On The Angry Prepper‚ we are going to talk about how Something Is Really Wrong. Something is not making sense as well as this bad feeling we all have. Things are off &; we need to be prepared for whatever might happen.

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On The Angry Truth‚ we are going to talk about how This Is Super Bad &; Over The Top. There has to be a line in the sand. This is too much &; enough is enough.

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Sometimes‚ all you need for a new discovery is some creative math. That was the case for a new paper by Edward Williams and Laurent Montési of the University of Maryland’s Department of Geology. They released a brief paper at the Lunar and Planetary Science Conference last month that describes a mathematical way to estimate the size of a lava tube using only remote sensing techniques. A critical starting point was the discovery that the ridge height of a surface above a lava tube is proportional to the cube of the height of the lava tube’s roof. Plenty of lava tubes have been studied in detail on Earth‚ and those studies were used to form the basis of that equation. However‚ until now‚ there was no relationship between the roof thickness and the details of the shape of the lava tunnel itself. Enter physical modeling – the authors used a physics modeling program (COMSOL Multiphysics) to model different roof heights based on different characteristics of tunnels. Fraser looks at how we might explore laval tubes. One big difference was the form of the tunnel itself – they focused on two styles. One‚ known as “laccolith‚” was a rectangle‚ whereas most people would think of a half-ellipse style when considering lava tubes. The modeling program also had to consider things like the material strength of the regolith as well as the pressure inside the tunnel itself – which would usually match the outside atmospheric pressure of largely airless worlds like the Moon and Mars‚ assuming there is a hole that connects it to the greater atmosphere. The equation the authors eventually found uses some fancy calculus and is beyond the scope of this article. Still‚ their model seems to fit the data for most modeled lava caves‚ including those on Earth. They turned their model to a well-known cave structure on Earth to prove that point. Valentine’s Cave‚ located in the Lava Beds National Monument in California‚ has been studied for decades by NASA researchers as an analog to caves found on the Moon and Mars. Those studies have resulted in accurate cave heights and ridge height estimates using techniques such as LIDAR. When applying their new model and using the known ridge height of Valentine’s Cave‚ the authors find a tube height within .07 m of the actual height of the Cave. Not bad for calculating the height only from the ridge height‚ which is an externally visible feature. Lava tubes are a central feature of any future crewed exploration mission. The obvious next step is to attempt to estimate some lava tube heights on our neighboring planetary bodies. At least some remote observatories around the Moon and Mars should be capable of estimating ridge height from their orbital positions. It’s then up to the team to estimate what the inside of the tube might look like. Unfortunately‚ it will probably be a while before human or robotic explorers enter one of these tubes to confirm the author’s estimates. But there are plenty of proposals for that as well – and one day‚ undoubtedly‚ someone or something will indeed step foot inside one of these ancient geological formations. Learn More:William &; Montési – DETERMINATION OF LAVA TUBE DEPTH AND SHAPE FROM TOPOGRAPHYUT – It’s Time to Study Lunar Lava Tubes. Here’s a Mission That Could HelpUT – Future Mars Helicopters Could Explore Lava TubesUT – Lava Tubes on the Moon Maintain Comfortable Room Temperatures Inside Lead Image:Lava tube on MarsCredit – NASA/JPL-Caltech/University of Arizona The post Mapping Lava Tubes on the Moon and Mars from Space appeared first on Universe Today.

