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65 Sentences With "atmospheric pressures"

How to use atmospheric pressures in a sentence? Find typical usage patterns (collocations)/phrases/context for "atmospheric pressures" and check conjugation/comparative form for "atmospheric pressures". Mastering all the usages of "atmospheric pressures" from sentence examples published by news publications.

At normal atmospheric pressures, oxygen turns solid at -6603 degrees Fahrenheit.
And then there are storm surges — where the low atmospheric pressures and powerful storm winds push waves to dangerous heights.
Sanjoy Som and his colleagues at the University of Washington, in Seattle, were looking at lava to measure ancient atmospheric pressures.
A team led by Ryan Fogt, an atmospheric scientist at Ohio University, came to this conclusion after reconstructing atmospheric pressures for the frozen continent from 1905 to the present.
Arctic sea ice melted usually quickly between March and May in 2016, according to the report, before slowing slightly in August and September as low atmospheric pressures and cloudy skies arrived.
Life has evolved to comfortably handle the shapes in which most molecules have arranged themselves under temperatures of about 32 degrees Fahrenheit and atmospheric pressures of an average day at sea level.
Instead, the pinkish substance is lightly painted over a scale model, which is then set up in a wind tunnel that mimics the intense atmospheric pressures on a real spacecraft or aircraft.
Because molten salt reactors run not on solid uranium rods, but rather on a liquid fuel in their heat exchange, molten salt reactor vessels are able to operate at normal, atmospheric pressures making reactor blowouts nearly impossible.
The printing technology behind this product is called "SuPR-NaP" (Surface Photo-Reactive Nano metal Printing), which can be used at normal temperatures and atmospheric pressures without the etching equipment for indium tin oxide (ITO) or metal film that was previously required, which enables more efficient and precise mass production in the workplace.
High-resolution spectrum obtained in 2020 has indicated the atmosphere of Kappa Andromedae b is filled by thick cloud deck extending to low atmospheric pressures.
Psychrometry measures the rates of condensation through evaporation into the air moisture at various atmospheric pressures and temperatures. Water is the product of its vapor condensation—condensation is the process of such phase conversion.
Hydrothermal liquefaction is a process similar to pyrolysis that can process wet materials. The process is typically at moderate temperatures up to 400 °C and higher than atmospheric pressures. The capability to handle a wide range of materials make hydrothermal liquefaction viable for producing fuel and chemical production feedstock.
The bulk modulus of iridium trihydride is 190 GPa which is much less than that of iridium (383 GPa). Decomposition of iridium trihydride is slow when the pressure is reduced to 6 GPa, and perhaps it can be metastable at atmospheric pressures. A dihydride, IrH2, is predicted to be stable over 14 GPa.
Much of the water on Mars is permanently frozen, mixed with the rocks. So terrestrial permafrosts are a good analogue. And some of the Carnobacterium species isolated from permafrosts have the ability to survive under the conditions of the low atmospheric pressures, low temperatures and dominated anoxic atmosphere of Mars.Nicholson, Wayne, et al.
The standard addresses the four primary environmental factors (temperature, thermal radiation, humidity, and air speed) and two personal factors (activity and clothing) that affect thermal comfort. It is applicable for healthy adults at atmospheric pressures in altitudes up to (or equivalent to) , and for indoor spaces designed for occupancy of at least 15 minutes.
Corona discharges appear at atmospheric pressures in strongly non-uniform electric fields. Sharp edges of high voltage electrodes produce such fields in their vicinity. When the field in the rest space is negligible – this happens at large distances to the electric grounds – the corona discharge can be ignited. Otherwise, the high voltage electrodes may spark to the ground.
EVA training is conducted at the Sonny Carter Training Facility. Candidates are also trained to deal with emergencies associated with hyperbaric and hypobaric atmospheric pressures and are given exposure to the microgravity of space flight. Candidates maintain their flying proficiency by flying 15 hours per month in NASA's fleet of T-38 jets based at nearby Ellington Field.
