Near Vertical Incidence Skywave (NVIS)
|
|
- Asher Lewis
- 5 years ago
- Views:
Transcription
1 Near Vertical Incidence Skywave (NVIS) Larry Randall WA5BEN Revision: Issue Date: 17 October 2007
2 Topics Terminology Why do we need NVIS Defining NVIS Relationship between Path Length and MUF Relationship between Layer Height and MUF Required Take-off angles Signal to Noise Ratio (SNR) Antenna Efficiency Points to Ponder Summary
3 Terminology NVIS: Relatively short-range range skywave communication with high take-off angle Take-off angle: The angle of incidence at earth; the angle of the ray for a specific path SSN: Smoothed Sunspot Number MUF: Maximum Usable Frequency; the highest frequency launched from Point A A that will be returned to earth at Point B B LUF: Lowest Usable Frequency; the lowest frequency launched from Point A A that will be returned to earth at Point B B with sufficient strength to overcome path loss and absorption
4 Terminology Short antenna: Any antenna less than ¼ λ for a monopole, or ½ λ for a dipole Feedpoint Resistance: The resistive portion of the impedance at the feedpoint.. It consists of: Radiation Resistance ( R R ): The portion of antenna impedance that results from radiation i.e., the pure resistance that would dissipate the same amount of power that is actually radiated by the antenna Material Resistance and Coil Resistance ( R C ): The resistance of the antenna material and (for a loaded antenna) the resistance of the loading coil(s). Ground Loss ( R G ): The portion of antenna feedpoint resistance that results from warming worms. R R R C R G
5 Terminology F2 Layer The ionized layer of the atmosphere most responsible for usable HF communications. Virtual height falls between 200 and 550 km. F1 Layer The lower F layer, present only during daylight split F F conditions. Virtual height falls between 160 and 250 km. E Layer Primarily a spoiler layer, impacting NVIS only in daylight. Virtual height falls between 95 and 120 km. D Layer Present only in daylight. Absorbs low HF range. Effect is greatest in summer, below 7 MHz.
6 Why do we need NVIS? NVIS is the only reliable mode for wide area Emergency Communication All commercial telephone services including cellular - failed in the area struck by Katrina All remained out for more than 10 days Most repeaters in the area also failed Louisiana statewide trunked system failed NVIS HF radio provided the first (and, for many hours, the only) communication to the outside world and within the disaster area Regional nets (Texas nets, ARES, SATERN, CAP, MARS, TBM, etc.)
7 Defined by distance Wires on the ground Warming Worms Vertically polarized NVIS is not
8 NVIS This presentation will demonstrate: That NVIS is defined best by take-off angle That a given path may be NVIS at some times, non-nvis at others That whether a path is NVIS or non-nvis is dependant upon: SSN Season Time of day Chosen Frequency That NVIS requires a Horizontal antenna That NVIS antenna efficiency is very important That there is an optimum height for an NVIS antenna
9
10 Relationship between Path Length and MUF For the same SSN, on the same date*,, an increase in path length results in an increased MUF The increase in path length results in a decrease in the angle of incidence at the refracting layer A decrease in the angle of incidence at the refracting layer allows the same density to refract higher frequencies * Basic data in this presentation based upon date of 01 Jun 2007 Sunrise = 0619 CDST (1119 UTC) Sunset = 2030 CDST (0130 UTC) Solar Noon = 1324 CDST (1824 UTC) (Sun Lat. = N) Seasonal comparison based upon 01 Dec 2007 Sunrise = 0711 CST (1311 UTC) Sunset = 1720 CST (2320 UTC) Solar Noon = 1215 CST (1815 UTC) (Sun Lat. = S)
11 MUF Comparison June 50, 150, 250, and 350 mile paths 50 miles -- Sherman 7 MHz MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN miles -- Bryan 7 MHz MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN miles San Antonio 7 MHz MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN miles Corpus Christi 7 MHz MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN 150
12 MUF Comparison December 50, 150, 250, and 350 mile paths 50 miles -- Sherman MUF SSN 7 (Dec) MUF SSN 20 (Dec) MUF SSN 50 (Dec) MUF SSN 100 (Dec) MUF SSN 150 (Dec) miles -- Bryan MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN miles San Antonio MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN miles Corpus Christi MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN 150
13 Relationship between Virtual Height and MUF An increase in SSN results in an increase in Virtual Height at the MUF At any SSN, the Virtual Height for a given frequency is maximum when that frequency is equal to the MUF The Virtual Height for a given frequency decreases when the MUF exceeds that frequency Also note that there is a Daylight Hump in Virtual Height that is not related to MUF. This hump is centered on local Solar Noon.
