Measurement of Speed of Sound Profile Using Laaces Balloon

Total Page:16

File Type:pdf, Size:1020Kb

Measurement of Speed of Sound Profile Using Laaces Balloon Abstract Measuring and Calculating the Speed of Sound Profile Results The goal of this mission was to test the speed of sound at different The environmental data measured in the launch at NASA CSBF on May altitudes and ultimately at a maximum height of 100,000 feet during 16 agree reasonably well with the data measured by Dallas weather a total solar eclipse. In conjunction with this testing, environmental during a Total Solar Eclipse using LaACES Balloon station which is about 122 miles north from the CSBF. The sonar parameters including temperature, pressure, and humidity are stopped working at temperatures lower than -40 °C (readings are all measured and used to calculate the speed of sound to compare to zeros). In addition, the acquired speed of sound data are quite noisy. the measured results. The first balloon launch of payload Dorothy Adam Chase, William Dever, Matthew Foltz, Tyler Morgan, Brett was conducted in NASA CSBF on May 16, 2017. The improved payload “Dorothy 2” was launched successfully in Carbondale, IL. on Schaefer, Brian Schaefer, and Zhuang Li Aug. 21, 2017. Data are analyzed and further improvement plan is discussed. McNeese State University, Lake Charles, LA Background The measurements of speed Pressure and humidity data from May 16th launch of sound profiles were conducted 6 Volt Battery Pack in the 1960’s when measurements were conducted in New York Temperature 5-V Voltage 3-V Voltage Pressure City, New York, both in the Sensor Regulator Regulator Sensor Summer and Winter seasons, as show in the figure to the Humidity right [1]. The measurements Sensor Arduino Due Sound Speed were in a much wider range Microcontroller Sensor (0 to 120 km). For the altitude range of 0 to 30 km, it can be 3 Volt DC heating seen in the figure that the Battery pad Temperature data and speed of sound plotted as measured and calculated th speed of sound dec reases as it from May 16 launch Overall layout of electronic components Power supply layout reaches 10 km and then 352 370 y = 45.463x - 435.59 350 y = 24.302x - 70.782 inc reases again as it reac hes The Arduino Due allows for a lower power consumption and better compatibility with existing hardware to make the 350 R² = 0.80208 348 330 the 30 km altitude. 346 integration seamless. 310 344 (m/ s ) 290 342 270 The speed of sound can be calculated using measured temperature, speed of sound 340 A 6-V battery pack supplies power for the microcontroller and sensors. Most of the devices run off 3.3 V line while the 250 15 15. 5 16 16. 5 17 17. 5 speed of sound (m/s) 338 humidity, and pressure data from an empirical formula studied by E.A. sonar runs off the 5 V line supplied by the board. Most of the hardware connections are actually done through the 16. 95 17 17. 05 17. 1 17. 15 17. 2 17. 25 17. 3 Dean 330 325 (1) coding of the Arduino Due, which lightens the payload while also makes it easier to test and prepare the module before 320 cT= 20.06 s 320 flight. To ensure the sonar sensor still func tions at low temperatures, a heading pad is used. The heading pad, 310 300 315 where Ts is c alled absolute sonic temperature that inc ludes the effec ts 290 constructed using a mesh of polyester filament and micro metal conductive Fiber, is powered by a stand-alone 3-V 310 280 of humidity and pressure [2]. The speed of sound on a normal day is 270 battery. y = 23.517x - 73.347 305 y = 23.269x - 71.261 260 speed of sound (m/s) roughly 340 m/s under one standard atmospheric pressure on the 250 speed of sound (m/s) 300 Mechanical Design 15. 75 15. 8 15. 85 15. 9 15. 95 16 16. 05 16. 1 16. 15 16. 2 16. 45 16. 5 16. 55 16. 6 16. 65 16. 