Research shows strong Midwest summer storms can puncture the stratosphere, bringing aerosols and burning biomass from western wildfires. This could affect the ozone layer's stability and warm the stratosphere.
A new study reveals how variations in the stratospheric polar vortex affect where and when extreme cold hits, with a focus on the northwestern US. The research finds two distinct patterns that steer Arctic air into different areas, leading to colder winters in regions like Montana and Texas.
Researchers have discovered that urban areas experience a greater difference in wet bulb globe temperature between 0.5 m and 1.5 m above ground due to surface heat radiation, posing health risks to children and pets during extreme heat events. Total solar eclipses also alter atmospheric conditions and insect behavior, with some species...
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A new study suggests that adding particles to the atmosphere at a lower altitude near the polar regions can effectively cool the planet. Commercial jets like Boeing 777F could reach this altitude.
A new UCLA-led study reveals that the Hunga Tonga-Hunga Haʻapai volcano eruption in 2022 actually cooled the Southern Hemisphere by 0.1 C due to the formation of smaller sulfate aerosols. This effect was more significant than initially thought and challenges geoengineering efforts to combat climate change.
Scientists have identified a new reason for UK winter storm clusters, pointing to stronger winds in the Arctic stratosphere. This research reveals that an intense swirling vortex of winds miles above the Arctic can make severe winter storms more likely, and may offer early warnings for forecasters up to a month before they happen.
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Climate change drives large increases in electricity demand and costs in Texas due to extreme temperatures. Meanwhile, atmospheric rivers become more frequent, larger, and moister globally. Diagnostic studies also predict malaria outbreaks with five-month lead time using sea-surface temperature anomalies.
A new study reveals that atmospheric gravity waves play a crucial role in driving latitudinal air currents on Mars, particularly at high altitudes. The findings suggest fundamental differences from Earth's middle atmosphere.
A new study by MIT confirms the Antarctic ozone layer is healing, with high statistical confidence that reductions in CFCs are the primary cause. The research uses fingerprinting to isolate the anthropogenic signal and rule out natural variability.
The Amazon rainforest is a significant source of condensation nuclei for clouds, according to two studies. The rainforest's plant transpiration and thunderstorms produce aerosol particles that can be transported thousands of kilometers, influencing marine cloud formation.
The USTC team found that positive NBEs occur during convective uplift, while negative NBEs occur during downdraft phase. This discovery suggests a new model where convection modulates charged layers within the cloud, governing cloud-top discharge intensity.
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A team of geoscientists has identified the origin of the massive asteroid that wiped out 70% of Earth's species 66 million years ago. The study found the asteroid was a carbonaceous-type asteroid that formed outside Jupiter's orbit.
MIT researchers detected a clear signal of human influence on upper tropospheric ozone trends, separate from climate noise. The study provides insights into specific human activities driving this trend.
A new study published by Texas A&M University researchers found that the Hunga Tonga volcano eruption did not contribute to global warming as initially thought. Instead, the eruption resulted in more energy leaving the climate system than entering it, leading to a slight cooling effect.
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Researchers at Washington University in St. Louis have found a new mechanism that produces a significant amount of particles in the Earth's atmosphere, which could impact climate change and weather patterns. The discovery suggests that stratospheric air intrusions play a crucial role in forming these particles.
The University of Washington's STRIVE project aims to understand the troposphere and stratosphere, where the ozone layer resides, and their interface. This will help monitor changes in the ozone layer, air quality, and climate processes.
A new study reveals that microplastic fibers settle substantially slower than spherical particles in the atmosphere, allowing them to reach remote regions such as Arctic glaciers. The research suggests that these fibers could even reach the stratosphere, with potential implications for cloud processes and ozone depletion.
The study found that the eruption changed the chemistry and dynamics of the stratosphere, leading to unprecedented losses in the ozone layer. The injection of water vapor and sulfur dioxide increased sulfate aerosols, which drove changes in temperature and circulation, resulting in decreased ozone levels in the Southern Hemisphere.
A University of Oklahoma-led study highlights newly measured extremes in stratospheric water vapor recorded during the DCOTSS field project. High-level thunderstorms enhance water vapor in the stratosphere at levels higher than previously understood.
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Researchers at Purdue University detect unprecedented levels of alloy aerosols in the atmosphere, likely from spacecraft and satellites. The team found that nearly 10% of large sulfuric acid particles contained aluminum and other spacecraft metals.
An international team has detected aerosols from the Hunga Tonga eruption in the Northern Hemisphere stratospheric westerlies, aiding simulation of volcanic plume processes. This discovery provides key insights into physical properties and evolutionary process of volcanic aerosols in the stratosphere.