14 Relationship between Virtual Height and MUF Explanation of graphs in next two slides Chart for SSN = 7 Chart for SSN = 50
15 Virtual 3.5 MHz - June DAL-AUS AUS (200 mile path) 5 Virtual 3.5 MHz DAL-AUS Path: Virtual MUF MUF MUF falls falls to to MHz MHz at at SSN SSN = MUF MUF falls falls to to near near MHz MHz at at SSN SSN = V MUF MUF exceeds 3.5 MHz Vir SSN 7 Vir SSN 20 Vir SSN 50 Vir SSN 100 Vir SSN 150 MUF MUF rises rises past past MHz MHz at at SSN SSN = MUF rises past 3.5 MHz at SSN = 7 V 3.5 MHz
16 MUF MUF falls falls to, to, then then below, below, MHz MHz at at SSN SSN = = MUF MUF falls falls to, to, then then below, below, MHz MHz at at SSN SSN = = Virtual 7.3 MHz - June DAL-AUS AUS (200 mile path) MUF MUF falls falls to, to, then then below, below, MHz MHz at at SSN SSN = = Virtual 7.3 MHz DAL-AUS Path: Virtual MUF MUF exceeds 7.3 MHz MUF falls to, then below, 7.3 MHz at SSN = 150 Vir SSN 7 Vir SSN 20 Vir SSN 50 Vir SSN 100 Vir SSN 150
17 Relationship between MUF and Take-off Angle For a given path and frequency, the take-off angle varies: Greatly with seasons Slightly because of day and night variations Markedly during daylight if the frequency is well below the MUF Within narrow limits if the frequency is near and below the MUF The required take-off angle for any frequency X X decreases when the MUF rises past that frequency
18 MUF and Take- off Angle SSN=7 to SSN=150 DAL Sherman (50 mile path - June) MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN T Angle 3.5 SSN 7 T Angle 3.5 SSN 20 T Angle 3.5 SSN 50 T Angle 3.5 SSN 100 T Angle 3.5 SSN 150 F1 Layer Note symmetry about local solar noon (1324 CDST, 1824 UTC) T Angle 5.2 SSN 7 T Angle 5.2 SSN 20 T Angle 5.2 SSN 50 T Angle 5.2 SSN 100 T Angle 5.2 SSN T Angle 7.3 SSN 7 T Angle 7.3 SSN 20 T Angle 7.3 SSN 50 T Angle 7.3 SSN 100 T Angle 7.3 SSN Take-off angles below 40 degrees are non-nvis paths
19 MUF and Take- off Angle SSN=7 to SSN=150 DAL Bryan (150 mile path - June) MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN T Angle 3.5 SSN 7 T Angle 3.5 SSN 20 T Angle 3.5 SSN 50 T Angle 3.5 SSN 100 T Angle 3.5 SSN 150 E Layer T Angle 5.2 SSN 7 T Angle 5.2 SSN 20 T Angle 5.2 SSN 50 T Angle 5.2 SSN 100 T Angle 5.2 SSN 150 F1 Layer T Angle 7.3 SSN 7 T Angle 7.3 SSN 20 T Angle 7.3 SSN 50 T Angle 7.3 SSN 100 T Angle 7.3 SSN 150 Take-off angles below 40 degrees are non-nvis paths
20 MUF and Take-off Angle SSN=7 to SSN=150 DAL San Antonio (250 mile path - June) MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN T Angle 3.5 SSN 7 T Angle 3.5 SSN 20 T Angle 3.5 SSN 50 T Angle 3.5 SSN 100 T Angle 3.5 SSN 150 E Layer F1 Layer T Angle 5.2 SSN 7 T Angle 5.2 SSN 20 T Angle 5.2 SSN 50 T Angle 5.2 SSN 100 T Angle 5.2 SSN 150 E Layer T Angle 7.3 SSN 7 T Angle 7.3 SSN 20 T Angle 7.3 SSN 50 T Angle 7.3 SSN 100 T Angle 7.3 SSN 150 Take-off angles below 40 degrees are non-nvis paths
21 MUF and Take-off Angle SSN=7 to SSN=150 DAL San Antonio (250 mile path - December) MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN T Angle 3.5 SSN 7 T Angle 3.5 SSN 20 T Angle 3.5 SSN 50 T Angle 3.5 SSN 100 T Angle 3.5 SSN 150 F1 Layer E Layer F1 Layer F1 Layer T Angle 5.2 SSN 7 T Angle 5.2 SSN 20 T Angle 5.2 SSN 50 T Angle 5.2 SSN 100 T Angle 5.2 SSN T Angle 7.3 SSN 7 T Angle 7.3 SSN 20 T Angle 7.3 SSN 50 T Angle 7.3 SSN 100 T Angle 7.3 SSN 150 Take-off angles below 40 degrees are non-nvis paths
