ANNEX Q TO MARS CORRECT: CRITIQUE OF ALL NASA MARS WEATHER DATA MSL Year 2 to 3 Winter (Ls 90 to Ls 180, Sols 1,213 to 1,392)

Size: px
Start display at page:

Download "ANNEX Q TO MARS CORRECT: CRITIQUE OF ALL NASA MARS WEATHER DATA MSL Year 2 to 3 Winter (Ls 90 to Ls 180, Sols 1,213 to 1,392)"

Transcription

1 ANNEX Q MARS ORRET: RITIQUE OF ALL NASA MARS WEATHER DATA MSL to 3 Winter (Ls 90 to Ls 80, Sols,3 to,39) This Annex reveals all Mars Science Laboratory (MSL) weather data for MSL s Mars to 3 winter. It shows what was published by the Rover Environmental Monitoring Station (REMS) Team and JPL. It also reveals what the Roffman Team sees as weather anomalies, and how the REMS Team and JPL altered their data after we color-highlighted what was off the expected temperature and pressure curves. Q-

2 On Table column subjects and color codings are as follows: olumn A (Sol). The Martian day is about 39 minutes longer than the terrestrial day. olumn B is solar longitude (Ls). MSL is in the Southern Hemisphere on Mars. The landing was at Ls 50 in winter. Ls 80 begins the spring there. Ls 70 starts summer, Ls 0 starts the fall. Ls 90 starts winter. olumn shows the pressure reported by the REMS Team. olumn D shows the date on Earth. olumn E shows the maximum air temperature. With respect to the freezing point, from 0 at atm pressure it will increase up to 0.0 at atm (about the average pressure on Mars as given by NASA). This is the triple point of water. At lower pressures water will never be liquid. It will change directly between solid and gas phase (sublimation). The temperature for this phase change, the sublimation point, will decrease as the pressure is further decreased olumn F shows minimum air temperature. olumn G shows the air temp. range for each sol. On Earth temperatures can vary by 40 in deserts. In column G where the range is 59 or less yellow background color is used. The world record in a diurnal temperature variation is 0 F (57 ) (from 46 F (8 ) to 56 F ( 49 )) in Browning, Montana (elevation 4,377 feet/,334 meters) on January 3 to 4, 96. There were days in Montana where the temperature changed by 57. olumn H shows temperature range divided by 40. This allows us to compare terrestrial deserts with Gale rater, Mars. How much cooling occurs at night is related to the density of the atmosphere. Here we see the ratio of cooling on a Mars sol to the typical 40 cooling figure for Earth's deserts shown with a green background when that ratio is under.5. For MSY when we altered the devisor from 40 to 57 then 88 of the ratios were altered to or less than, meaning that Martian air pressure is indeed likely much higher than NASA claims. olumn I shows maximum ground temperature. As with terrestrial deserts, the ground on Mars heats more during the day than the air does, and it cools more at night than the air does. In olumn K when the maximum ground temperature is given by REMS is above 0 it is shown with a red background. olumn J shows the minimum ground temperature. When it is -90 or colder the background is in purple. The ground temperatures are not very precise. The requirement was to measure ground brightness temperature over the range from 50 to 300 K with a resolution of K and an accuracy of 0 K. olumn K. Drop in ground temperature day to night. olumn L shows increase in temperature from the mast.5 meters above the ground down to the ground during the daylight hours. In column N anytime there is an increase in temperature of or more this in indicated with a dark blue background. olumn M shows the decrease in temperature from the ground to the air at nights. If the data were valid we would expect similar heating or cooling to occur over the set distance from ground to boom. A quick survey of the data immediately shows that this was not found. In column L we see a variation in heating between 0 and at least 5 with a 54 anomaly on Sol,070. For nighttime cooling any variation from to 9 is shown with a medium blue background. More than that is shown with a dark blue background. olumn N shows the pressure for the same Ls in MSL. olumn O shows the absolute value of the change in pressure in scals from the same Ls in the previous year (olumn [M] - []). olumn P shows the original pressure for the same Ls in MSL before JPL revised their data. olumn Q shows the Ls during. olumn R shows the for the sol in. olumn S shows the for the sol in. All sols in MSL and have opacity listed as sunny which seems dubious. olumn T shows comments, if any. Q-

3 SOL YELLOW IF <60 /40 GREEN IF <.5 RED IF > 0 PURPLE = >-90 OR OLDER DAY Yellow numbers = -80 to -89, red background = -90 or colder drop IN BLUE =>0 IN PURPLE = >0 AT IN MSL /4/ YELLOW = > 7 ) -6 BEFORE OMMENTS 90 N/A M M FIRST DAY OF WINTER /5/ N/A M M /6/ N/A H M Max ground temp seems too warm for this Ls /7/ N/A M H /8/ N/A M H Max ground temp seems too warm for this Ls /9/ N/A M M /0/ N/A M M // N/A M H Max ground temp seems too warm for this Ls. Q-3

4 SOL /40 DAY IN IN BEFORE OMMENTS // N/A M M Max ground temp seems too warm for this Ls /3/ N/A M M Max ground 0 elsius temp seems way too warm fo this Ls. See Figure /4/ N/A M M See above /5/ N/A M M Above freezing ground temp but 98 degrees elsius (76.4F) colder at night. WHY? /6/ N/A M M /7/ N/A M M Ground high above /8/ N/A M M Ground high above /9/ N/A M H Ground high above /0/ N/A M M Ground high above // N/A M M Q-4

5 SOL /40 DAY IN IN BEFORE OMMENTS // N/A M M Ground high above /3/ N/A M M Ground high above /4/ N/A M M Ground high above 0 Ground high still above 0, /6/ N/A M H air lows seem stuck.at -88. SEE FIGURE BELOW /7/ N/A M H SEE FIGURE BELOW /8/ N/A M H Ground high above /9/ N/A M H SEE FIGURE BELOW /30/ N/A M M /3/ N/A M M Ground high above 0 SEE FIGURE BELOW. Ground high above 0 SEE FIGURE BELOW. Q-5