This works both ways - if the pressure is increased beyond normal atmospheric pressures, the boiling of hot water could be suppressed far beyond normal temperatures. The cooling system of a modern internal combustion engine is a common example. # When a liquid boils it turns into a gas. The resulting gas takes up far more space than the liquid did.
Most storms formed and dissipated within the tropics, with the exception of Severe Tropical Storm Alda. During the season, atmospheric conditions shifted from El Niño to La Niña, but despite the shift, the season was similarly inactive as its predecessor. In general, sea surface temperatures were below normal, and atmospheric pressures were above normal, both unfavorable for tropical cyclogenesis.
Much of the country was located at about 30 latitudinal degrees North, where there tends to be high atmospheric pressures and little precipitation. The western United States were largely covered in seawater during the Late Triassic. Mountain building and volcanic activity were ongoing in the same region. The Triassic saw the Earth's biosphere recovering from the end-Permian mass extinction.
A pebble bed reactor using high mass-flow gaseous nitrogen coolant near normal atmospheric pressures is a possible heat source. Power generation could be accomplished with gas turbine technology, which is well developed. Nuclear fuel would be highly enriched uranium encapsulated in low- boron graphite balls probably 5–10 cm in diameter. The graphite would also moderate the neutrons of the nuclear reaction.
The Combustion Integrated Rack (CIR) chamber can operate at low (0.02 atm) or high (up to 3 atm) atmospheric pressures. Tools are not required to open the chamber or change or service the eight windows on the chamber. Gases are delivered through the bottles on the front of the rack. The exhaust package features a filter that can recycle the gas used or convert it to an expellable gas.
When grown under elevated hydrostatic pressure, the cells are rod-shaped with a sheath-like outer structure, motile, have a mean length of 1-1.5 mum and stain Gram-negative. They appear singly or in short chains. When grown at lower, or atmospheric, pressures, the cells elongate and become twisted. Growth is enhanced by hydrostatic pressure; the optimal pressure for growth is 40 MPa (26 MPa pressure at sampling site).
Using the second method, water vapor is compressed by means of a mechanical device, electrically driven in most cases. This form is designated mechanical vapor compression (MVC). The MVC process comprises two different versions: vapor compression (VC) and vacuum vapor compression (VVC). VC designates those systems in which the evaporation effect takes place at manometric pressure, and VVC the systems in which evaporation takes place at sub-atmospheric pressures (under vacuum).
Iridium disulfide is the binary inorganic compound with the formula IrS2. Prepared by the direct reaction of the elements, the compound adopts the pyrite crystal structure at high pressure. At normal atmospheric pressures, an orthorhombic polymorph is observed.. The high- and low-pressure forms both feature octahedral Ir centers, but the S–S distances are pressure dependent. Although not practical, IrS2 is a highly active catalyst for hydrodesulfurization.
Julian P. Cooke and Sarah E. Beard, "Verbal Communication Intelligibility in Oxygen-Helium and Other Breathing Mixtures at Low Atmospheric Pressures" Aerospace Medicine 36(December 1965): 116-1172. Her work was consulted in planning for the Manned Orbiting Laboratory Program. In 1969, she held the rank of Lieutenant Colonel, and was assigned to the Pentagon as special assistant. She was chair of the Aerospace Medical Association's Flight Nurse Section from 1968 to 1970.
Until then the shuttle and the station had kept one hatch closed to maintain respective atmospheric pressures, allowing the shuttle crew to conduct their spacewalks and mission goals. After a welcome ceremony and briefing, the eight spacefarers conducted structural tests of the station and its solar arrays, transferred equipment, supplies and refuse back and forth between the spacecraft, and checked out the television camera cable installed by Tanner and Noriega for the upcoming mission.
Early on September 20, it further weakened to a Category 2 hurricane. Rising atmospheric pressures to the north forced the storm to curve northwestward on September 21. Later that day, Gladys weakened to a Category 1 hurricane. The storm posed a threat to the East Coast of the United States, and passed about east of Cape Hatteras, North Carolina, before a deepening low pressure area over the Great Lakes region caused it to veer northeastward.