22 MUF and T-Angle T SSN=7 to SSN=150 DAL Corpus Christi (350 mile path - June) MUF SSN 7 MUF SSN 20 MUF SSN 50 MUF SSN 100 MUF SSN T Angle 3.5 SSN 7 T Angle 3.5 SSN 20 T Angle 3.5 SSN 50 T Angle 3.5 SSN 100 T Angle 3.5 SSN 150 E Layer F1 Layer T Angle 5.2 SSN 7 T Angle 5.2 SSN 20 T Angle 5.2 SSN 50 T Angle 5.2 SSN 100 T Angle 5.2 SSN 150 E Layer T Angle 7.3 SSN 7 T Angle 7.3 SSN 20 T Angle 7.3 SSN 50 T Angle 7.3 SSN 100 T Angle 7.3 SSN 150 Take-off angles below 40 degrees are non-nvis paths
23 Relationship between MUF and Signal-Noise Ratio (SNR) For a given path, the SNR is highest at the MUF SNR decreases as the frequency is decreased below the MUF Stated another way, as the MUF rises past a given frequency, the SNR on that frequency begins to drop The amount by which the SNR drops is directly related to the amount by which the MUF exceeds the frequency
24 SNR at SSN=20 and SSN=100 - June DAL SAT: 1.8 MHz to 7.3 MHz SSN = 20 SSN = MUF SSN= MUF SSN= SNR 1.8 SSN 20 SNR 3.5 SSN 20 SNR 5.2 SSN 20 SNR 7.3 SSN 20 MUF SSN SNR 1.8 SSN 100 SNR 3.5 SSN 100 SNR 5.2 SSN 100 SNR 7.3 SSN 100 MUF SSN
25 SNR at SSN=20 and SSN=100 - December DAL SAT: 1.8 MHz to 7.3 MHz SSN = SSN = SNR 1.8 SSN 20 SNR 3.5 SSN 20 SNR 5.2 SSN 20 SNR 7.3 SSN 20 MUF SSN 20 MUF SSN= SNR 1.8 SSN 100 SNR 3.5 SSN 100 SNR 5.2 SSN 100 SNR 7.3 SSN 100 MUF SSN 100 MUF SSN=20
26 Optimized Antenna Heights for NVIS Required take-off angles range from 40 to 70 degrees for path lengths of 200 miles to 350 miles Take-off angles for shorter paths: are increasingly higher while the MUF is increasingly lower One height provides optimized coverage of NVIS 40 to 90 degree take-off angles NVIS Range of 0 to ~ 350 miles, with usable NVIS / non-nvis coverage to about 500 miles That height is 1/8 λ
27 Optimized Antenna Heights for NVIS 1/8 λ for various bands 1.8 MHz = 60 feet 3.7 MHz = 30 feet 4.6 MHz = 25 feet (MARS / CAP) 5.2 MHz = 22 feet 7.2 MHz = 16 feet MHz = 11 feet (Highest NVIS band) 14 MHz is well above NVIS frequency range /8 λ /4 λ /2 λ
28 Antenna Efficiency for NVIS: Antenna Length -- R R The length of an antenna element is the most significant factor for Radiation Resistance For a monopole, R R = h 2 /312 R R is radiation resistance in Ohms h is the antenna length in electrical degrees Typical R R for an 8 foot mobile whip at 7 MHz is 3 Ohms For a 7 MHz dipole made of two mobile whips, R R is 6 Ohms Low R R invariably means low antenna efficiency R R is in series with the coil loss ( R C ) and ground loss ( R G ) 7 MHz efficiency of a two mobile whip dipole at 16 feet is less than Your 100 Watt transmitter now equals 10 Watts or less! 10% (if lower, efficiency is much worse) 3.5 MHz efficiency of a two mobile whip dipole at 30 feet is less Your 100 Watt transmitter now equals 5 Watts or less! than 5% (if lower, efficiency is much worse) R R R C R G
29 Antenna Efficiency for NVIS: Antenna Length Broad VSWR Full Size Dipole at 16 feet Resonant at ~ feet 1 inch per side VSWR < 1.8:1 for voice portion Full Size Dipole at 16 feet Resonant at ~ feet 7 inches per side VSWR < 1.8:1 across entire band The typical mobile whip has a VSWR bandwidth of only 10 to 20 khz.