A new MIT study reveals that smoke particles from Australian wildfires can trigger chemical reactions that erode the protective ozone layer. The research found a 3-5% depletion of total ozone at mid-latitudes and widened the Antarctic ozone hole by 10% in 2020.
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A study found that a northward position of North Pacific sea surface temperature anomalies weakens the Arctic stratospheric polar vortex. This weakening can lead to Eurasian cooling and negative surface temperature anomalies.
Researchers used the parallax effect to measure the height of the volcano's plume, reaching an altitude of 57 km, surpassing previous records. The study provides new insights into volcanic eruptions and their impact on the climate.
A study published in Scientific Reports found that Australian bushfires contributed to the highest recorded temperature in the lower stratosphere since the early 1990s. The smoke aerosols emitted by the fires led to a significant increase in stratospheric temperatures, with a modelled temperature spike of around 0.65 degrees Celsius.
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Researchers led by Cornell University are evaluating the potential of making the stratosphere 'brighter' to cool the Earth. They use geoengineering simulations to assess the impact of injecting sulfate aerosols, a known pollutant, on climate change mitigation strategies.
Researchers found a correlation between Arctic ozone depletion and extreme weather events in the Northern Hemisphere. Simulations suggest that reduced ozone levels contribute to warmer temperatures and droughts in central Europe, while wet conditions prevail in polar regions.
A large, all-season ozone hole has been detected over tropical regions, with an area seven times greater than the Antarctic ozone hole. The discovery highlights the need for further research on ozone depletion and its impact on human health and ecosystems.
Researchers verified the existence of an atmospheric acoustic duct using rocket launch data. Infrasound signals were detected within the duct, related to a Blue Origin rocket launch in April 2021. The duct may channel a variety of natural and anthropogenic sounds, including signals from earthquakes and ground explosions.
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Research reveals that tropospheric ozone contributes more to the Southern Ocean's warming than previously thought. This finding highlights the importance of reducing air pollution to mitigate ocean heat uptake and climate change.
A new study reveals that smoke from major wildfires can destroy atmospheric ozone in the Southern Hemisphere for months. Researchers warn that more frequent wildfires with a changing climate will lead to increased damage and exposure to harmful ultraviolet radiation.
A new study questions a widely-held theory that sudden stratospheric warming caused the extreme cold weather in Texas and other parts of the US. The research suggests that the polar vortex's disruption, which occurred six weeks after the initial warming event, was not significant enough to impact the weather.
Researchers found a chemical link between wildfire smoke and ozone depletion, which may stall ozone recovery for years. The study discovered that the smoke from Australian wildfires in 2019-2020 depleted ozone by 1%, highlighting the potential impact of future, more frequent fires.
A new study from UC Berkeley suggests that copper in soil and seawater acts as a catalyst for producing two potent halocarbon compounds that destroy ozone. The compounds, methyl bromide and methyl chloride, are major contributors to stratospheric ozone depletion and have puzzled scientists for over 20 years.
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A new study suggests that atmospheric conditions in the stratosphere pose a challenge to generating sulfuric acid, a crucial component of a proposed geoengineering strategy to mitigate climate change. Researchers found that solar radiation causes HOSO2 to quickly photolyse, breaking it down into harmful sulfur dioxide, which may reduce...
Researchers at Stanford University have discovered the physical mechanism behind icy plumes that precede severe thunderstorms and potentially deadly tornadoes. The study reveals a hydraulic jump phenomenon triggered by fluid obstacles in the atmosphere, leading to rapid water vapor injection into the stratosphere.
Climatologists tested a solar geoengineering scenario using the MAR climate model to reduce Greenland's mass loss by 6% locally. However, the researchers warn that this approach is not sufficient to stabilize the ice cap by the end of the century and poses risks to the ozone layer and water cycles.
Australian wildfires injected massive amounts of smoke into the stratosphere, causing record-breaking levels of atmospheric aerosols in the Southern Hemisphere. The effect was comparable to that of a moderate volcanic eruption and caused significant cooling over cloud-free ocean regions.
Researchers at NASA and German Aerospace Center sent microbes to Earth's stratosphere, replicating Martian conditions, to test their endurance. The study found that some microorganisms, such as spores from the black mold fungus, could survive high UV radiation and desiccation during space travel.
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A global team of researchers found a record-setting smoke cloud from Australian wildfires that measured 1,000 kilometers across and remained intact for three months. The team's findings provide critical information on the impact of wildfires on the Earth's atmosphere, which is expected to increase due to climate change.