Scientists have been underutilizing a key resource we can use to help us understand Earth: animals. Our fellow Earthlings have a much different‚ and usually much more direct‚ relationship with the Earth. They move around the planet in ways and to places we don’t. What can their movements tell us? Humanity has a fleet of satellites orbiting Earth that tell us all kinds of things about the planet. Satellites track temperature‚ CO2 emissions‚ rainfall‚ forest fires‚ drought‚ volcanic eruptions‚ etc. We know more about Earth than ever‚ and a lot of it is thanks to satellites. Climate change is our biggest concern right now‚ and new research shows that sensors attached to animals can elevate our climate change data to a new‚ more granular level. The research perspective is titled “Animal-borne sensors as a biologically informed lens on a changing climate‚” published in Nature Climate Change. The lead author is Diego Ellis-Soto‚ a graduate student at Yale University and a NASA FINESST (Future Investigators in NASA Earth and Space Science and Technology) fellow. The first animal tracker was probably just a piece of coloured string. In 1803‚ American Naturalist John Audobon wanted to know if birds migrated and returned to the same place yearly. So he attached a piece of string around a bird’s leg before it flew south for the winter. Next spring‚ he spotted the bird and knew it had returned to the same place. The tools at scientists’ disposal now are much more powerful than Audobon’s piece of string. Ellis-Soto studies animal movements and what they can tell us about rapid environmental change. He uses remote sensing‚ GPS tracking‚ and citizen science to try to forecast environmental changes at fine spatio-temporal scales. This type of research has its roots in things like the Great Backyard Bird Count‚ where citizen scientists spend four days each February recording what birds they see. Participants spend only a few minutes each day recording what they see and uploading it to a website. The result is a massive collection of data unattainable by any other method. The Bird Count is a more passive example of animal movement studies that the authors advocate. They’re pursuing more active methods of studying animal movement and gathering data to get around some of the roadblocks scientists face when studying the climate. “Traditional climate measurements are often constrained by geographically static‚ coarse‚ sparse and biased sampling‚ and only indirect links to ecological responses‚” Ellis-Soto and his co-authors write in their research. “Here we discuss how animal-borne sensors can deliver spatially fine-grain‚ biologically fine-tuned‚ relevant sampling of climatic conditions in support of ecological and climatic forecasting.” A 130-pound wolf watches biologists in Yellowstone National Park after being captured and fitted with a radio collar on 1-9-03. Tracking wolves as they move through their territory can also tell researchers about the environmental and climate conditions that motivate their movements. Image Credit: By William C. Campbell – U.S. Fish &; Wildlife Service‚ Public Domain‚ https://commons.wikimedia.org/w/index.php?curid=30609 Even though we have a fleet of powerful satellites and a massive number of ground-based data collectors‚ they each have a weakness of some type. Ground stations can only sample data from a single location. Satellites have their own limitations. They can collect data in fine spatial resolution‚ across multiple wavelengths‚ or at high temporal frequency. But they don’t do it all at once. They’re also inhibited by cloud cover and‚ in some cases‚ the darkness of night. The result is data that though powerful‚ has gaps in it. Animal sensors can bridge those gaps‚ according to Ellis-Soto. “Animals are an integral component of Earth observation‚” he said. Animal-borne sensors (ABS) aren’t new. They’ve been used for decades to track various animals‚ including predators like lions‚ ocean-going animals like orcas‚ migrating birds‚ and even insects. These trackers monitor and report an animal’s movements in places that satellites can’t monitor‚ and humans can’t easily access. But Ellis-Soto says we can use trackers to gather other data‚ like temperature. In South Africa’s Kruger National Park‚ scientists used temperature and movement trackers on elephants to monitor the animals as they moved around in the park for one year. They combined it with satellite temperature data. Two maps from that effort show how the elephant sensors filled in gaps in the satellite data and created a much more complete picture. These two maps show satellite temperature data (top) and elephant location and temperature data from ABSs. Image Credit: NASA Earth Observatory images by Michala Garrison‚ using Landsat data from the U.S. Geological Survey and elephant-borne sensor data from Thaker‚ M. et al. (2019). Ellis-Soto sees the issue in terms of bias. Each satellite has a sampling bias. Sampling bias is unavoidable when designing satellites and their instruments. But animals have a sampling bias‚ too‚ and scientists can use that bias for their own purposes. “These animals are extremely biased sensors‚ and this bias is called animal ecology and behaviour‚” said Ellis-Soto. The elephants in Kruger National Park are just one example. The use of ABSs is widespread. This image shows how ABSs are used to collect different environmental data. 1 to 9 show ABSs used to estimate measurements ranging from wind speed and direction to air temperature. 10 to 16 shows ABSs used to measure sea surface temperature and salinity. 17 and 18 show ABSs used to measure near-surface temperature in terrestrial realms. Image Credit: Ellis-Soto et al. 2023 Ellis-Soto and his colleagues see many opportunities to expand this kind of monitoring and combine it with other data‚ including satellite data. “Technological advances in ABSs offer an ever-increasing number and quality of auxiliary on-board sensors that collect climatic variables‚” they write. Technological advancements in ABSs combined with animal movement are powerful tools that can play a larger role. “Animals can access and monitor remote areas and detect rare events and hard-to-measure environmental conditions of potential importance for climate change projections.” The authors highlight the issue of snowmelt. Around the world‚ snowmelt is an important indicator in understanding the coming growing season. Snowmelt provides irrigation water for millions of farmers around the world. For example‚ in India and Pakistan‚ 130 million farmers rely on meltwater to irrigate their crops. “In many areas of the globe‚ snowmelt is a crucial component of the natural hydrological cycle‚” they write. “A biological warning system of earlier snowmelt under climate change by ABSs may improve estimates of the contribution to mountain hydrology‚ a critical area of improvement for climate change projections and water runoffs for food production.” In the Arctic‚ researchers used ABSs to track the movements of three types of birds: snowy owls‚ rough-legged buzzards‚ and peregrine falcons. The ABS data showed how these animals follow the snowmelt during migratory journeys. The data was more granular than satellites could provide. “Spatially fine-scaled capture of patches of snowmelt as homed in on by animals is otherwise hard to attain but highly useful for understanding the phenology and distribution of Arctic species under changing climate conditions‚” the authors write. There are many examples of ABSs being used to gather otherwise unattainable or difficult-to-obtain environmental data. But there are also many more opportunities waiting to be realized. This figure shows how harp seals can be fitted with ABSs to record and transmit data while going about their business. ARGOS is a satellite network dedicated to wildlife monitoring. Image Credit: McMahon et al. 2021. “We see a real opportunity for the ecological and meteorological community to employ ABSs for a strongly expanded‚ representative and biologically interpretable measurement of meteorologicaland climatic conditions under current and future climate‚” the authors write. Our fellow Earthlings are like an army of unwitting citizen scientists. As long as the ABSs don’t hamper or harm them‚ they can greatly contribute to Earth’s well-being without even knowing it. “The thousands of animals today swimming‚ running and flying around the globe carrying electronic tags are agile earth observers with the potential to provide transformative data collection in support of global change research‚ meteorology‚ climate forecasting and ecology‚” the authors conclude. The post How Animal Movements Help Us Study the Planet appeared first on Universe Today.