The origins of Fabian were from a tropical wave and a cold front that entered the northwestern Caribbean Sea on October 12\. The two systems interacted in the Gulf of Honduras, producing convection and low atmospheric pressures. An anticyclone developed over the system, which aided in the organization of the thunderstorms. At 1300 UTC on October 15, a Hurricane Hunters flight observed sustained winds of 40 mph (65 km/h) to the southwest of the Isle of Youth.
Though Isbell struck the state as a Category 2 hurricane, no winds in excess of 100 mph (160 km/h) were reported. Measurements peaked at 90 mph (150 km/h) at both Everglades City and Indiantown. Hurricane-force gusts were measured in Belle Glade, Fort Lauderdale, Key West, Pompano Beach, and West Palm Beach. Atmospheric pressures fell to 970.7 mb (hPa; 28.67 inHg) in the Dry Tortugas and 977.5 mb (hPa; 28.87 inHg) on the mainland in Juno Beach.
Since there is no carbon in ammonia, no carbon by-products are produced; thereby making this possibility a "carbon neutral" option for the future. Pure ammonia burns poorly at the atmospheric pressures found in natural gas fired water heaters and stoves. Under compression in an automobile engine it is a suitable fuel for slightly modified gasoline engines. Ammonia is the suitable alternative fuel because it has 18.6 MJ/kg energy density at NTP and carbon-free combustion byproducts.
In early-mid June 1972, atmospheric conditions favored tropical cyclogenesis in the Caribbean Sea. Banded convection developed in the northwestern Caribbean Sea by June 11, though the system did not significantly organize. After an upper trough moved east, wind shear decreased, causing lower atmospheric pressures observations in Cozumel, Quintana Roo, Mexico. It is estimated that a tropical depression developed by 1200 UTC on June 14, while centered over the Yucatán Peninsula, about southeast of Mérida, Yucatán.
Positive displacement pumps are the most effective for low vacuums. Momentum transfer pumps in conjunction with one or two positive displacement pumps are the most common configuration used to achieve high vacuums. In this configuration the positive displacement pump serves two purposes. First it obtains a rough vacuum in the vessel being evacuated before the momentum transfer pump can be used to obtain the high vacuum, as momentum transfer pumps cannot start pumping at atmospheric pressures.
Liquid helium is a physical state of helium, at very low temperatures if it is at standard atmospheric pressures. Liquid helium may show superfluidity. At standard pressure, the chemical element helium exists in a liquid form only at the extremely low temperature of −269 °C (about 4 K or −452.2 °F). Its boiling point and critical point depend on which isotope of helium is present: the common isotope helium-4 or the rare isotope helium-3.
A tropical wave emerged into the Atlantic Ocean from the west coast of Africa in late July; a weather station in Dakar, Senegal observed a wind shift on July 23\. The system moved quickly across the Atlantic at and reached the Lesser Antilles by July 28. The wave then continued moving rapidly westward across the Caribbean Sea. However, falling atmospheric pressures over the Southern United States eroded a subtropical ridge, causing the system to decelerate by July 30\.
Magnesocene is a white solid at room temperature. It has a melting point of 176 °C, though at atmospheric pressures it sublimes at 100 °C. Unlike ferrocene, magnesocene displays slight dissociation and subsequent ion association in polar, electron-donating solvents (such as ether and THF). :MgCp2 <=> MgCp+ + Cp- :MgCp2 + MgCp+ <=> Mg2Cp3+ :MgCp2 + Cp- <=> MgCp3- While ferrocene is stable at ambient conditions, magnesocene decomposes rapidly on exposure to oxygen or moisture, and as such must be synthesized and stored under inert conditions.
Recent advances in out of autoclave (OOA) processes hold promise for improving performance and lowering costs for composite structures. Using vacuum-bag-only (VBO) for atmospheric pressures, the new OOA processes promise to deliver less than 1 percent void content required for aerospace primary structures. Led by material scientists at Air Force Research Lab, the technique would save the costs of constructing and installing large structure autoclaves ($100M saved at NASA) and making small production runs of 100 aircraft economically viable.