30 Antenna Efficiency for NVIS: Antenna Length Broad VSWR Full Size flat-top Dipole at 30 feet Resonant at ~ MHz 61 feet 0 inch per side VSWR < 1.8:1 from 3.81 to 3.95 MHz VSWR bandwidth = 140 khz. Full Size Vee Dipole Center at 30 feet, ends at 15 feet Now Resonant at ~ MHz 61 feet 0 inch per side VSWR < 1.8:1 from to MHz The typical mobile whip has a VSWR bandwidth of only 10 khz.
31 Antenna Efficiency for NVIS: Antenna Height A properly designed and installed NVIS antenna exhibits a gain of 3 dbd to 5 dbd at all supported take-off angles The gain and efficiency of a horizontal antenna drops drastically as it is brought near earth The effect of moving a 4 MHz half-wave dipole from 25 feet above ground ( ( 0.11 λ,, which is slightly too low) to 8 feet (0.035 λ) ) is a gain decrease of > 6 db (from > +3 dbd to -3 dbd) For a 100 Watt transmitter, that is a change from 200 Watts radiated to 50 Watts radiated! Moving the antenna lower dramatically increases ground losses, and a dramatically increases the attenuation of both transmitted and received signals Antennas are reciprocal devices: Poor TX is always poor RX A very low height full-sized dipole antenna usually has a relatively broad VSWR curve, but is shifted in resonant frequency Feedpoint resistance is increased at very low heights, but the increase is because of ground loss.
32 7 MHz Dipole at 16 Feet 4.8 dbi = 2.7 dbd 185 Watts 6.4 dbi = 4.3 dbd 270 Watts Azimuth pattern is circular within 3 db above 40 elevation
33 3.5 MHz Dipole at 30 Feet 5.1 dbi = 3.0 dbd 200 Watts 6.8 dbi = 4.7 dbd 295 Watts Azimuth pattern is circular within 2 db above 40 elevation
34 Compromise: 3.8 / 7.2 MHz Fan Vee Dipole Heights: 30 feet at Center, 15 feet at ends of 3.7 MHz elements Ends of 7.2 MHz elements are 3 feet below 3.7 MHz elements GREEN lines are antenna wires PURPLE arcs show current distribution at that frequency MHz MHz 4.4 dbd 275 Watts 3.5 dbd 225 Watts 3.8 dbd 240 Watts 2.6 dbd 180 Watts MHz MHz < 1.8:1 from to < 1.8:1 from to 3.935
35 Compromise: 3.8 / 7.2 MHz Fan Vee Dipole Heights: 30 feet at Center, 15 feet at ends of 3.7 MHz elements Ends of 7.2 MHz elements are 3 feet below 3.7 MHz elements ~ 35 feet from feedpointon 75 meter half element 75 meter half element 75 meter half element length = meter half element length = About 3 1/8 inch nyon or cotton cord 1/8 inch nyon or cotton cord End of 40 meter half element Detail of 40 Meter tie-off Only one half of antenna shown 30
36 NVIS Points to Ponder At 3.5 MHz, a full-size dipole installed at 1/8 λ: Is at very least 10 times as efficient as a two mobile whip dipole Produces transmitted signal strengths (at the distant receiver) that are 18 db to 24 db greater Provides much greater Capture Area, so received signals are much stronger than those on a two mobile whip dipole At 7 MHz, transmitted signal strengths from a full-sized dipole installed at 1/8 λ are 11 db to 18 db greater than those from the two mobile whip dipole Received signals are correspondingly stronger When I can easily deploy an antenna that radiates 185 to 300 Watts from my 100 Watt transmitter, why would I willingly deploy an antenna that makes that same transmitter equivalent to 5 or 10 Watts? Have I given myself the best chance of successful communication?