6 SOL /40 DAY IN IN BEFORE OMMENTS // N/A M M New high in ground temp for this month (Mars month 4). Previous high 6- in MSL // N/A M M SEE FIGURE BELOW. New low in ground temp for this month (Mars month 4). Previous low -99 this year. -97 in MSL Largest ground temperature range this winter SEE FIGURE BELOW /3/ N/A M M Ground high above /4/ N/A M H Ground high above /5/ N/A M M /6/ N/A M M /7/ N/A M M /8/ N/A M M /9/ N/A M M /0/ N/A M M Major drop in air temp high, but not in air temp low // N/A M M Q-6

7 SOL /40 DAY IN IN BEFORE OMMENTS // N/A M M /3/ N/A M M /4/ N/A M M /5/ N/A M M /6/ N/A M M /7/ N/A M M /8/ N/A M M /9/ N/A M M /0/ N/A M M // N/A M M // N/A M M /3/ N/A M M /4/ N/A M M /5/ N/A M M Q-7

8 SOL /40 DAY IN IN BEFORE OMMENTS /6/ N/A M M /7/ N/A M H /8/ N/A M M /9/ N/A M M // N/A M M /3/ N/A M M /4/ N/A M M /5/ M N/A M H /6/ N/A M M /7/ N/A M M /8/ N/A M M /9/ N/A M M /0/ N/A H M Original was Low, but NASA ler altered all Low Q-8

9 SOL /40 DAY IN IN BEFORE OMMENTS // N/A M M -37 high air temp likely wrong, no corresponding usually cold night air temp. See revision on line below // N/A H M This line shows how REMS/JPL revised data for Sol 78 after we pointed out above the problems with a -37 high air temperature // N/A H M /3/ N/A H M /4/ N/A H M /5/ N/A M M /6/ N/A H M /7/ N/A M M /8/ N/A M M /9/ N/A M M /0/ N/A M M // N/A M (was N/A ) Q-9

10 SOL /40 DAY IN IN BEFORE OMMENTS N/A 3//06 N/A N/A N/A N/A N/A N/A N/A N/A N/A N/A N/A 5 N/A N/A M 6 N/A 3/3/06 N/A N/A N/A N/A N/A N/A N/A N/A N/A N/A N/A 6 N/A N/A M /4/ N/A H M /5/ N/A H M /6/ N/A M M /7/ N/A M M /8/ N/A M M /9/ N/A M M /30/ N/A M M /3/ N/A M M // N/A M H // N/A M H // N/A M H Pressure spike will likely be declared a typographical error. See Figures 3, 4, and 5 below. Watch for JPL to alter this data. PREDIN ABOVE FULFILLED! See Figure /3/ N/A M H Pressure is higher than the 50 transducer capability. Watch for JPL to alter this data. Q-0

11 SOL /40 DAY IN IN BEFORE OMMENTS /3/ N/A M H PREDIN ABOVE FULFILLED. See Figure /4/ N/A M H Back to "normal" pressure for this time of year /5/ N/A H H /6/ N/A M H /7/ N/A H H /8/ N/A H M /0/ N/A H M // N/A H M // N/A H M /3/ N/A M H /4/ N/A H H /5/ N/A H H /6/ N/A H H /7/ N/A H H Q-

12 SOL /40 DAY IN IN BEFORE OMMENTS /8/ N/A H H /9/ N/A H H /0/ N/A H H // N/A H H // N/A H H /3/ N/A H H /4/ N/A H H /5/ N/A H H /6/ N/A H H PREDITION: At this rate JPL should claim a minimum pressure of about 78 to 730 around Ls 47 to 50 between MSL Sols 33 and /7/ N/A H H /8/ N/A H M /9/ N/A H H /30/ N/A H M // N/A H M Q-

13 SOL /40 DAY IN IN BEFORE OMMENTS Note: Prediction made on Sol 33 about Ls of minimum pressures was accessed by NASA San Diego IP addess on 5/4/06 at Sol 39 was the first sol in the winter with an identical pressure to (735 ) // N/A H M In the MSL Autumn data there was only sol (45) with an initial report of idetical pressure to the previous year. Based on highly unusual temperatures we predicted that JPL would alter the data and they did. Pressure on Sol 45 was altered from 907 to 903. The temperatures were also altered (see The last agreement between pressures on identical sols was for the summer season, but NASA has altered some pressures on a continuing basis /3/ N/A H H /4/ N/A H H /5/ N/A H H /6/ N/A H H Low pressure for Q-3

14 SOL /40 DAY IN IN BEFORE OMMENTS /7/ N/A H H Low Pressure for is tied on /8/ N/A H H First day over freezing since Sol 36, Pressure remains tied with last year's low at /9/ N/A H H Pressure remains tied with last year's low at /0/ N/A H H // N/A H H END OF MSL BEGIN MSL 3, ONTINUE WINTER REPORT ON NEXT PAGE Q-4

15 SOL /40 DAY IN IN BEFORE OMMENTS A B SOL /40 DAY IN IN AT IN MSL 3 BEFORE 3 OMMENTS (AND ORRESPONDING SOL NUMBER) // N/A H H (670) /3/ N/A H H (67) /4/ N/A H H (67) /5/ N/A H H (673) /7/ N/A H H (674) /8/ N/A H H (675) /9/ N/A H H (676) /0/ N/A H M (677) // N/A H M (678) // N/A H M (679) Q-5

16 SOL /40 DAY IN IN BEFORE OMMENTS /3/ N/A H M (680) /4/ N/A M M (68) /5/ N/A M H (68) /6/ N/A H H (683) /7/ N/A H M (684) /8/ N/A H H (685) /9/ N/A H H (686) /30/ N/A H H (687) /3/ N/A H H (688) // N/A H H (689) // N/A H H (690) /3/ N/A H H (69) /4/ N/A H H (69) /5/ N/A H H (693) /6/ N/A H H (694) /7/ N/A H H (695) /8/ N/A H H (696) /9/ N/A H H (697) /0/ N/A H H (698) // (699) N/A H H Q-6

