, strongly absorbs seen gentle, together with each blue and crimson wavelengths. Excessive concentrations of absorbing aerosols can darken the sky, contributing to a “black” look. Concurrently, if different aerosols or scattering results are current, the remaining gentle could also be predominantly crimson, resulting in the attribute coloring. An instance consists of mud storms that carry iron oxide particles, which soak up blue gentle extra effectively, leading to reddish-brown skies.
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Nitrogen Dioxide Absorption
Nitrogen dioxide (NO2), a pollutant produced by combustion processes, absorbs blue gentle. Elevated ranges of NO2 can contribute to a yellowish or reddish coloration of the sky, significantly in city environments. Whereas NO2 is never current in concentrations excessive sufficient to create a very black sky, it may possibly improve the reddish hues by selectively absorbing blue gentle. This impact is extra noticeable in polluted areas throughout sundown when the trail size of daylight by means of the environment is longer, growing the quantity of absorption.
In abstract, whereas atmospheric absorption alone is unlikely to supply the phenomenon, it performs a modifying function by selectively lowering the depth of sure wavelengths. The interaction between absorption and scattering, significantly by aerosols and particulate matter, determines the ultimate perceived coloration. Understanding the contribution of atmospheric absorption is essential for precisely modeling atmospheric radiative switch and decoding observations.
6. Particulate matter
Particulate matter constitutes a essential element within the formation of dramatically altered atmospheric coloration. Consisting of microscopic stable or liquid particles suspended within the air, its presence and traits considerably affect the scattering and absorption of daylight, thereby modifying the perceived coloration of the sky.
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Focus and Opacity
Elevated concentrations of particulate matter, corresponding to these ensuing from volcanic eruptions, wildfires, or industrial emissions, improve the opacity of the environment. This elevated opacity reduces the transmission of daylight, inflicting a darkening impact. When the focus of particles is sufficiently excessive, the sky might seem black or considerably darkened because of the total discount in gentle reaching the observer. For instance, throughout intense mud storms or following large-scale industrial accidents, visibility may be severely restricted, resulting in a darkish or black sky.
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Selective Mild Scattering
The scale and composition of particulate matter affect the scattering of various wavelengths of sunshine. Smaller particles, corresponding to these present in wildfire smoke, are likely to scatter shorter wavelengths (blue gentle) extra effectively, whereas bigger particles scatter gentle extra uniformly. When particular varieties of particulate matter are current, corresponding to soot or black carbon, they soak up sure wavelengths of sunshine extra readily. In eventualities characterised by coloration, these particles usually selectively soak up or scatter blue and inexperienced gentle, permitting longer wavelengths, corresponding to crimson and orange, to dominate the visible spectrum.
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Composition and Coloration
The chemical composition of particulate matter immediately impacts its light-absorbing and scattering properties, thereby influencing the ensuing coloration. As an illustration, iron oxide particles, generally present in desert mud, soak up blue gentle and scatter crimson gentle, contributing to reddish or brownish skies throughout mud storms. Black carbon, produced throughout incomplete combustion, strongly absorbs gentle throughout the seen spectrum, resulting in a darkening impact. The presence of sulfates and nitrates, usually shaped from industrial emissions, can scatter gentle and improve the general brightness of the sky. Nonetheless, if these compounds are mixed with absorbing aerosols, they’ll additionally contribute to a darkened impact.
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Aerosol Layers and Altitude
The vertical distribution of particulate matter within the environment impacts the looks. Excessive-altitude aerosol layers, corresponding to these shaped by volcanic ash or smoke plumes, can work together with daylight at completely different angles, influencing the colours noticed throughout dawn and sundown. When the solar is low on the horizon, its gentle travels by means of an extended path within the environment, growing the scattering and absorption by particulate matter. This impact can improve the crimson and orange hues, significantly when mixed with excessive concentrations of aerosols at particular altitudes. Satellite tv for pc measurements and atmospheric fashions are essential for monitoring the distribution and properties of aerosol layers, enabling a greater understanding of their affect on atmospheric optics.