37 NVIS Summary Optimum NVIS antenna design is almost the polar opposite of DX antenna design A height of 1/8 λ results in optimum take-off angles and substantial antenna gain at those angles Placing the antenna above 1/8 λ results in lowered take- off angles that do not fully cover the required area, and in lowered gain Placing the antenna too low results in negative gain (i.e., LOSS) for both TX and RX signals Because most deployed stations will have no more than 100 Watt output, antenna efficiency is critical at ALL sites and especially for deployed stations.
38 Thank you Near Vertical Incidence Skywave (NVIS) Larry Randall WA5BEN
Copyright , Larry Randall, d/b/a The NRE Group All Rights Reserved
NEAR VERTICAL INCIDENCE SKYWAVE (NVIS) Larry Randall -WA5BEN The NRE Group larry@nregroup.net Revision: 1.6 Issue Date: 06 Nov 2014 Copyright 2007 2015, Larry Randall, d/b/a The NRE Group All Rights Reserved
More informationthe Upcoming DXpeditions? Will the Sun Cooperate for Carl Luetzelschwab K9LA SEDXC Aug 2015 K9LA 1
Will the Sun Cooperate for the Upcoming DXpeditions? Carl Luetzelschwab K9LA k9la@arrl.net http://k9la.us SEDXC Aug 2015 K9LA 1 Topics Cycle 24 and beyond Predictions for upcoming DXpeditions Bonus Trees
More informationSunrise, Sunset and Daylight in Relation to Low Band Propagation Carl Luetzelschwab K9LA January 2017
Sunrise, Sunset and Daylight in Relation to Low Band Propagation Carl Luetzelschwab K9LA January 2017 This month s column begins my 20 th year of writing monthly columns about propagation and solar topics.
More informationCCMR Educational Programs
CCMR Educational Programs Title: Date Created: August 10, 2006 Latest Revision: August 10, 2006 Author(s): Myriam Ibarra Appropriate Level: Grades 8-10 Abstract: Energy and the Angle of Insolation Sun
More informationIII. Spherical Waves and Radiation
III. Spherical Waves and Radiation Antennas radiate spherical waves into free space Receiving antennas, reciprocity, path gain and path loss Noise as a limit to reception Ray model for antennas above a
More informationA LOOK AT PROPAGATION FOR THE 2017/2018 CONTEST SEASON
A LOOK AT PROPAGATION FOR THE 2017/2018 CONTEST SEASON Frank Donovan W3LPL Carl Luetzelschwab K9LA 1 THANKS TO THE WWROF FOR SPONSORING THIS WEBINAR wwrof.org And thanks to Ken K4ZW for facilitating this
More informationEffect of Solar Flare X-Rays on digisonde fmin values. S. C. Tripathi H. Haralambous
Effect of Solar Flare X-Rays on digisonde fmin values S. C. Tripathi H. Haralambous SOLAR FLARE Solar flares occur when the sun's magnetic field twists up and reconnects, blasting energy outward and superheating
More information3. Which color of the visible light has the shortest wavelength? A) violet B) green C) yellow D) red
Name: Topic 6 Test 1. Which process is responsible for the greatest loss of energy from Earth's surface into space on a clear night? A) condensation B) conduction C) radiation D) convection 2. Base your
More informationUnderstanding Solar Indices
Understanding Solar Indices By Ken Larson KJ6RZ Long distance HF radio communications is made possible by a region of charged particles in the Earth s upper atmosphere, 30 to 200 miles above the Earth
More informationTILT, DAYLIGHT AND SEASONS WORKSHEET
TILT, DAYLIGHT AND SEASONS WORKSHEET Activity Description: Students will use a data table to make a graph for the length of day and average high temperature in Utah. They will then answer questions based
More informationIONOSPHERE By Marcel H. De Canck, ON5AU The Earth's Atmosphere