17 SOL /40 DAY IN IN BEFORE OMMENTS (700) // N/A H H Note: 7 degree increase in max air temp from previous sol /3/ N/A H H (70) /4/ N/A H H (70) /5/ N/A H H (703) /6/ N/A H H (704) /7/ N/A H H (705) /8/ N/A H H (706) /9/ N/A H H (707) /0/ N/A H H (708) Largest air temperature range this winter (-77 ) // N/A H H (709) /3/ N/A H H (70) Odd that max air temp drops so much while max ground temp. climbs so high /4/ N/A H H (7) /5/ N/A H H (7) /6/ N/A H H (73) /7/ N/A H M (74) /8/ N/A H M (75) /9/ N/A H H (76) Q-7

18 SOL /40 DAY IN IN BEFORE OMMENTS /30/ N/A H H (77) // N/A H H (78) // N/A H H (79) Largest air temperature range this winter (-77 ) N/A 7/3/06 N/A N/A N/A N/A N/A N/A N/A N/A N/A 76 N/A 78 N/A N/A H (70) N/A 7/4/06 N/A N/A N/A N/A N/A N/A N/A N/A N/A 76 N/A 79 N/A N/A H (7) N/A 7/5/06 N/A N/A N/A N/A N/A N/A N/A N/A N/A 760 N/A 79 N/A N/A H (7) N/A SOL 7/6/06 N/A N/A N/A N/A N/A N/A N/A N/A N/A 76 N/A 80 N/A N/A H /40 DAY TIME IN IN AT IN MSL 3 BEFORE 3 (73) FIRST DAY OF SPRING - NO DATA AVAILABLE AGAIN UNTIL SOL 398 AT LS 84 SOL THIS DAY BAK IN Q-8

Atmospheric & Ocean Circulation-

Atmospheric & Ocean Circulation- Atmospheric & Ocean Circulation- Overview: Atmosphere & Climate Atmospheric layers Heating at different latitudes Atmospheric convection cells (Hadley, Ferrel, Polar) Coriolis Force Generation of winds

More information

National Renewable Energy Laboratory. Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009

National Renewable Energy Laboratory. Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009 National Renewable Energy Laboratory Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009 Prepared for: National Renewable Energy Laboratory 1617 Cole Boulevard

More information

Chapter: Atmosphere Section 3: Air Movement

Chapter: Atmosphere Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 3: Air Movement We will learn about Air Movement=Wind -Why different latitudes on Earth will receive different amounts of Solar Energy -The Coriolis Effect

More information

PURE SUBSTANCE. Nitrogen and gaseous air are pure substances.

PURE SUBSTANCE. Nitrogen and gaseous air are pure substances. CLASS Third Units PURE SUBSTANCE Pure substance: A substance that has a fixed chemical composition throughout. Air is a mixture of several gases, but it is considered to be a pure substance. Nitrogen and

More information

renewable energy projects by renewable energy people

renewable energy projects by renewable energy people renewable energy projects by renewable energy people Our Services Full lifecycle services across renewable energy sectors 2 Time variant energy yield analysis A case study Presenter: Daniel Marmander Date:

More information

Atmospheric & Ocean Circulation- I

Atmospheric & Ocean Circulation- I Atmospheric & Ocean Circulation- I First: need to understand basic Earth s Energy Balance 1) Incoming radiation 2) Albedo (reflectivity) 3) Blackbody Radiation Atm/ Ocean movement ultimately derives from

More information

Wind Regimes 1. 1 Wind Regimes

Wind Regimes 1. 1 Wind Regimes Wind Regimes 1 1 Wind Regimes The proper design of a wind turbine for a site requires an accurate characterization of the wind at the site where it will operate. This requires an understanding of the sources

More information

Experiment. THE RELATIONSHIP BETWEEN VOLUME AND TEMPERATURE, i.e.,charles Law. By Dale A. Hammond, PhD, Brigham Young University Hawaii

Experiment. THE RELATIONSHIP BETWEEN VOLUME AND TEMPERATURE, i.e.,charles Law. By Dale A. Hammond, PhD, Brigham Young University Hawaii Experiment THE RELATIONSHIP BETWEEN VOLUME AND TEMPERATURE, i.e.,charles Law By Dale A. Hammond, PhD, Brigham Young University Hawaii The objectives of this experiment are to... LEARNING OBJECTIVES introduce

More information

Andrew Carter. Dry Ice: Sublimating underwater, Forming a Cloud of CO 2, and CO 2 gas spilling over an edge.

Andrew Carter. Dry Ice: Sublimating underwater, Forming a Cloud of CO 2, and CO 2 gas spilling over an edge. Flow Visualization MCEN 5151, Spring 2011 Andrew Carter Team Project 3 5/4/11 Dry Ice: Sublimating underwater, Forming a Cloud of CO 2, and CO 2 gas spilling over an edge. Purpose: The objective of this

More information

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of 6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of elements comprise the largest portion of oceans and atmosphere

More information

Chapter 4: Moisture and Atmospheric Stability The hydrologic cycle

Chapter 4: Moisture and Atmospheric Stability The hydrologic cycle Chapter 4: Moisture and Atmospheric Stability The hydrologic cycle from: USGS http://water.usgs.gov/edu/watercycle.html Evaporation: enough water to cover the entire surface of Earth to 1 meter cycles

More information

Meteorology. Circle the letter that corresponds to the correct answer

Meteorology. Circle the letter that corresponds to the correct answer Chapter 4 Worksheet 3 Meteorology Name: Circle the letter that corresponds to the correct answer 1) Natural convection and turbulence are most likely to occur when: a) temperature decreases rapidly with

More information

Hydrostatics Physics Lab XI

Hydrostatics Physics Lab XI Hydrostatics Physics Lab XI Objective Students will discover the basic principles of buoyancy in a fluid. Students will also quantitatively demonstrate the variance of pressure with immersion depth in

More information

3/30/2013. Vapor Pressure and Changes of State Phase Diagrams. Chapter 10 Sections 8, 9

3/30/2013. Vapor Pressure and Changes of State Phase Diagrams. Chapter 10 Sections 8, 9 Vapor Pressure and Changes of State Chapter 10 Sections 8, 9 Vapor Pressure In a closed container, liquid evaporates. The vapor starts to condensate. Condensation and evaporation happens simultaneously.