7 surface of the earth. kelvin kelvin The external structure is composed of two layers of 1/2 inch thick polystyrene. The dimensions of the container form a square root of temperature square root of temperature th The physical measurement of the speed of sound can be done by box with sides 7.5 inches wide, 8.8 inches long, and 4.69 inches tall (19.05 cm x 22.38 cm x 11.91 cm). The thickness of Sonar data from May 16 launch timing how long a sound wave reaches a target of a fixed distance. In the box serves as thermal insulation and shock absorption. Econokote, a heat shrinking skin, was ironed on to the In the second launch, the sonar was functioning over the entire flight. the balloon payload Dorothy, the speed of sound is measured by outside of the box for extra structural and thermal support. There are 5 holes in the box. Two holes are 16 cm apart at Data are much less noisy. It means the heater worked as expected. timing a ultrasonic sonar pulse reflecting off a purely reflective mirror. opposite corners of the box on top and bottom for the strings, with another one on top for external temperature However, the recorded ping times at altitudes higher than 5 km are In the meantime, temperature, pressure, and humidity are measured sensor, pressure sensor, and sonar. The circuit boards were glued to the bottom of the box with hot glue using a piece signific antly less than reasonable values. Further investigations exc luded and applied to the empirical formula (1) to calculate the speed of of foam as a spacer. The housing was built to be compact to save weight and to heat components and batteries more the wind or vacuum influences. Similar behavior was repeated in freezer sound. The measured and calculated results are compared. efficiently. Small PVC pipes, which are stronger than ordinary soda straws, were used to help guide the rope and make tests as frost was observed on the transmitter/receiver. So a defrosting it easier to open and c lose the module. The parts for holding the mirror and sonar are 3D printed using PL A plastic , mechanism will be implemented in the next revision. Payload Design known for it’s durability and ease of use. All parts are glued using Gorilla brand glues due to their high strength. 30 350 25 Electrical Design meas ured 340 20 calculated 15 330 10 The payload needs to be able to conduct all environmental testing as 320 y = 32.723x - 227.13 Altitude (km)5 well as measuring the time from the ultrasonic sonar module. To do speed of sound (m/s) 0 310 this without losing resolution in the data and not receiving false 280 300 320 340 360 16.5 17 17.5 18 speed of sound (m/s) readouts from the sonar module itself, an Arduino Due is used. Such a square root of temperature kelvin microcontroller has a clock speed of 87 MHz which can read the timing Sonar data from Aug. 21 stlaunch during solar e clipse of the sonar down to the microsecond level and can read the data from all available components in a timely manner or around 3.14 Conclusion sec onds a reading. The results from the Aug. 21st were as expected for the conditions that had taken place during the eclipse. Environmental readings showed Completed build of Dorothy 2 module Wind Tunnel testing of Dorothy 2 improved reliability in its data c ompared to the first launc h. The sonar experienced icing on the transmitter/receiver causing the data to give false readings. Overall, the launch was a success and the data can be Software Design used to in conjunction with future launches. The software runs off a main loop that runs infinitely. An interrupt was designed to allow for safe system initiation and shutoff and also safe data acquisition in the form of an SD card. The program records the data from all sensors within References 3.14 seconds. Another loop within the main loop takes about 10 readings from the sonar in around 3 seconds to give an 1. Yang, X.R. Atmospheric Acoustics, D e Gruyter (2016) average reading in the post flight analysis. The program also has an initial startup check sequence and LED notification 2. Dean, E.A. Atmospheric Effects on the Speed of Sound, U. S. Army loc ated on the Arduino shield for visible notific ation to the operator. Report ASL-CR-79-1011-4 (1979) .