IONOSPHERE By Marcel H. De Canck, ON5AU The Earth's Atmosphere Taking a look at the neutral composition of the atmosphere around our planet, we can divide it into three main regions: the homosphere to
More informationSolutions Manual to Exercises for Weather & Climate, 8th ed. Appendix A Dimensions and Units 60 Appendix B Earth Measures 62 Appendix C GeoClock 63
Solutions Manual to Exercises for Weather & Climate, 8th ed. 1 Vertical Structure of the Atmosphere 1 2 Earth Sun Geometry 4 3 The Surface Energy Budget 8 4 The Global Energy Budget 10 5 Atmospheric Moisture
More informationME 476 Solar Energy UNIT THREE SOLAR RADIATION
ME 476 Solar Energy UNIT THREE SOLAR RADIATION Unit Outline 2 What is the sun? Radiation from the sun Factors affecting solar radiation Atmospheric effects Solar radiation intensity Air mass Seasonal variations
More informationOrbit and Transmit Characteristics of the CloudSat Cloud Profiling Radar (CPR) JPL Document No. D-29695
Orbit and Transmit Characteristics of the CloudSat Cloud Profiling Radar (CPR) JPL Document No. D-29695 Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109 26 July 2004 Revised
More informationChapter Seven. Solar Energy
Chapter Seven Solar Energy Why Studying Solar energy To know the heat gain or heat loss in a building In making energy studies In the design of solar passive homes. Thermal Radiation Solar spectrum is
More informationSolar Radiophysics with HF Radar
Solar Radiophysics with HF Radar Workshop on Solar Radiophysics With the Frequency Agile Solar Radiotelescope (FASR) 23-25 May 2002 Green Bank, WV Paul Rodriguez Information Technology Division Naval Research
More informationCTU Presents. The Fitful Rise of Solar Cycle 24 What it Means in the Coming Year. Frank Donovan W3LPL
CTU Presents The Fitful Rise of Solar Cycle 24 What it Means in the Coming Year Frank Donovan W3LPL Introduction This presentation focuses on: The four major fall and winter DX contests: CQ WW SSB and
More informationInterference Problems at the Effelsberg 100-m Telescope
Interference Problems at the Effelsberg 100-m Telescope Wolfgang Reich Max-Planck-Institut für Radioastronomie, Bonn Abstract: We summarise the effect of interference on sensitive radio continuum and polarisation
More informationC) the seasonal changes in constellations viewed in the night sky D) The duration of insolation will increase and the temperature will increase.
1. Which event is a direct result of Earth's revolution? A) the apparent deflection of winds B) the changing of the Moon phases C) the seasonal changes in constellations viewed in the night sky D) the
More informationHOW TO SOLVE YOUR ANTENNA MATCHING PROBLEMS
HOW TO SOLVE YOUR ANTENNA MATCHING PROBLEMS John Sexton, G4CNN. Reprinted from Echelford Amateur Radio Society Newsletter for November 1978. Introduction. In January 1977 there appeared in RADCOM an article
More informationEarth is tilted (oblique) on its Axis!
MONDAY AM Radiation, Atmospheric Greenhouse Effect Earth's orbit around the Sun is slightly elliptical (not circular) Seasons & Days Why do we have seasons? Why aren't seasonal temperatures highest at
More informationLaboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons and Daily Weather
Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons and Daily Weather page - Section A - Introduction: This lab consists of questions dealing with atmospheric science. We beginning
More information(1) How does the annual average sun angle at solar noon (that is, the sun angle at noon averaged over a full year) depend on latitude?