More information

CORESTA RECOMMENDED METHOD N 6

CORESTA RECOMMENDED METHOD N 6 CORESTA RECOMMENDED METHOD N 6 DETERMINATION OF VENTILATION DEFINITIONS AND MEASUREMENT PRINCIPLES (2015 Revision September 2016) 1. SCOPE This CORESTA Recommended Method specifies a method for the determination

More information

1 Currents. TAKE A LOOK 2. Read a Map In what direction does the Gulf Stream flow?

1 Currents. TAKE A LOOK 2. Read a Map In what direction does the Gulf Stream flow? CHAPTER 5 1 Currents SECTION The Movement of Ocean Water BEFORE YOU READ After you read this section, you should be able to answer these questions: What factors affect ocean currents? Why are ocean currents

More information

Assessment Schedule 2016 Earth and Space Science: Demonstrate understanding of processes in the ocean system (91413)

Assessment Schedule 2016 Earth and Space Science: Demonstrate understanding of processes in the ocean system (91413) NCEA Level 3 Earth & Space Science (91413) 2016 page 1 of 6 Assessment Schedule 2016 Earth and Space Science: Demonstrate processes in the ocean system (91413) Evidence Statement Q Evidence with with Excellence

More information

Site Summary. Wind Resource Summary. Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser

Site Summary. Wind Resource Summary. Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser Site Summary Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser Station ID: 2857 Latitude: 55 7 45.8 N Longitude: 162 16 10.6 W Tower Type: 30 m NRG Tall

More information

Chapter 12. Properties of Gases

Chapter 12. Properties of Gases Properties of Gases Each state of matter has its own properties. Gases have unique properties because the distance between the particles of a gas is much greater than the distance between the particles

More information

Predicting climate conditions for turbine performance

Predicting climate conditions for turbine performance Predicting climate conditions for turbine performance Mark Žagar, Vinay Belathur Krishna, Alvaro Matesanz Gil Vestas Data Engineering & Analytics / Advanced Plant Modelling Resource assessment, power curve,

More information

Compiled by: B Beard. Approved by: SH Carstens. Description of requirements and procedures for compact provers to be used as verification standards.

Compiled by: B Beard. Approved by: SH Carstens. Description of requirements and procedures for compact provers to be used as verification standards. 1. Scope Description of requirements and procedures for compact provers to be used as verification standards. 2. Reference documents Trade Metrology Act SANS1698 3. Policy A. BASIC REQUIREMENTS Compact

More information

Wind Project Siting and Permitting Blaine Loos

Wind Project Siting and Permitting Blaine Loos Wind Project Siting and Permitting Blaine Loos Energy Project Analyst Center for Wind Energy at James Madison University Wind Project Siting and Permitting The Energy in Wind Resource Assessment (Macro-siting)

More information

Thermodynamics ERT 206 Properties of Pure Substance HANNA ILYANI ZULHAIMI

Thermodynamics ERT 206 Properties of Pure Substance HANNA ILYANI ZULHAIMI Thermodynamics ERT 206 Properties of Pure Substance HANNA ILYANI ZULHAIMI Outline: Pure Substance Phases of pure substance Phase change process of pure substance Saturation temperature and saturation pressure

More information

4. Using the kinetic molecular theory, explain why a gas can be easily compressed, while a liquid and a solid cannot?

4. Using the kinetic molecular theory, explain why a gas can be easily compressed, while a liquid and a solid cannot? Name Period HW 1 Worksheet (Goals 1-4) - Kinetic Molecular Theory 1. Describe how gases, liquids, and solids compare using the following table. Solids Liquids Gases Volume (definite or indefinite) Molecular

More information

Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection.

Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection. Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection. -Differences in density affect the circulation of fluids. Cold air is

More information

HKA TECHNOLOGIES INC. TEMPERATURE COMPENSATION

HKA TECHNOLOGIES INC. TEMPERATURE COMPENSATION HKA TECHNOLOGIES INC. TEMPERATURE COMPENSATION Different Methods of Air Leak Testing Conventional vs Bell Jar Pressure Decay and Differential Pressure Decay Mass Flow and Differential Mass Flow HKA mainly

More information

Chapter: Atmosphere Section 3: Air Movement

Chapter: Atmosphere Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 3: Air Movement We will learn about: -Air Movement=Wind -Why different latitudes on Earth will receive different amounts of Solar Energy -The Coriolis Effect

More information

Gas Pressure. Pressure is the force exerted per unit area by gas molecules as they strike the surfaces around them.

Gas Pressure. Pressure is the force exerted per unit area by gas molecules as they strike the surfaces around them. Chapter 5 Gases Gas Gases are composed of particles that are moving around very fast in their container(s). These particles moves in straight lines until they collides with either the container wall or

More information

Santa Ana Winds. Surface weather map showing typical Santa Ana conditions.

Santa Ana Winds. Surface weather map showing typical Santa Ana conditions. Santa Ana Winds Surface weather map showing typical Santa Ana conditions. High Desert Elevation ~1500-2000 ft Santa Ana Winds ~1500 meters 0 meters Santa Ana Winds ~875 mb ~1500 meters ~875 mb Horizontal

More information

Retention Time Locking: Concepts and Applications. Application

Retention Time Locking: Concepts and Applications. Application Retention Time Locking: Concepts and Applications Application Gas Chromatography December 1997 Authors Vince Giarrocco Bruce Quimby Matthew Klee Agilent Technologies, Inc. 2850 Centerville Road Wilmington,

More information

Wind Resource Assessment for NOME (ANVIL MOUNTAIN), ALASKA Date last modified: 5/22/06 Compiled by: Cliff Dolchok

Wind Resource Assessment for NOME (ANVIL MOUNTAIN), ALASKA Date last modified: 5/22/06 Compiled by: Cliff Dolchok 813 W. Northern Lights Blvd. Anchorage, AK 99503 Phone: 907-269-3000 Fax: 907-269-3044 www.akenergyauthority.org SITE SUMMARY Wind Resource Assessment for NOME (ANVIL MOUNTAIN), ALASKA Date last modified:

More information

NMISA NEW GAS FLOW CALIBRATION FACILITY. Deona Jonker 7 October 2013

NMISA NEW GAS FLOW CALIBRATION FACILITY. Deona Jonker 7 October 2013 NMISA NEW GAS FLOW CALIBRATION FACILITY Deona Jonker 7 October 2013 Introduction Flow the total volume of a fluid that flows past a fixed point in a given time Flow measurements used in industry as a means

More information

Chapter 7 Weather and Climate

Chapter 7 Weather and Climate Chapter 7 Weather and Climate *Describe what weather is, what affects it, and where it occurs. *Explain the connection between air pressure and wind. * *Many factors affect a region s weather. * *atmosphere

More information

PVP Copyright 2009 by ASME

PVP Copyright 2009 by ASME Proceedings of PVP 009 009 ASME Pressure Vessel and Piping Division Conference July 6-30, 009, Prague, Czech Republic PVP009-7746 UPDATE OF THE TABULATED «M AND Y» VALUES IN THE NEW REVISIONS OF FRENCH

More information

Requirements and Methods for Calibration of Equipment in Clinical Laboratories. NK Chan (HKRCBTS) 24 August 2007

Requirements and Methods for Calibration of Equipment in Clinical Laboratories. NK Chan (HKRCBTS) 24 August 2007 Requirements and Methods for Calibration of Equipment in Clinical Laboratories NK Chan (HKRCBTS) 24 August 2007 1 Contents Basic Requirements of Equipment Calibration Calibration of Electronic Balance

More information

V. SEA and LAND BREEZES:

V. SEA and LAND BREEZES: V. SEA and LAND BREEZES: A. Pressure largely reflects the weight of overlying air, owing to gravity, and is proportional to mass. Therefore pressure decreases with height. 1. Remember, surface pressure

More information

Bell Work. Compare and contrast warm fronts and cold fronts. What type of weather is associated with a high pressure and low pressure systems?

Bell Work. Compare and contrast warm fronts and cold fronts. What type of weather is associated with a high pressure and low pressure systems? Daily Routine Sit in your appropriate seat quietly Have all necessary materials out All back packs on the floor All cell phones on silent and away in backpacks All music devices off and headphones out

More information

Pressure measurement explained

Pressure measurement explained Rev A1, May 25 th, 2018 Sens4Knowledge Sens4 A/S Nordre Strandvej 119 G 3150 Hellebaek Denmark Phone: +45 8844 7044 Email: info@sens4.com www.sens4.com Introduction Pressure is defined as the force per

More information

What causes the tides in the ocean?

What causes the tides in the ocean? What causes the tides in the ocean? By NASA and NOAA on 02.09.17 Word Count 809 Level MAX Flying gulls on Morro Strand State Beach, California, at low tide. Morro Rock is seen in the background. Photo

More information

Technical Note. Determining the surface tension of liquids by measurements on pendant drops

Technical Note. Determining the surface tension of liquids by measurements on pendant drops Technical Note Pendant Drop Measurements Technical note: TN316e Industry section: all Author: FT, TW Date: 12/2010 Method: Drop Shape Analyzer DSA100 Keywords: Methods, surface tension, interfacial tension,

More information

NEAR-SURFACE FACETED CRYSTALS ON A SLOPE COVERED WITH STONE PINE TREES. Peter Höller*

NEAR-SURFACE FACETED CRYSTALS ON A SLOPE COVERED WITH STONE PINE TREES. Peter Höller* NEAR-SURFACE FACETED CRYSTALS ON A SLOPE COVERED WITH STONE PINE TREES Peter Höller* ABSTRACT: This paper presents snow surface temperature measurements as well as snow temperature investigations in the

More information

Identify the Principal Investigator for this data set, including general affiliation, if applicable.

Identify the Principal Investigator for this data set, including general affiliation, if applicable. 1. TITLE 1.1. Data set identification Soil water potential measured by tensiometer 1.2. Revision date of this document (yy/mm/dd) 05/99 2. INVESTIGATOR(S) Identify the Principal Investigator for this data

More information

REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330

REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330 REMINDERS: Midterm 2: Friday, February 28 - lecture material covering chapters 6, 7, and 15 (since first midterm and through Wed lecture) - same Format as first midterm UPCOMING REVIEW SESSIONS: - Thursday,

More information

Pressure and Density Altitude

Pressure and Density Altitude Pressure and Density Altitude Reference Sources Pilot s Handbook of Aeronautical Knowledge o Pages 9-1 to 9-4, Aircraft Performance o Pages 9-20 to 9-21, Density Altitude Charts Study Questions 1. Where

More information

USING A PROBABILITY APPROACH TO RANK IN-LINE INSPECTION ANOMALIES FOR EXCAVATION AND FOR SETTING REINSPECTION INTERVALS

USING A PROBABILITY APPROACH TO RANK IN-LINE INSPECTION ANOMALIES FOR EXCAVATION AND FOR SETTING REINSPECTION INTERVALS USING A PROBABILITY APPROACH TO RANK IN-LINE INSPECTION ANOMALIES FOR EXCAVATION AND FOR SETTING REINSPECTION INTERVALS by Dennis C. Johnston and Carolyn E. Kolovich Kiefner & Associates, Inc. P.O. Box

More information

Exit Ticket: Coriolis Effect

Exit Ticket: Coriolis Effect Exit Ticket: Coriolis Effect 1. How does the Coriolis Effect influence the path of projectiles or wind traveling through the atmosphere? Causes them to curve 2. In which direction does the Coriolis Effect

More information

What s UP in the. Pacific Ocean? Learning Objectives

What s UP in the. Pacific Ocean? Learning Objectives What s UP in the Learning Objectives Pacific Ocean? In this module, you will follow a bluefin tuna on a spectacular migratory journey up and down the West Coast of North America and back and forth across

More information

ELEVATION CORRECTION FACTORS FOR RADON MONITORS*

ELEVATION CORRECTION FACTORS FOR RADON MONITORS* ELEVATION CORRECTION FACTORS FOR E-PERM@ RADON MONITORS* P. Kotrappa and L. R. Stiefl Abstract-E-PERMm radon monitors are based on the principle of electret ion chambers and are usually calibrated in a

More information

3 1 PRESSURE. This is illustrated in Fig. 3 3.