Researchers developed a balloon-based system to study stratospheric radiation over the Tibetan Plateau, providing in situ measurements for the first time. The data helps understand radiation variations and thermal conditions associated with clouds and aerosols during the Asian summer monsoon period.
Researchers detected inorganic iodine in the stratosphere at a concentration of 0.77 parts per trillion by volume, suggesting it plays a crucial role in ozone depletion. Iodine emissions from humans may increase particle formation and continue to affect stratospheric ozone levels.
A new study has quantified small levels of iodine in the stratosphere and links it to ozone layer decline. The research suggests that air pollution from the surface can trigger ozone destruction higher in the atmosphere.
Scientists studied a massive wildfire smoke plume that lasted for nearly nine months, providing an ideal opportunity to test climate models. The findings show that black carbon was key to the plume's rapid rise and persistence, challenging previous nuclear winter studies.
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Researchers compared observations with model simulations, revealing gaps in smoke plume rise and duration modeling. The study found that solar heating warmed air within the plume, causing it to self-loft to nearly 23 kilometers, but observed smoke lifetime was 40% shorter than calculated models due to photochemical loss of organic carbon.
A new study suggests that super volcanic eruptions could significantly impact ozone layer recovery, with estimated depletions ranging from 2.5% to 6.4%. The research used transport and chemistry-climate models to simulate the effects of super volcanoes on stratospheric ozone during different recovery periods.
The Manaro Voui volcano in Vanuatu released the largest amount of sulfur dioxide in 2018, with 400k tons during its most active phase in July. The eruption had devastating effects, including acid rain and destruction of homes.
Researchers found that extratropical eruptions produce strong hemispheric cooling in proportion to their sulfur release, contrary to the assumed weaker impact. This study sheds light on the importance of injection height and helps quantify volcanic eruptions' past climate variability effects.
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A new MIT study identifies chloroform as a significant threat to ozone layer recovery, with increased emissions in East Asia potentially delaying the process by four to eight years. The researchers found that production of products from chloroform is on the rise in the region, contributing to the growing problem.
Cameron R. Homeyer, a University of Oklahoma meteorologist, will lead a $30 million NASA-funded project to investigate the impact of summer storms on the stratosphere's chemistry. The five-year project aims to understand how these storms affect ozone depletion and the potential for increased water in the stratosphere.
Researchers from Texas A&M and Harvard will investigate the impact of strong summertime convective storms on the stratosphere, collecting data from a high-altitude NASA aircraft. The study aims to understand how these storms can change the chemistry of the lower stratosphere, potentially affecting ozone levels.
The ozone layer has continued to decline in the lower stratosphere, contrary to expectations that it would have recovered by the middle of the century. Satellite measurements show a decrease in ozone concentrations at latitudes between 60° S and 60° N since the Montreal Protocol banned ozone-depleting substances in 1989.
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Global ozone decline since the 1970s persists, with unexpected decreases in lower stratosphere preventing recovery at lower latitudes. Scientists point to climate change and short-lived substances as potential causes.
A NASA-led team has identified that gravity waves are the primary driver of Jupiter's equatorial jet stream's reversal, with convection in the lower atmosphere producing waves that travel up to the stratosphere. The findings could help scientists better understand the dynamic atmosphere of Jupiter and other planets.
Long-lasting compounds still dominate the outlook for ozone recovery, despite regulations by the Montreal Protocol. Short-lived compounds from human sources are expected to have minimal impact on ozone recovery due to their short lifetimes.
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The oversized planet WASP-18b is wrapped in a smothering stratosphere loaded with carbon monoxide and devoid of water. The formation of this atmosphere is attributed to 'sunscreen'-like molecules absorbing UV radiation and releasing heat, which is unusual compared to other gas giants.
A recent study reveals that high-latitude volcanic eruptions can transport sulfate aerosols into the tropical stratosphere, influencing both hemispheres' climates. The research found that favorable atmospheric conditions can enable such long-distance transport, making these eruptions a global concern.
Researchers used a new model to simulate atmospheric conditions in three dimensions, revealing a key role for stellar radiation in creating moist greenhouse states on exoplanets. This process could make planets closer to their stars habitable despite intense radiation and tidal forces.
Researchers discovered increasing emissions of short-lived ozone-depleting chemicals in East Asia, threatening the recovery of the ozone layer. The study found dichloromethane and 1,2-dichloroethane in large amounts, which can be carried up into the stratosphere and cause damage.
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Researchers found that volcanic eruptions can cause ozone depletion until 2070, despite declining levels of human-made CFCs. Natural sources of halogen gases from marine plankton and microalgae become important in the lower stratosphere after CFC concentrations decline.