(1) How does the annual average sun angle at solar noon (that is, the sun angle at noon averaged over a full year) depend on latitude? (A) * As latitude increases, average sun angle at solar noon decreases.
More informationEE Properties of Sunlight. Y. Baghzouz Professor of Electrical Engineering
EE 495-695 2.2 Properties of Sunlight Y. Baghzouz Professor of Electrical Engineering Azimuth angle The azimuth angle is the compass direction from which the sunlight is coming. At the equinoxes, the sun
More informationFor most observers on Earth, the sun rises in the eastern
632 CHAPTER 25: EARTH, SUN, AND SEASONS WHAT IS THE SUN S APPARENT PATH ACROSS THE SKY? For most observers on Earth, the sun rises in the eastern part of the sky. The sun reaches its greatest angular altitude
More informationPractice Questions: Seasons #1
1. Seasonal changes on Earth are primarily caused by the A) parallelism of the Sun's axis as the Sun revolves around Earth B) changes in distance between Earth and the Sun C) elliptical shape of Earth's
More informationMeasurements of the DL0SHF 8 GHz Antenna
Measurements of the DL0SHF 8 GHz Antenna Joachim Köppen, DF3GJ Inst.Theoret.Physik u.astrophysik, Univ. Kiel September 2015 Pointing Correction Position errors had already been determined on a few days
More informationMIDTERM PRACTICE EXAM ANSWERS
MIDTERM PRACTICE EXAM ANSWERS 1. (2) Location B shows that the altitude of the noon Sun increases between Dec 21. and June 21. Location B also shows that the Dec. 21 noon Sun is at an altitude of approximately
More information(1) Over the course of a day, the sun angle at any particular place varies. Why?
(1) Over the course of a day, the sun angle at any particular place varies. Why? (Note: Although all responses below are true statements, only one of them actually explains the observation!) (A)The sun
More informationPropagation Topics Cycle 24
Propagation Topics Cycle 24 Carl Luetzelschwab K9LA k9la@arrl.net Agenda Recent Cycle 24 data Cycle 24 Predictions Cycle 24 FAQs Waller Flag observations Anomalies in the F 2 region more propagation in
More informationLab 2. Characterization of Solar Cells
Lab 2. Characterization of Solar Cells Physics Enhancement Programme Department of Physics, Hong Kong Baptist University 1. OBJECTIVES To familiarize with the principles of commercial solar cells To characterize
More informationComputer Activity #3 SUNRISE AND SUNSET: THE SEASONS
NAME(S)!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! ASTRONOMY 25 Computer Activity #3 SUNRISE AND SUNSET: THE SEASONS SECTION DAY/TIME S. V. LLOYD Overview The seasonal variation in temperature is due to two changes
More informationE-JUST s Sample Entrance Exam Faculty of Engineering
E-JUST s Sample Entrance Exam Faculty of Engineering PHYSICS Time: 1 hr Choose the right answer: 1. Three equal resistors connected in series across a source e.m.f. together dissipate 10 watt. If the same
More informationStudent Exploration: Seasons in 3D
Name: Date: Student Exploration: Seasons in 3D Vocabulary: axis, equinox, latitude, Northern Hemisphere, revolve, rotate, solar energy, solar intensity, Southern Hemisphere, summer solstice, winter solstice
More informationLaboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons
Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons page - 1 Section A - Introduction: This lab consists of both computer-based and noncomputer-based questions dealing with atmospheric
More informationWhich Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N
1. In which list are the forms of electromagnetic energy arranged in order from longest to shortest wavelengths? A) gamma rays, x-rays, ultraviolet rays, visible light B) radio waves, infrared rays, visible
More informationWhich graph best shows the relationship between intensity of insolation and position on the Earth's surface? A) B) C) D)
1. The hottest climates on Earth are located near the Equator because this region A) is usually closest to the Sun B) reflects the greatest amount of insolation C) receives the most hours of daylight D)
More information1. (P2.2D) Describe the acceleration and speed of an object that is experiencing uniform circular motion.