3 1 PRESSURE. This is illustrated in Fig. 3 3. P = 3 psi 66 FLUID MECHANICS 150 pounds A feet = 50 in P = 6 psi P = s W 150 lbf n = = 50 in = 3 psi A feet FIGURE 3 1 The normal stress (or pressure ) on the feet of a chubby person is much greater than

More information

Chapter 13 Fluids. Copyright 2009 Pearson Education, Inc.

Chapter 13 Fluids. Copyright 2009 Pearson Education, Inc. Chapter 13 Fluids Phases of Matter Density and Specific Gravity Pressure in Fluids Atmospheric Pressure and Gauge Pressure Pascal s Principle Units of Chapter 13 Measurement of Pressure; Gauges and the

More information

Presented to the International Technical Rescue Symposium, November Abstract

Presented to the International Technical Rescue Symposium, November Abstract Presented to the International Technical Rescue Symposium, November 21 Presented by: Chuck Weber, PMI Quality Manager Abstract This paper presents the results of 162 individual drop tests performed at

More information

Chapter 13 Temperature, Kinetic Theory, and the Gas Laws 497

Chapter 13 Temperature, Kinetic Theory, and the Gas Laws 497 Chapter 13 Temperature, Kinetic Theory, and the Gas Laws 497 Figure 13.25 This photograph of Apollo 17 Commander Eugene Cernan driving the lunar rover on the Moon in 1972 looks as though it was taken at

More information

Student Exploration: Boyle s Law and Charles Law

Student Exploration: Boyle s Law and Charles Law Name: Date: Student Exploration: Boyle s Law and Charles Law Vocabulary: absolute zero, Boyle s law, Charles law, Gay-Lussac s law, Kelvin scale, pressure Prior Knowledge Question (Do this BEFORE using

More information

Pendant Drop Measurements

Pendant Drop Measurements KRÜSS pplication Note TN316d Page 1 Pendant Drop Measurements pplication note: TN316d Industry section: all uthor: Dr. Tobias Winkler Date: December 2010 Method: Drop Shape nalysis System DS100 Drop Shape

More information

Skills Key Words. Task. Key words. Write a definition for each of the key words listed below. Hypothesis. Variable. Prediction. Method.

Skills Key Words. Task. Key words. Write a definition for each of the key words listed below. Hypothesis. Variable. Prediction. Method. KS3 Science Skills Skills Key Words Write a definition for each of the key words listed below Key words Hypothesis Variable Prediction Method Hazard Precision Accuracy Repeatability Reproducibility Anomaly

More information

Vortex Flow Meter Wafer or Flange Connection. - Steam - Liquid - Gas

Vortex Flow Meter Wafer or Flange Connection. - Steam - Liquid - Gas Vortex Flow Meter Wafer or Flange Connection - Steam - Liquid - Gas Working Principle & Circuit Diagram Working Principle When a column body placed in flowing fluids in pipe, a series of vortices will

More information

Buckland Wind Resource Report

Buckland Wind Resource Report Buckland Wind Resource Report By: Douglas Vaught, P.E., V3 Energy LLC, Eagle River, Alaska Date: September 17, 2010 Buckland met tower; D. Vaught photo Contents Summary... 2 Test Site Location... 2 Photographs...

More information

WIND DATA REPORT. Vinalhaven

WIND DATA REPORT. Vinalhaven WIND DATA REPORT Vinalhaven January - December, 2003 Prepared for Fox Islands Electric Cooperative by Anthony L. Rogers May 12, 2004 Report template version 1.1 Renewable Energy Research Laboratory 160

More information

Section 1. Global Wind Patterns and Weather. What Do You See? Think About It. Investigate. Learning Outcomes

Section 1. Global Wind Patterns and Weather. What Do You See? Think About It. Investigate. Learning Outcomes Chapter 5 Winds, Oceans, Weather, and Climate Section 1 Global Wind Patterns and Weather What Do You See? Learning Outcomes In this section, you will Determine the effects of Earth s rotation and the uneven

More information

An Engineering Approach to Precision Ammunition Development. Justin Pierce Design Engineer Government and International Contracts ATK Sporting Group

An Engineering Approach to Precision Ammunition Development. Justin Pierce Design Engineer Government and International Contracts ATK Sporting Group An Engineering Approach to Precision Ammunition Development Justin Pierce Design Engineer Government and International Contracts ATK Sporting Group 1 Background Federal Premium extensive experience with

More information

TROUBLESHOOTING. Dwell Volume Revisited. Gradient transfer does not have to be problematic.

TROUBLESHOOTING. Dwell Volume Revisited. Gradient transfer does not have to be problematic. 458 LCGC NORTH AMERICA VOLUME 24 NUMBER 5 MAY 2006 www.chromatographyonline.com LC TROUBLESHOOTING Dwell Volume Revisited Gradient transfer does not have to be problematic. John W. Dolan LC Troubleshooting

More information

Introductory Physics PHYS101

Introductory Physics PHYS101 Introductory Physics PHYS101 Dr Richard H. Cyburt Office Hours Assistant Professor of Physics My office: 402c in the Science Building My phone: (304) 384-6006 My email: rcyburt@concord.edu TRF 9:30-11:00am

More information

GNSS Technology for the Determination of Real-Time Tidal Information

GNSS Technology for the Determination of Real-Time Tidal Information GNSS Technology for the Determination of Real-Time Tidal Information Benjamin Kidder C-Nav Positioning Solutions European region Outline of Topics Covered Introduction to Tides Past and Present Methods

More information

Atmospheric Rossby Waves in Fall 2011: Analysis of Zonal Wind Speed and 500hPa Heights in the Northern and Southern Hemispheres

Atmospheric Rossby Waves in Fall 2011: Analysis of Zonal Wind Speed and 500hPa Heights in the Northern and Southern Hemispheres Atmospheric Rossby Waves in Fall 211: Analysis of Zonal Wind Speed and 5hPa Heights in the Northern and Southern s Samuel Cook, Craig Eckstein, and Samantha Santeiu Department of Atmospheric and Geological

More information

Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined

Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined to use for answering the questions. Essential Question:

More information

SG TF. Q = 963 Cv (P1 - P2)(P1 + P2) TECHNICAL INFORMATION. Flow Q (GPM)