Recommended publications
  • Unit 11 Sound Speed of Sound Speed of Sound Sound Can Travel Through Any Kind of Matter, but Not Through a Vacuum
    Unit 11 Sound Speed of Sound Speed of Sound Sound can travel through any kind of matter, but not through a vacuum. The speed of sound is different in different materials; in general, it is slowest in gases, faster in liquids, and fastest in solids. The speed depends somewhat on temperature, especially for gases. vair = 331.0 + 0.60T T is the temperature in degrees Celsius Example 1: Find the speed of a sound wave in air at a temperature of 20 degrees Celsius. v = 331 + (0.60) (20) v = 331 m/s + 12.0 m/s v = 343 m/s Using Wave Speed to Determine Distances At normal atmospheric pressure and a temperature of 20 degrees Celsius, speed of sound: v = 343m / s = 3.43102 m / s Speed of sound 750 mi/h Speed of light 670 616 629 mi/h c = 300,000,000m / s = 3.00 108 m / s Delay between the thunder and lightning Example 2: The thunder is heard 3 seconds after the lightning seen. Find the distance to storm location. The speed of sound is 345 m/s. distance = v t = (345m/s)(3s) = 1035m Example 3: Another phenomenon related to the perception of time delays between two events is an echo. In a canyon, an echo is heard 1.40 seconds after making the holler. Find the distance to the canyon wall (v=345m/s) distanceround trip = vt = (345 m/s )( 1.40 s) = 483 m d= 484/2=242m Applications: Sonar, Ultrasound, and Medical Imaging • Ultrasound or ultrasonography is a medical imaging technique that uses high frequency sound waves and their echoes.
    [Show full text]
  • Atmospheric Cold Front-Generated Waves in the Coastal Louisiana
    Journal of Marine Science and Engineering Article Atmospheric Cold Front-Generated Waves in the Coastal Louisiana Yuhan Cao 1 , Chunyan Li 2,* and Changming Dong 1,3,* 1 School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] 2 Department of Oceanography and Coastal Sciences, College of the Coast and Environment, Louisiana State University, Baton Rouge, LA 70803, USA 3 Southern Laboratory of Ocean Science and Engineering (Zhuhai), Zhuhai 519000, China * Correspondence: [email protected] (C.L.); [email protected] (C.D.); Tel.: +1-225-578-2520 (C.L.); +86-025-58695733 (C.D.) Received: 15 October 2020; Accepted: 9 November 2020; Published: 11 November 2020 Abstract: Atmospheric cold front-generated waves play an important role in the air–sea interaction and coastal water and sediment transports. In-situ observations from two offshore stations are used to investigate variations of directional waves in the coastal Louisiana. Hourly time series of significant wave height and peak wave period are examined for data from 2004, except for the summer time between May and August, when cold fronts are infrequent and weak. The intra-seasonal scale variations in the wavefield are significantly affected by the atmospheric cold frontal events. The wave fields and directional wave spectra induced by four selected cold front passages over the coastal Louisiana are discussed. It is found that significant wave height generated by cold fronts coming from the west change more quickly than that by other passing cold fronts. The peak wave direction rotates clockwise during the cold front events.
    [Show full text]
  • A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods
    water Review A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods Elahe Akbari 1,2, Seyed Kazem Alavipanah 1,*, Mehrdad Jeihouni 1, Mohammad Hajeb 1,3, Dagmar Haase 4,5 and Sadroddin Alavipanah 4 1 Department of Remote Sensing and GIS, Faculty of Geography, University of Tehran, Tehran 1417853933, Iran; [email protected] (E.A.); [email protected] (M.J.); [email protected] (M.H.) 2 Department of Climatology and Geomorphology, Faculty of Geography and Environmental Sciences, Hakim Sabzevari University, Sabzevar 9617976487, Iran 3 Department of Remote Sensing and GIS, Shahid Beheshti University, Tehran 1983963113, Iran 4 Department of Geography, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany; [email protected] (D.H.); [email protected] (S.A.) 5 Department of Computational Landscape Ecology, Helmholtz Centre for Environmental Research UFZ, 04318 Leipzig, Germany * Correspondence: [email protected]; Tel.: +98-21-6111-3536 Received: 3 October 2017; Accepted: 16 November 2017; Published: 14 December 2017 Abstract: Oceans/Seas are important components of Earth that are affected by global warming and climate change. Recent studies have indicated that the deeper oceans are responsible for climate variability by changing the Earth’s ecosystem; therefore, assessing them has become more important. Remote sensing can provide sea surface data at high spatial/temporal resolution and with large spatial coverage, which allows for remarkable discoveries in the ocean sciences. The deep layers of the ocean/sea, however, cannot be directly detected by satellite remote sensors.