Astronomers are pretty sure they know where the Moon came from. In the early Solar System‚ a Mars-sized object dubbed Theia smashed into Earth. This cataclysmic collision knocked a huge mass of material into orbit‚ which coalesced and cooled into the Moon. But establishing exactly when this occurred is a difficult task. At the 55th annual Lunar and Planetary Science Conference (LPSC 55) last month in The Woodlands‚ Texas‚ researchers proposed a new timeline of events that moves the giant impact earlier than previous predictions‚ at just 50 million years after the formation of the Solar System. Dating the giant impact event is challenging because the existing evidence is conflicting‚ telling stories that don’t line up. One line of evidence is derived from planetary orbits. The most likely cause of the impact is an instability in Jupiter’s orbit‚ which would have thrown objects like Theia into Earth’s path within the first 100 million years of the Solar System. If that orbital instability happened any later‚ the paths of the inner planets would have been disrupted‚ and Jupiter’s trojan asteroids‚ like binary pair Patroclus and Menoetius‚ (which NASA’s Lucy spacecraft plans to visit in 2033) would not remain where we see them today. The best estimate based on these orbital observations places the impact between 37-62 million years after the formation of the Solar System. The Moon‚ researchers believe‚ would have cooled from a lake of magma into a solid surface within about 10 million years after impact. Geological evidence‚ however‚ seems to be telling a different story. The earliest known moon rocks formed much later‚ appearing to have crystalized from magma at about 208 million years. Rocks on Earth‚ similarly‚ seem to have formed into a proper crust at about 218 million years. A third dating scheme‚ done by measuring the decay of the element Hafnium into Tungsten‚ pushes the collision date early again‚ suggesting the Moon’s core formed at about 50 million years. Any explanation for lunar formation needs to account for all of these evidence types. A 2022 simulation of the giant impact that created the Moon. NASA / Durham University / Jacob Kegerreis. The scenario proposed at LPSC 55 does just that. They suggest an early collision around 50 million years‚ followed by a 10 million-year-long period of cooling. But the Moon then went through a cycle of reheating before finally cooling again at the 200-million-year mark. That reheating process is the key to this theory‚ and if it is correct‚ it would have been caused by tidal forces. The Moon’s orbit‚ according to this theory‚ was not yet stable around Earth‚ and its inclination and eccentricity increased in the years following impact‚ squeezing and stretching the Moon and liquifying it. These same tidal processes occur on other moons today: around Jupiter‚ for example‚ we see them creating volcanoes on Io and liquid oceans on Europa. The cooling process was also likely slowed by violent secondary impacts‚ as leftover material from the initial impact slammed into the Moon over millions of years. The team also added one new piece of evidence that strengthens the case for an early giant impact around 50 million years. Similar to the Hafnium-Tungsten decay method‚ the team measured the decay of earthly Rubidium sources into Strontium‚ giving an independent estimate supporting the early date. This research was carried out by Steven. J. Desch of Arizona State University and A. P. Jackson of Towson University. The post What's the Earliest the Moon Could Have Formed? appeared first on Universe Today.

Reports online claim there could be dozens, or as many as 60 staff members being laid off.