The most efficient atmospheric pressure at which a conventional propelling nozzle works is set by the geometry of the nozzle bell. While the geometry of the conventional bell remains static the atmospheric pressure changes with altitude and therefore nozzles designed for high performance in the lower atmosphere lose efficiency as they reach higher altitudes. In traditional rockets this is overcome by using multiple stages designed for the atmospheric pressures they encounter. The SABRE engine must operate at both low and high altitude scenarios.
As it moved over the warm waters of the Gulf Stream, it quickly organized and intensified into a Category 1 hurricane while east of Jacksonville, Florida. Because it was embedded within the western extension of the subtropical ridge, Bob retained higher-than- average atmospheric pressures throughout its lifespan. The hurricane continued north, and made landfall near Beaufort, South Carolina early on July 25 while maintaining winds of . Bob quickly weakened over land, decaying into a tropical storm three hours after landfall.
Despite favorable upper-level winds and falling atmospheric pressures, there were initially no signs of a circulation at the surface. Convection again increased early on August 20, and it gradually became better organized. Based on a ship's wind report of the system, it is estimated the wave developed into Tropical Depression Nine on August 21 while located about 260 miles (415 km) south of San Juan, Puerto Rico. The depression quickly showed signs of organization with the development of banding features around its blossoming convection.
Nitrous oxide can also be used to artificially increase the mass of oxygen present in the intake air. This is accomplished by injecting liquid nitrous oxide into the intake, which supplies significantly more oxygen in a given volume than is possible with atmospheric air. Nitrous oxide is 36.3% available oxygen by mass after it decomposes as compared with atmospheric air at 20.95%. Nitrous oxide also boils at at atmospheric pressures and offers significant cooling from the latent heat of vaporization, which also aids in increasing the overall air charge density significantly compared to natural aspiration.
A doubling or more of these small pressure differences could be achieved only by very major changes in the breathing effort at high altitudes. All of the above influences of low atmospheric pressures on breathing are accommodated primarily by breathing deeper and faster (hyperpnea). The exact degree of hyperpnea is determined by the blood gas homeostat, which regulates the partial pressures of oxygen and carbon dioxide in the arterial blood. This homeostat prioritizes the regulation of the arterial partial pressure of carbon dioxide over that of oxygen at sea level.
As a halogen, chlorine is a highly efficient disinfectant, and is added to public water supplies to kill disease- causing pathogens, such as bacteria, viruses, and protozoans, that commonly grow in water supply reservoirs, on the walls of water mains and in storage tanks. The microscopic agents of many diseases such as cholera, typhoid fever, and dysentery killed countless people annually before disinfection methods were employed routinely. By far most Chlorine is manufactured from table salt (NaCl) by electrolysis in the chlor-alkali process. The resulting gas at atmospheric pressures is liquified at high pressure.
Being a part of Pannonian plain the Municipality of Temerin has its climate characteristics. Pannonian plain is quite far away from the Adriatic or the Mediterranean Sea on the south and the Atlantic Ocean on the west. These distances are even bigger because of Dinarics and Alps mountain ranges which keep the humid airstreams coming from seas and oceans away. Airstreams, influencing weather changes through the year, are conditioned by unequal warming of Earth surface and different atmospheric pressures above Adriatic and Mediterranean, Atlantic Ocean and wide Euro-Asian land.
It is also predicted that Earth will become a desert planet within a billion years due to the Sun's increasing luminosity. A study conducted in 2013 concluded that hot desert planets without runaway greenhouse effect can exist in 0.5 AU around Sun-like stars. In that study, it was concluded that a minimum humidity of 1% is needed to wash off carbon dioxide from the atmosphere, but too much water can act as a greenhouse gas itself. Higher atmospheric pressures increase the range in which the water can remain liquid.