    [Show full text]
  • Physical Geography Chapter 5: Atmospheric Pressure, Winds, Circulation Patterns
    Physical Geography Chapter 5: Atmospheric Pressure, Winds, Circulation Patterns Torricelli – 1643- first Mercury barometer (76 cm, 29.92 in) – measures response to pressure Pressure – millibars- 1013.2 mb, will cause Hg to rise in tube Unequal heating of Earth’s surface is responsible for differences in pressure to! Variations in Atmospheric Pressure 1. Vertical Variations – increase in elevation, less air pressure Mt. Everest – 8848 m (or 29, 028 ft) – 1/3 pressure 2. Horizontal Variations a. Thermal (determined by T) Warm air is less dense – it rises away from the surface at the equator b. Dynamic: Air from the tropics moves northward and then to the east due to the Coryolis Effect. It collects at this latitude, increasing pressure at the surface. Basic Pressure Systems 1. Low – cyclone – converging air pressure decreases 2. High – anticyclone – Divergins air pressure increases Wind Isobars- line of equal pressure Pressure Gradient - significant difference in pressure Wind- horizontal movement of air in response to differences in pressure ¾ Responsible for moving heat toward poles ¾ 38° Lat and lower: radiation surplus If Earth did not rotate, and if there wasno friction between moving air and the Earth’s surface, the air would flow in a straight line from areas of higher pressure to areas of low pressure. Of course, this is not true, the Earth rotates and friction exists: and wind is controlled by three major factors: 1) PGF- Pressure is measured by barometer 2) Coriolis Effect 3) Friction 1) Pressure Gradient Force (PGF) Pressure differences create wind, and the greater these differences, the greater the wind speed.
    [Show full text]
  • Diving Air Compressor - Wikipedia, the Free Encyclopedia Diving Air Compressor from Wikipedia, the Free Encyclopedia
    2/8/2014 Diving air compressor - Wikipedia, the free encyclopedia Diving air compressor From Wikipedia, the free encyclopedia A diving air compressor is a gas compressor that can provide breathing air directly to a surface-supplied diver, or fill diving cylinders with high-pressure air pure enough to be used as a breathing gas. A low pressure diving air compressor usually has a delivery pressure of up to 30 bar, which is regulated to suit the depth of the dive. A high pressure diving compressor has a delivery pressure which is usually over 150 bar, and is commonly between 200 and 300 bar. The pressure is limited by an overpressure valve which may be adjustable. A small stationary high pressure diving air compressor installation Contents 1 Machinery 2 Air purity 3 Pressure 4 Filling heat 5 The bank 6 Gas blending 7 References 8 External links A small scuba filling and blending station supplied by a compressor and Machinery storage bank Diving compressors are generally three- or four-stage-reciprocating air compressors that are lubricated with a high-grade mineral or synthetic compressor oil free of toxic additives (a few use ceramic-lined cylinders with O-rings, not piston rings, requiring no lubrication). Oil-lubricated compressors must only use lubricants specified by the compressor's manufacturer. Special filters are used to clean the air of any residual oil and water(see "Air purity"). Smaller compressors are often splash lubricated - the oil is splashed around in the crankcase by the impact of the crankshaft and connecting A low pressure breathing air rods - but larger compressors are likely to have a pressurized lubrication compressor used for surface supplied using an oil pump which supplies the oil to critical areas through pipes diving at the surface control point and passages in the castings.