The mixed results of focus, selective scattering, composition, and vertical distribution contribute to the formation. Analyzing these components is crucial for understanding the precise mechanisms behind altered atmospheric coloration and assessing the potential impacts on air high quality, local weather, and human well being.
7. Solar angle
The angle of the solar above the horizon exerts a big affect on the perceived coloration of the sky, significantly in contexts involving elevated ranges of atmospheric particulate matter. When the solar is low on the horizon, corresponding to throughout dawn and sundown, daylight traverses a considerably longer path by means of the environment in comparison with noon. This prolonged path size will increase the likelihood of scattering and absorption of sunshine by atmospheric constituents, together with aerosols and fuel molecules. The resultant impact is a selective depletion of shorter wavelengths (blue and inexperienced gentle) on account of elevated scattering, whereas longer wavelengths (crimson and orange gentle) are much less affected and thus change into extra dominant. Consequently, the presence of a excessive focus of particulate matter, corresponding to volcanic ash or wildfire smoke, additional intensifies the preferential scattering and absorption, resulting in a markedly altered chromatic show. The looks of the darkened sky together with vividly saturated crimson and orange hues is, due to this fact, extremely depending on the solar’s place relative to the horizon.
Additional evaluation reveals that the precise scattering and absorption processes are contingent upon the composition and dimension distribution of the particulate matter current. Bigger particles are likely to scatter gentle extra uniformly, resulting in a common discount in sky brightness. Nonetheless, smaller particles, corresponding to these produced by wildfires, are extra environment friendly at scattering shorter wavelengths, thereby enhancing the redness of the sky when mixed with a low solar angle. The altitude of the particulate matter layer additionally performs an important function. Excessive-altitude aerosol layers work together with daylight in a different way than ground-level aerosols, contributing to variations within the noticed sky coloration. Actual-world examples, corresponding to the extreme crimson sunsets noticed after main volcanic eruptions or during times of intensive wildfires, underscore the importance of this relationship. The eruption of Mount Pinatubo in 1991 and the Australian bushfires of 2019-2020 are notable cases the place the mix of excessive aerosol loading and low solar angle resulted in exceptionally vivid and extended atmospheric coloration.
In abstract, the solar’s angle is a essential consider influencing atmospheric coloration, significantly within the presence of particulate matter. A low solar angle will increase the trail size of daylight by means of the environment, enhancing scattering and absorption processes. This impact, when mixed with elevated aerosol concentrations, results in the preferential scattering and absorption of shorter wavelengths, ensuing within the attribute phenomenon. Understanding this interaction is essential for decoding atmospheric optical phenomena and assessing the impacts of particulate matter on local weather and air high quality. Ongoing analysis and monitoring efforts are important for enhancing the accuracy of atmospheric fashions and predicting the consequences of environmental occasions on the Earth’s environment.
Regularly Requested Questions About Altered Atmospheric Coloration
The next part addresses widespread inquiries relating to atmospheric phenomena characterised by darkish, and intensely coloured skies. These solutions present a factual and scientific perspective on the causes and implications of those occasions.
Query 1: What main components contribute to the manifestation of a darkened sky contrasted by crimson and orange hues?
Elevated concentrations of particulate matter, corresponding to volcanic ash, wildfire smoke, or industrial pollution, are the first drivers. These particles scatter and soak up daylight selectively, attenuating shorter wavelengths (blue gentle) whereas permitting longer wavelengths (crimson and orange gentle) to dominate.
Query 2: Is there a correlation between this altered coloration and environmental occasions?
A powerful correlation exists. Observations are ceaselessly related to important environmental occasions, together with volcanic eruptions, intensive wildfires, mud storms, and industrial accidents that launch substantial quantities of particulate matter into the environment.
Query 3: Can the phenomenon function an indicator of air high quality?
Sure. The presence of such altered coloration might function a visible indicator of decreased air high quality and potential well being hazards. The depth and length can present a qualitative evaluation of the severity and extent of atmospheric air pollution.
Query 4: What function does the solar’s angle play in these visible shows?
The solar’s angle considerably influences the perceived coloration. When the solar is low on the horizon (dawn or sundown), daylight traverses an extended path by means of the environment, growing scattering and absorption. This impact intensifies the crimson and orange hues.