The first model used for operational forecasts, the single-layer barotropic model, used a single pressure coordinate at the 500-millibar (about ) level, and thus was essentially two-dimensional. High-resolution models—also called mesoscale models—such as the Weather Research and Forecasting model tend to use normalized pressure coordinates referred to as sigma coordinates. This coordinate system receives its name from the independent variable \sigma used to scale atmospheric pressures with respect to the pressure at the surface, and in some cases also with the pressure at the top of the domain.
Because of its symmetrical shape, Vanguard 3 was selected by the experimenters for use in determining upper atmospheric densities as a function of altitude, latitude, season, and solar activity. As the spacecraft continuously orbited, it would lag its predicted positions slightly, accumulating greater and greater delay due to drag of the residual atmosphere. By measuring the rate and timing of orbital shifts, the relevant atmosphere's parameters could be back-calculated knowing the body's drag properties. It was determined that atmospheric pressures, and thus drag and orbital decay, were higher than anticipated, as Earth's upper atmosphere tapered into space gradually.
Further complicating estimates of the habitability of the Martian surface is the fact that very little is known about the growth of microorganisms at pressures close to those on the surface of Mars. Some teams determined that some bacteria may be capable of cellular replication down to 25 mbar, but that is still above the atmospheric pressures found on Mars (range 1–14 mbar). In another study, twenty-six strains of bacteria were chosen based on their recovery from spacecraft assembly facilities, and only Serratia liquefaciens strain ATCC 27592 exhibited growth at 7 mbar, 0 °C, and CO2-enriched anoxic atmospheres.
By early on June 21, a large extratropical trough spawned a low pressure area, which resulted in baroclinic activity. As a result, Agnes restrengthened into a tropical storm at 1800 UTC on June 21, while centered over eastern North Carolina. Three hours later, the National Hurricane Center noted decreasing atmospheric pressures, and indicated that winds had reached gale-force winds and once again upgraded Agnes to a tropical storm. By early on June 22, Agnes emerged into the northwestern Atlantic Ocean, where it continued to re-intensify. At 1200 UTC, Agnes reached its minimum atmospheric pressure of , as reported by a reconnaissance aircraft.
Southern oscillation, a phenomenon first observed by Sir Gilbert Thomas Walker, director general of observatories in India, refers to the seesaw relationship of atmospheric pressures between Tahiti and Darwin, Australia. Walker noticed that when pressure was high in Tahiti, it was low in Darwin, and vice versa. A Southern Oscillation Index (SOI), based on the pressure difference between Tahiti and Darwin, has been formulated by the Bureau of Meteorology (Australia) to measure the strength of the oscillation. Walker noticed that the quantity of rainfall in the Indian subcontinent was often negligible in years of high pressure over Darwin (and low pressure over Tahiti).
In general, the farther inland from the Mediterranean Sea a given part of the country lies, the greater are the seasonal contrasts in temperature and the less rainfall. Atmospheric pressures during the summer months are relatively uniform, whereas the winter months bring a succession of marked low pressure areas and accompanying cold fronts. These cyclonic disturbances generally move eastward from over the Mediterranean Sea several times a month and result in sporadic precipitation. Most of the East Bank receives less than of rain a year and may be classified as a dry desert or steppe region.
Because of its symmetrical shape, Vanguard 2 was selected by the experimenters for use in determining upper atmospheric densities as a function of altitude, latitude, season, and solar activity. As the spacecraft continuously orbited, it would lead its predicted positions slightly, accumulating greater and greater advance as it spiraled lower and faster due to the drag of the residual atmosphere. By measuring the rate and timing of orbital shifts, the relevant atmosphere's parameters could be back-calculated knowing the body's drag properties. It was determined that atmospheric pressures, and thus drag and orbital decay, were higher than anticipated, as Earth's upper atmosphere gradually tapered into space.
Vanguard 1 with its six solar cells attached Because of its symmetrical shape, Vanguard 1 was used by experimenters for determining upper atmospheric densities as a function of altitude, latitude, season, and solar activity. As the satellite continuously orbited, it would deviate from its predicted positions slightly, accumulating greater and greater shift due to drag of the residual atmosphere. By measuring the rate and timing of orbital shifts, together with the body's drag properties, the relevant atmosphere's parameters could be back-calculated. It was determined that atmospheric pressures, and thus drag and orbital decay, were higher than anticipated, since Earth's upper atmosphere does taper off into space gradually.