    [Show full text]
  • Air Pressure and Wind
    Air Pressure We know that standard atmospheric pressure is 14.7 pounds per square inch. We also know that air pressure decreases as we rise in the atmosphere. 1013.25 mb = 101.325 kPa = 29.92 inches Hg = 14.7 pounds per in 2 = 760 mm of Hg = 34 feet of water Air pressure can simply be measured with a barometer by measuring how the level of a liquid changes due to different weather conditions. In order that we don't have columns of liquid many feet tall, it is best to use a column of mercury, a dense liquid. The aneroid barometer measures air pressure without the use of liquid by using a partially evacuated chamber. This bellows-like chamber responds to air pressure so it can be used to measure atmospheric pressure. Air pressure records: 1084 mb in Siberia (1968) 870 mb in a Pacific Typhoon An Ideal Ga s behaves in such a way that the relationship between pressure (P), temperature (T), and volume (V) are well characterized. The equation that relates the three variables, the Ideal Gas Law , is PV = nRT with n being the number of moles of gas, and R being a constant. If we keep the mass of the gas constant, then we can simplify the equation to (PV)/T = constant. That means that: For a constant P, T increases, V increases. For a constant V, T increases, P increases. For a constant T, P increases, V decreases. Since air is a gas, it responds to changes in temperature, elevation, and latitude (owing to a non-spherical Earth).
    [Show full text]
  • Aircraft Performance: Atmospheric Pressure
    Aircraft Performance: Atmospheric Pressure FAA Handbook of Aeronautical Knowledge Chap 10 Atmosphere • Envelope surrounds earth • Air has mass, weight, indefinite shape • Atmosphere – 78% Nitrogen – 21% Oxygen – 1% other gases (argon, helium, etc) • Most oxygen < 35,000 ft Atmospheric Pressure • Factors in: – Weather – Aerodynamic Lift – Flight Instrument • Altimeter • Vertical Speed Indicator • Airspeed Indicator • Manifold Pressure Guage Pressure • Air has mass – Affected by gravity • Air has weight Force • Under Standard Atmospheric conditions – at Sea Level weight of atmosphere = 14.7 psi • As air become less dense: – Reduces engine power (engine takes in less air) – Reduces thrust (propeller is less efficient in thin air) – Reduces Lift (thin air exerts less force on the airfoils) International Standard Atmosphere (ISA) • Standard atmosphere at Sea level: – Temperature 59 degrees F (15 degrees C) – Pressure 29.92 in Hg (1013.2 mb) • Standard Temp Lapse Rate – -3.5 degrees F (or 2 degrees C) per 1000 ft altitude gain • Upto 36,000 ft (then constant) • Standard Pressure Lapse Rate – -1 in Hg per 1000 ft altitude gain Non-standard Conditions • Correction factors must be applied • Note: aircraft performance is compared and evaluated with respect to standard conditions • Note: instruments calibrated for standard conditions Pressure Altitude • Height above Standard Datum Plane (SDP) • If the Barometric Reference Setting on the Altimeter is set to 29.92 in Hg, then the altitude is defined by the ISA standard pressure readings (see Figure 10-2, pg 10-3) Density Altitude • Used for correlating aerodynamic performance • Density altitude = pressure altitude corrected for non-standard temperature • Density Altitude is vertical distance above sea- level (in standard conditions) at which a given density is to be found • Aircraft performance increases as Density of air increases (lower density altitude) • Aircraft performance decreases as Density of air decreases (higher density altitude) Density Altitude 1.