SG TF. Q = 963 Cv (P1 - P2)(P1 + P2) TECHNICAL INFORMATION. Flow Q (GPM) TECHNICAL INFORMATION BuTech designs all pressure-containing equipment to meet or exceed the applicable requirements of Section VIII, Division1 or Division 2 of the ASME Boiler and Pressure Vessel Code

More information

Atmospheric Rossby Waves Fall 2012: Analysis of Northern and Southern 500hPa Height Fields and Zonal Wind Speed

Atmospheric Rossby Waves Fall 2012: Analysis of Northern and Southern 500hPa Height Fields and Zonal Wind Speed Atmospheric Rossby Waves Fall 12: Analysis of Northern and Southern hpa Height Fields and Zonal Wind Speed Samuel Schreier, Sarah Stewart, Ashley Christensen, and Tristan Morath Department of Atmospheric

More information

Envs, Geol, Phys 112: Global Climate. Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10

Envs, Geol, Phys 112: Global Climate. Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10 Exam 1 Review Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10 Location on Earth (L04) Latitude & Longitude great circles, prime meridian, time zones, cardinal points, azimuth

More information

Modeling Approaches to Increase the Efficiency of Clear-Point- Based Solubility Characterization

Modeling Approaches to Increase the Efficiency of Clear-Point- Based Solubility Characterization Modeling Approaches to Increase the Efficiency of Clear-Point- Based Solubility Characterization Paul Larsen, Dallin Whitaker Crop Protection Product Design & Process R&D OCTOBER 4, 2018 TECHNOBIS CRYSTALLI

More information

Operating Instructions METTLER TOLEDO Pipette Check Application for AX and MX/UMX Balances Version 1.xx

Operating Instructions METTLER TOLEDO Pipette Check Application for AX and MX/UMX Balances Version 1.xx Operating Instructions METTLER TOLEDO Pipette Check Application for AX and MX/UMX Balances Version 1.xx Contents 1 Introducing the Pipette Check application... 3 2 important notes... 3 3 Selecting the

More information

THE WAY THE VENTURI AND ORIFICES WORK

THE WAY THE VENTURI AND ORIFICES WORK Manual M000 rev0 03/00 THE WAY THE VENTURI AND ORIFICES WORK CHAPTER All industrial combustion systems are made up of 3 main parts: ) The mixer which mixes fuel gas with combustion air in the correct ratio

More information

Predicted Dispense Volume vs. Gravimetric Measurement for the MICROLAB 600. November 2010

Predicted Dispense Volume vs. Gravimetric Measurement for the MICROLAB 600. November 2010 Predicted Dispense Volume vs. Gravimetric Measurement for the MICROLAB 600 November 2010 Table of Contents ``Abstract...3 ``Introduction...4 ``Methods & Results...6 ``Data Analysis...9 ``Conclusion...12

More information

Air Pressure and Wind

Air Pressure and Wind Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways. The

More information

DEPARTMENT OF THE NAVY DIVISION NEWPORT OFFICE OF COUNSEL PHONE: FAX: DSN:

DEPARTMENT OF THE NAVY DIVISION NEWPORT OFFICE OF COUNSEL PHONE: FAX: DSN: IMAVSBA WARFARE CENTERS NEWPORT DEPARTMENT OF THE NAVY NAVAL UNDERSEA WARFARE CENTER DIVISION NEWPORT OFFICE OF COUNSEL PHONE: 401 832-3653 FAX: 401 832-4432 DSN: 432-3653 Attorney Docket No. 85031 Date:

More information

3/6/2001 Fig. 6-1, p.142

3/6/2001 Fig. 6-1, p.142 First GOES 11 image http://visible earth.nasa.g ov/view_rec. php?id=190 Air-born dust from the Sahara Desert, Feb. 2001 Fig. 6-CO, p.140 dust from China over Japan. 3/5/2001 FIGURE 6.1 A model of the atmosphere

More information

Civil Air Patrol Auxiliary of the United States Air Force

Civil Air Patrol Auxiliary of the United States Air Force Mountain Flying Qualification Course Civil Air Patrol Auxiliary of the United States Air Force DENSITY ALTITUDE Pressure Altitude Pressure Altitude: Absolute altitude corrected for non-standard atmospheric

More information

Ground Flat Stock & Drill Rod

Ground Flat Stock & Drill Rod NOW OFFERING 140 NEW SIZES TO THE INDUSTRY S BIGGEST SELECTION! NOW AVAILABLE 72" NUTEC42 72" A-2 GROUND FLAT STOCK EXPANDED DRILL ROD LINE Ground Flat Stock & Drill Rod Our conformance to specifications

More information

Why Are Temperatures Different Near the Coasts and Inland?

Why Are Temperatures Different Near the Coasts and Inland? 2.6 Investigate Why Are Temperatures Different Near the Coasts and Inland? Earlier in this Learning Set, you analyzed climate maps that indicated the effects of latitude on temperature. The maps are repeated

More information

Pokémon Organized Play Tournament Operation Procedures

Pokémon Organized Play Tournament Operation Procedures Pokémon Organized Play Tournament Operation Procedures Revised: September 20, 2012 Table of Contents 1. Introduction...3 2. Pre-Tournament Announcements...3 3. Approved Tournament Styles...3 3.1. Swiss...3

More information

Chapter 10 Fluids. Which has a greater density? Ch 10: Problem 5. Ch 10: Problem Phases of Matter Density and Specific Gravity

Chapter 10 Fluids. Which has a greater density? Ch 10: Problem 5. Ch 10: Problem Phases of Matter Density and Specific Gravity Chapter 10 Fluids 10-1 Phases of Matter The three common phases of matter are solid, liquid, and gas. A solid has a definite shape and size. A liquid has a fixed volume but can be any shape. A gas can

More information

2600T Series Pressure Transmitters Plugged Impulse Line Detection Diagnostic. Pressure Measurement Engineered solutions for all applications

2600T Series Pressure Transmitters Plugged Impulse Line Detection Diagnostic. Pressure Measurement Engineered solutions for all applications Application Description AG/266PILD-EN Rev. C 2600T Series Pressure Transmitters Plugged Impulse Line Detection Diagnostic Pressure Measurement Engineered solutions for all applications Increase plant productivity