The next day, however, the feature deteriorated as thunderstorm activity spread across the Greater Antilles, although the upper-level regime remained favorable for eventual redevelopment. On June 24, a low-level circulation had gradually become better established to the south of Jamaica, although it was displaced from its poorly organized convection. By 1800 UTC, a surface low-pressure area had formed about 105 miles (165 km) to the northeast of Cabo Gracias a Dios, Nicaragua, but due to a lack of persistent thunderstorm activity, it was not yet considered a tropical cyclone. Later that day, convection increased over the center of circulation, and atmospheric pressures dropped across the region.
Ion funnels are frequently used in mass spectroscopy devices to collect ions from an ionization source. Previous devices lacking an ion funnel often lost ions during the transition from ionization source to the detector of the mass spectrometer. This loss was due to the increasing number of collisions undergone by ions with other gas molecules present in the atmosphere. The introduction of the ion funnel greatly reduced the amount of ions lost during experiments by guiding ions towards a desired destinationSmith, Richard D.; Shaffer, Scott A. Method and apparatus for directing ions and other charged particles generated at near atmospheric pressures into a region under vacuum.
A roughing pump is any vacuum pump (typically mechanical) used to initially evacuate a vacuum system, as a first stage towards achieving high vacuum or ultra high vacuum. The term "roughing pump" derives from the vacuum range it works in, "rough vacuum", above 1x10−3 torr (0.1 Pa). Pumps that operate in the high vacuum ranges typically don't operate, or only operate inefficiently, at atmospheric pressures, whereas pumps that work efficiently at atmospheric pressure usually cannot produce a vacuum lower than approximately 1x10−3 torr. One consideration for choosing a roughing pump is whether the pump uses lubricating oil that's exposed to the vacuum.
Later that day, a cold front entered the northwestern Caribbean and may have contributed to the further development of the system. A broad low-pressure area formed on October 21, after convection intensified near the wave's axis. However, the upper- level winds were only described as "marginally favorable" and relatively dry air in the region was expected to act as a hindrance to development. Throughout the day on October 22, atmospheric pressures decreased and the circulation continuously became better defined, while convection increased significantly on the western side of the system and near the center. Around 06:00 UTC on October 23, the system strengthened into Tropical Depression Eighteen, while situated about north of Providencia Island.
The following is a List of atmospheric pressure records in Europe and the extratropical Northern Atlantic (it does not include localised events, such as those that occur in tornados). Extreme pressure values in Europe show both seasonal and geographical differentiation. The greatest pressure extremes occur in winter (January) with the deepest lows occurring to the northwest of the continent with a diminishing influence of low pressure to the southeast towards Central Europe and Southeast Europe. This is related to the main cyclonic centre of the Icelandic low, and the North Atlantic extratropical storm track, close to which have been observed some of the lowest atmospheric pressures of the Northern Hemisphere outside the tropics.
During November 1988, weather patterns over the Bay of Bengal were dominated by the winter monsoon, leading to lower atmospheric pressures over the region and the conglomeration of moisture across the area. The genesis of the 1988 Bangladesh cyclone was preceded by floods that occurred over the Malay Peninsula as a result of a monsoon trough redeveloping over the region. By 18:00 UTC on November 21, a low-pressure area within the Strait of Malacca was sufficiently organized such that the Joint Typhoon Warning Center (JTWC) issued a Significant Tropical Weather Advisory; thus, the JTWC began closely monitoring the newly developing storm. Over the next few days, the tropical depression tracked west-northwestward into the Andaman Sea.