    [Show full text]
  • OCN 201 El Nino
    OCN 201 El Nino El Nino theme page http://www.pmel.noaa.gov/tao/elnino/nino-home-low.html Reports to the Nation http://www.pmel.noaa.gov/tao/elnino/report/el-nino-report.html This page has all the text and figures and also how to get the booklet 1 El Nino is a major reorganisation of the equatorial climate system that affects regions far from its point of origin in the western Equatorial Pacific Occurs roughly every 6 years around Xmas-time Onset recognised by climatic effects --warm surface waters -- collapse of fisheries -- heavy rains in Peru/Ecuador/central Pacific -- droughts in Indonesia -- change in typhoon tracks Is a good example of how the ocean and atmosphere interact 2 What phase do you think we are in now? A El Nino B La Nina C Normal D I don’t know! A = El Nino 2014 2015 Southern Oscillation Atmospheric pressure differential between Tahiti and Darwin Normally low pressure in Darwin, high in Tahiti Low pressure High pressure Normal El Nino El Nino high pressure in Darwin, low in Tahiti Change in pressure differential results in weakening of easterly equatorial winds 3 Normal conditions in the Equatorial Pacific Strong easterly winds: Pile up warm water in the western Pacific -- thermocline deep in western Pacific, shallow in eastern Pacific Winds drive equatorial upwelling How much higher do you think that sea level is in the western Pacific? A 10cm B 50 cm C 1 metres D 5 metres E More! About 40 cm 4 Satellite image of chlorophyll abundance As thermocline is shallow in eastern Pacific upwelling brings nutrients to surface waters along
    [Show full text]
  • Quick Reference Guide on the Units of Measure in Hyperbaric Medicine
    Quick Reference Guide on the Units of Measure in Hyperbaric Medicine This quick reference guide is excerpted from Dr. Eric Kindwall’s chapter “The Physics of Diving and Hyperbaric Pressures” in Hyperbaric Medicine Practice, 3rd edition. www.BestPub.com All Rights Reserved 25 THE PHYSICS OF DIVING AND HYPERBARIC PRESSURES Eric P. Kindwall Copyright Best Publishing Company. All Rights Reserved. www.BestPub.com INTRODUCTION INTRODUCTIONThe physics of diving and hyperbaric pressure are very straight forTheward physicsand aofr edivingdefi nanded hyperbaricby well-k npressureown a nared veryacce pstraightforwardted laws. Ga sandu narede r definedpres subyr ewell-knowncan stor eande nacceptedormous laws.ene rgGasy, underthe apressuremount scanof storewhi cenormoush are o fenergy,ten the samountsurprisin ofg. whichAlso, s arema loftenl chan surprising.ges in the pAlso,erce smallntage schangesof the inva rtheiou spercentagesgases use dofa there variousgrea gasestly m usedagni fareied greatlyby ch amagnifiednges in am byb ichangesent pre sinsu ambientre. The pressure.resultan t pTheh yresultantsiologic physiologiceffects d effectsiffer w idifferdely d ewidelypend idependingng on the onp rtheess upressure.re. Thus ,Thus,divi ndivingg or oorpe operatingrating a a hy- perbarichype rfacilitybaric f requiresacility re gainingquires gcompleteaining c oknowledgemplete kn ofow theled lawsge o finvolvedthe law stoin ensurevolved safety.to ensure safety. UNITS OF MEASURE UNITS OF MEASURE This is often a confusing area to anyone new to hyperbaric medicine as both Ameri- This is often a confusing area to anyone new to hyperbaric medicine as can and International Standard of Units (SI) are used. In addition to meters, centimeters, both American and International Standard of Units (SI) are used. In addition kilos,to pounds,meters, andcen feet,time someters, kpressuresilos, po uarend givens, an dinf atmosphereseet, some p rabsoluteessures andare millimetersgiven in of mercury.atmosph Tableeres 1a bgivessolu thete a exactnd m conversionillimeters factorsof me rbetweencury.