More information

Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate

Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate Atmospheric Structure Consists of Layers Separated by Temperature Stratosphere: Temperature

More information

LABORATORY EXERCISE 1 CONTROL VALVE CHARACTERISTICS

LABORATORY EXERCISE 1 CONTROL VALVE CHARACTERISTICS Date: Name: LABORATORY EXERCISE 1 CONTROL VALVE CHARACTERISTICS OBJECTIVE: To demonstrate the relation between valve stem position and the fluid flow through a control valve, for both linear and equal

More information

Chapter. Air Pressure and Wind

Chapter. Air Pressure and Wind Chapter Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. 19.1 Understanding Air Pressure Air Pressure Defined Air pressure

More information

Specific Accreditation Criteria Calibration ISO IEC Annex. Mass and related quantities

Specific Accreditation Criteria Calibration ISO IEC Annex. Mass and related quantities Specific Accreditation Criteria Calibration ISO IEC 17025 Annex Mass and related quantities January 2018 Copyright National Association of Testing Authorities, Australia 2014 This publication is protected

More information

OCEANOGRAPHY STUDY GUIDE

OCEANOGRAPHY STUDY GUIDE OCEANOGRAPHY STUDY GUIDE Chapter 2 Section 1 1. Most abundant salt in ocean. Sodium chloride; NaCl 2. Amount of Earth covered by Water 71% 3. Four oceans: What are they? Atlantic, Pacific, Arctic, Indian

More information

Meteorology. Circle the letter that corresponds to the correct answer

Meteorology. Circle the letter that corresponds to the correct answer Chapter 4 Worksheet 2 Meteorology Name: Circle the letter that corresponds to the correct answer 1) If the air temperature remains constant, evaporating water into the air will the dew point and the relative

More information

Meteorology of Monteverde, Costa Rica 2007

Meteorology of Monteverde, Costa Rica 2007 Meteorology of Monteverde, Costa Rica 2007 Technical Report submitted to the Monteverde Institute Andrew J. Guswa, Associate Professor, Picker Engineering Program Amy L. Rhodes, Associate Professor, Department

More information

Standard Operating Procedure. Air Displacement Pipette Calibration

Standard Operating Procedure. Air Displacement Pipette Calibration University of Colorado at Denver October 28, 2003 - Revision 1.00 Page 1 of 7 1 Background: Standard Operating Procedure An accurate pipette is one of the most important tools in performing accurate analytical

More information

Executive Summary of Accuracy for WINDCUBE 200S

Executive Summary of Accuracy for WINDCUBE 200S Executive Summary of Accuracy for WINDCUBE 200S The potential of offshore wind energy has gained significant interest due to consistent and strong winds, resulting in very high capacity factors compared

More information

METNET Mission for Mars. MetNet. Atmospheric science network for Mars

METNET Mission for Mars. MetNet. Atmospheric science network for Mars MetNet Atmospheric science network for Mars A.-M. Harri (1), R. Pellinen (1), V. Linkin (2), K. Pichkadze (3), M. Uspensky (1), T. Siili (1), A. Lipatov (2), H. Savijärvi (4), V. Vorontsov (3), J.Semenov

More information

Gilbert Kirss Foster. Chapter 10. Properties of Gases The Air We Breathe

Gilbert Kirss Foster. Chapter 10. Properties of Gases The Air We Breathe Gilbert Kirss Foster Chapter 10 Properties of Gases The Air We Breathe Chapter Outline 10.1 The Properties of Gases 10.2 Effusion and the Kinetic Molecular Theory of Gases 10.3 Atmospheric Pressure 10.4

More information

Pressure Measurement

Pressure Measurement Pressure Measurement Manometers Sensors, Transducers Ashish J. Modi Lecturer, Dept. of Mech.Engg., Shri S.V.M. inst. Of Technology, Bharuch Pressure Pressure is a force per unit area exerted by a fluid

More information

M. Mikkonen.

M. Mikkonen. Wind study by using mobile sodar technology M. Mikkonen Oulu University of Applied Sciences, School of Engineering, Oulu, Finland t3mimi00@students.oamk.com Abstract In this paper is presented a concept

More information

1. Matter comes in phases, they are: and! 3. Energy is associated with the phases as well: Gases have the energy, solids the

1. Matter comes in phases, they are: and! 3. Energy is associated with the phases as well: Gases have the energy, solids the Phases Chemistry Notes 1. Matter comes in phases, they are: and! 2. There are six phase changes that you need to know always: Between solid and liquid: & Between liquid and gas: & Between solid and gas:

More information

Ripple Tank. Equipment:

Ripple Tank. Equipment: Ripple Tank Two point source interference patterns Purpose: A single vibration applied to the surface of water produces circular waves that propagate out from that point. If two identical vibrations are

More information

Atmospheric and Ocean Circulation Lab

Atmospheric and Ocean Circulation Lab Atmospheric and Ocean Circulation Lab name Key Objectives: The main goal of this lab is to learn about atmospheric and oceanic circulation and how these two processes are strongly inter-dependent and strongly

More information

An Atlas of Oceanic Internal Solitary Waves (May 2002) by Global Ocean Associates Prepared for the Office of Naval Research - Code 322PO

An Atlas of Oceanic Internal Solitary Waves (May 2002) by Global Ocean Associates Prepared for the Office of Naval Research - Code 322PO Overview is located in the western Pacific Ocean along the west side of the Philippines (between approximately 5 o and 11 o N. latitude and 117 o and 123 o E. longitude). It is a deepwater sea, roughly

More information

Micro Channel Recuperator for a Reverse Brayton Cycle Cryocooler

Micro Channel Recuperator for a Reverse Brayton Cycle Cryocooler Micro Channel Recuperator for a Reverse Brayton Cycle Cryocooler C. Becnel, J. Lagrone, and K. Kelly Mezzo Technologies Baton Rouge, LA USA 70806 ABSTRACT The Missile Defense Agency has supported a research

More information

What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of

What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of the atmosphere. Measuring Wind Wind direction is determined

More information