Query 5: Are there potential aviation hazards related to these circumstances?
Sure, volcanic ash and dense smoke plumes can pose important aviation hazards. These particles can harm plane engines and scale back visibility. Airspace closures and rerouting of flights could also be needed in affected areas.
Query 6: How are these occasions monitored and tracked?
Monitoring is completed by means of a mixture of satellite tv for pc observations, ground-based measurements, and atmospheric modeling. Satellite tv for pc devices, corresponding to these on climate satellites and specialised aerosol monitoring platforms, present knowledge on aerosol concentrations and distribution. Floor-based networks, like AERONET, provide detailed measurements of aerosol optical properties.
Understanding the interaction of atmospheric processes and environmental occasions is essential for decoding uncommon celestial shows and assessing their potential impacts on the setting and human well being.
The next part gives actionable methods for understanding the implications.
Navigating Eventualities Involving a Strikingly Coloured Horizon
When confronted with atmospheric circumstances characterised by a darkened celestial vista contrasted with crimson or orange hues, adherence to particular pointers is advisable to make sure security and facilitate knowledgeable decision-making.
Tip 1: Confirm Environmental Reviews: Cross-reference visible observations with official reviews from environmental companies. Sources such because the Environmental Safety Company (EPA), the World Meteorological Group (WMO), and native air high quality monitoring stations present validated knowledge on atmospheric circumstances.
Tip 2: Assess Air High quality Indices: Seek the advice of real-time air high quality indices (AQI) to find out the extent of air pollution. Excessive AQI values point out elevated concentrations of particulate matter and potential respiratory hazards. Public well being advisories issued by native authorities must be heeded.
Tip 3: Monitor Volcanic Exercise: If volcanic exercise is suspected, seek the advice of reviews from america Geological Survey (USGS) or equal geological companies. These reviews present info on eruption standing, ash cloud trajectories, and potential hazards to aviation.
Tip 4: Consider Wildfire Circumstances: Assess wildfire circumstances utilizing assets such because the Nationwide Interagency Fireplace Middle (NIFC) or native fireplace departments. Info on lively fires, smoke plume forecasts, and evacuation orders can inform selections relating to out of doors actions and potential relocation.
Tip 5: Implement Respiratory Safety: In areas with compromised air high quality, make the most of applicable respiratory safety. N95 or higher-rated masks can filter out a big share of airborne particles, lowering the chance of respiratory irritation and well being problems.
Tip 6: Restrict Outside Publicity: Reduce extended out of doors actions during times of elevated particulate matter. Indoor environments provide a level of safety from airborne pollution. Recirculating air by means of HEPA filters can additional enhance indoor air high quality.
Tip 7: Defend Aviation Operations: Adhere to aviation security protocols and pointers. Volcanic ash and dense smoke plumes pose important dangers to plane. Seek the advice of aviation climate forecasts and observe directives from air site visitors management.
Constant utility of those methods ensures a measured and pragmatic strategy to navigating occasions involving visibly altered skies. By combining direct commentary with credible knowledge sources, a extra complete understanding of the underlying circumstances and potential hazards is achieved.
The following part gives a conclusion that integrates key elements of the atmospheric phenomena.
Conclusion
The previous exploration of “black and crimson sky” has illuminated the complicated interaction of atmospheric constituents and environmental occasions liable for this putting visible phenomenon. Elevated concentrations of particulate matter, usually originating from volcanic eruptions or wildfires, function the first drivers, selectively scattering and absorbing daylight to supply the attribute chromatic alteration. The solar’s angle, aerosol composition, and atmospheric absorption additional modulate the depth and spectral traits of the show. Understanding these components is essential for decoding the visible cues and assessing potential environmental and well being implications.
The prevalence of a darkened horizon punctuated by crimson and orange hues serves as a potent reminder of the dynamic nature of Earth’s environment and the profound affect of environmental perturbations. Continued analysis and monitoring efforts are important for refining our understanding of those phenomena and for growing methods to mitigate the related dangers. Vigilance, knowledgeable decision-making, and adherence to public well being pointers stay paramount when encountering such visually arresting, but probably hazardous, atmospheric circumstances.