7 The development of scuba gear allowed researchers to visually explore the oceans as it contains a self-contained underwater breathing apparatus allowing a person to breathe while being submerged 100 to 200 feet into the ocean. Submersibles were built like small submarines with the purpose of taking marine scientists to deeper depths of the ocean while protecting them from increasing atmospheric pressures that cause complications deep under water. The first models could hold several individuals and allowed limited visibility but enabled marine biologists to see and photograph the deeper portions of the oceans. Remotely operated underwater vehicles are now used with and without submersibles to see the deepest areas of the ocean that would be too dangerous for humans.
Upon completing his PhD, Brisdon worked for one year on a UKEA (Winfrith) funded project investigating on design, construction and testing of systems for sampling directly from a reaction chamber at or above atmospheric pressures and at high temperatures. He then completed his postdoctoral research at University of Leicester where he worked on synthesis of high oxidation-state transition metal fluorides and oxide-fluorides via high pressure and liquid fluorine syntheses and on the fluorination of the fullerene's, C60and C70. He then joined the University of Manchester as a Lecturer and was later on promoted to the position of Senior Lecturer. Brisdon's research in general is based on fluorine chemistry, including on HCFCs, fluorine-containing organometallic systems, fluorophosphines and fluorine-containing materials, such as ionic liquids and fluorographenes.
In Between Three > Points [2000] I explored the idea of reading a sculpture in time, as in a > work of music. The work is built from three pieces that... tell the story of > the creation of a form in three chapters: (1) the beginning, birth, or > underground level, (2) the initiation, or earth ground level, and (3) the > rebirth or result tending toward the sky. The form is not completely free to > grow as it will, but is constrained and guided by internal tectonic > pressures and external atmospheric pressures. The sculpture can be read in > two directions at the same time: horizontally between the three parts and > vertically between the ground and the sky.... > > In Between Earth and Sky [2002] the idea is the same but expressed more in > the vertical direction.
One of the surprises of the impacts was the small amount of water revealed compared to prior predictions. Before the impact, models of Jupiter's atmosphere had indicated that the break-up of the largest fragments would occur at atmospheric pressures of anywhere from 30 kilopascals to a few tens of megapascals (from 0.3 to a few hundred bar), with some predictions that the comet would penetrate a layer of water and create a bluish shroud over that region of Jupiter. Astronomers did not observe large amounts of water following the collisions, and later impact studies found that fragmentation and destruction of the cometary fragments in an 'airburst' probably occurred at much higher altitudes than previously expected, with even the largest fragments being destroyed when the pressure reached , well above the expected depth of the water layer. The smaller fragments were probably destroyed before they even reached the cloud layer.
Adams argues that the ML-1 design and implementation was flawed due to the decision to build an advanced, highly efficient, easily transportable closed-cycle nitrogen gas turbine before any other functional version of the design had been created. Adams opines that the designers of ML-1 made several incorrect decisions, including adding an unnecessary recuperator to enhance efficiency, using a calandria-based water-tube fission heat source unproven in the "real world", using nine atmospheres of pressure at the compressor inlet that saved space but required a custom-built turbine rather than one designed for atmospheric pressures, placing insulating foil within the gas piping to improve efficiency (the foil later broke off and contaminated the closed loop with its flecks, causing deflaking problems for engineers), and using custom- built, first-of-a-kind components instead of using commercially proven aircraft or power generation derived turbines.
In mid-October, a significant drop in atmospheric pressures over the western Caribbean Sea coincided with the development of a trough on October 17\. Observations suggested that a circulation formed on October 20, with the Atlantic hurricane database listing a tropical storm beginning at 00:00 UTC, with the system was situated about 95 mi (155 km) southeast of the Archipelago of San Andrés, Providencia and Santa Catalina. The cyclone initially moved slowly northwestward due to a high pressure system over Bermuda. Early on October 22, the storm intensified into a Category 1 hurricane, based on sustained winds of on Great Swan Island. The hurricane strengthened significantly over the northwestern Caribbean, becoming a Category 2 hurricane at 00:00 UTC on October 23 and a Category 3 hurricane six hours later. Around 18:00 UTC, the cyclone reached Category 4 intensity and peaked with maximum sustained winds of 140 mph (220 km/h) and a minimum barometric pressure of .

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