    [Show full text]
  • Presented by the NOAA Diving Center Seattle, Washington Global View
    Presented by the NOAA Diving Center Seattle, Washington Global View Definition Air pressure Water pressure Gauge and absolute pressures Measuring pressure Key Points Introduction Need & value: As NOAA divers performing underwater tasks, we need to calculate pressure at depth, gas volume changes caused by changing pressure, the partial pressures of gases, and more. Effect: When we learn the fundamentals of physics and use them properly, we can solve diving problems easily and correctly. This lesson focuses on the basic principles of calculating for pressure and is a foundation for more complex calculations we will learn in future lessons. Pressure Pressure is defined as, “Force acting on a unit area.” − Force per area (l x w) Gases exert force, or pressure, because they are composed of billions of molecules which are always in motion The more molecules present and the faster they are moving, the greater the pressure Each time a molecule strikes another molecule or an object it exerts a force or pressure against it Air Pressure Air exists in the atmosphere from 100 sea level up to approximately 100 mi miles in space − A person at sea level experiences 100 mi the full weight, or pressure, of the 100 air molecules mi The weight of air pressure is 100 commonly referred to as mi atmospheric pressure “We live submerged at the bottom of an ocean of the element air, which by unquestioned experiments is known to have weight” Torricelli Air Pressure 100 mi At sea level, the pressure exerted by a column of air 1” x 1” is 14.7 pounds
    [Show full text]
  • Measuring Water Content in Compressed Breathing Air Presents a Huge Technical Challenge That Must Take a Wide Range of Parameters Into Account
    MEASURING WATER CONTENT IN COMPRESSED BREATHING AIR IN COMPLIANCE WITH EN 12021:2014 – ULTRA-PRECISE AND ULTRA-RELIABLE WITH POLYMER TECHNOLOGY SPORTS & SAFETY BAUER KOMPRESSOREN WHY PRECISE MEASUREMENT OF WATER CONTENT IS A MATTER OF LIFE OR DEATH. Breathing Air Standard EN 12021:2014 Limit values Oxygen (O2) 21 % ± 1 % Carbon monoxide (CO) 5 ppm Carbon dioxide (CO2) 500 ppm Oil* 0.5 mg/m³ H2O 25 mg/m³ Excessive water content in breathing air causes cylinders to corrode from inside, resulting in material dama- ge and reductions in wall thickness –which will ultimately cause the cylinder to burst! In addition, excessive water content causes dangerous bacteria to proliferate. High water content is even hazardous on cold water dives. If the water content is not below the threshold specified in the standard, scuba regulators may freeze during dives in cold waters – a potentially fatal oc- currence. The moisture and the cold generated by the expanding air cause the breathing valve to ice up. The resulting uncontrolled air release may cause the air supply to fail altogether. Highly precise measurement of water content in compressed breathing air is a matter of life or death for fire- fighters as well as for divers. Because of this, the European Breathing Air StandardEN 12021:2014 exactly defines limits for the absolute water content. The limit value for water in compressed breathing air coming from the compressor is 25 mg/m³. *Limit value for breathing air, the limit value for Nitrox is 0.1 mg / m³ THE CHALLENGE: MEASURING WATER CONTENT IS A COMPLEX TECHNICAL PROCESS.
    [Show full text]
  • Atmospheric Pressure
    Meteorology and the Dynamics of Severe Weather at Sea (Back to Basics) • Sea-level pressure (2D of the 3D) • Fronts (temperature boundaries) • Highs and lows (weather systems) • The weather “pattern” (500 mb charts) • Putting it all together www.weather.gov www.opc.ncep.noaa.gov Joe Sienkiewicz NOAA / NWS Ocean Prediction Center College Park, MD USA Why sea-level pressure? U.S. NOAA JMA South Africa Brazil ATMOSPHERIC PRESSURE 7 Feb 1861 – First marine storm warning Adm. Robert Fitzroy Barometric pressure • The pressure exerted by the atmosphere as a consequence of gravitational attraction exerted upon the "column" of air lying directly above the point in question. (AMS Glossary) Average Sea-Level Pressure 1013.25 (mb millibars, hPa – hecto Pascals) 1018 mb 1022 mb Barometric pressure • 2 dimensional reflection of the 3 dimensional density distribution. (Joe) Average Sea-Level Pressure 1013.25 (mb millibars, hPa – hecto Pascals) 1018 mb 1022 mb 1018 1022 1022 1018 1018 1022 • Temperature distribution is the most important regulator of atmospheric density! 1018 1022 1022 1018 1018 1022 Pressure ~ Density ~ Temperature Pressure Gradient ~ Wind Dir/Spd 1018 1022 1022 1018 1018 1022 Temperature distribution ~ Wind Dir/Spd Hi If earth were not rotating – Highs would fill lows (Coriolis effect) Hi Instead winds blow inward toward lows and outward from highs Some thoughts… observing the weather • Routine observation of weather and logging • Watch change discussion • Changes during off going watch • Anticipated changes oncoming • Barometric trace
    [Show full text]