UNIT 5 Periodic Motion P2.2D P3.4D P3.6B P3.6d P3.6e P2.1h P2.2f State that uniform circular motion involves acceleration without a change in speed. Identify the force(s) acting on objects moving with
More informationRADIATING ELEMENTS MAY BE: DIPOLES, SLOTS, POLYRODS, LOOPS, HORNS, HELIX, SPIRALS, LOG PERIODIC STRUCTURES AND EVEN DISHES Dipoles simple structures,
ANTENNA ARRAYS Array - collection of radiating elements An array may be: 1D (linear), 2D (planar), 3D (frequency selective) structure of radiating elements Purpose More directivity, Steereable beams Radiation
More informationPage 1. Name:
Name: 1) What is the primary reason New York State is warmer in July than in February? A) The altitude of the noon Sun is greater in February. B) The insolation in New York is greater in July. C) The Earth
More informationQuestions you should be able to answer after reading the material
Module 4 Radiation Energy of the Sun is of large importance in the Earth System, it is the external driving force of the processes in the atmosphere. Without Solar radiation processes in the atmosphere
More informationExercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION
Exercise 6 Solar Panel Orientation EXERCISE OBJECTIVE When you have completed this exercise, you will understand how the solar illumination at any location on Earth varies over the course of a year. You
More information1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely
CHAPTER 3 SOLAR AND TERRESTRIAL RADIATION MULTIPLE CHOICE QUESTIONS 1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely 2. is the distance between successive
More informationLecture 34: MON 13 APR Ch ,5
Physics 2102 Jonathan Dowling James Clerk Maxwell (1831-1879) Lecture 34: MON 13 APR Ch.33.1 3,5 3,5 7: E&M Waves MT03 Avg: 65/100 Q1/P3 K. Schafer Office hours: MW 1:30-2:30 pm 222B Nicholson P1/Q2 J.
More information5. In which diagram is the observer experiencing the greatest intensity of insolation? A) B)
1. Which factor has the greatest influence on the number of daylight hours that a particular Earth surface location receives? A) longitude B) latitude C) diameter of Earth D) distance from the Sun 2. In
More informationWireless Communications
NETW701 Wireless Communications Dr. Wassim Alexan Winter 2018 Lecture 2 NETW705 Mobile Communication Networks Dr. Wassim Alexan Winter 2018 Lecture 2 Wassim Alexan 2 Reflection When a radio wave propagating
More informationIntroduction to Space Weather and Propagation
Introduction to Space Weather and Propagation Carl Luetzelschwab K9LA ARRL Vice Director, Central Division k9la@arrl.net https://k9la.us K9LA 1 What Is Space Weather? Space weather is the quiet Sun Electromagnetic
More informationChapter 31 Maxwell s Equations and Electromagnetic Waves. Copyright 2009 Pearson Education, Inc.
Chapter 31 Maxwell s Equations and Electromagnetic Waves Units of Chapter 31 Changing Electric Fields Produce Magnetic Fields; Ampère s Law and Displacement Current Gauss s Law for Magnetism Maxwell s
More information1. The diagram below represents Earth and the Moon as viewed from above the North Pole. Points A, B, C, and D are locations on Earth's surface.
1. The diagram below represents Earth and the Moon as viewed from above the North Pole. Points A, B, C, and D are locations on Earth's surface. 2. The graph below shows the change in tide heights of the
More informationAgricultural Science Climatology Semester 2, Anne Green / Richard Thompson
Agricultural Science Climatology Semester 2, 2006 Anne Green / Richard Thompson http://www.physics.usyd.edu.au/ag/agschome.htm Course Coordinator: Mike Wheatland Course Goals Evaluate & interpret information,
More informationProblem set 3. Electromagnetic waves
Second Year Electromagnetism Michaelmas Term 2017 Caroline Terquem Problem set 3 Electromagnetic waves Problem 1: Poynting vector and resistance heating This problem is not about waves but is useful to
More informationLESSON PLAN - Optimum Orientation of Solar Panels Using Soltrex Data
LESSON PLAN - Optimum Orientation of Solar Panels Using Soltrex Data Title of Lesson: Optimum Orientation of Solar Panels Using Soltrex Data Description of class: High School physics, astronomy, or environmental
More informationChapter 4 Layered Substrates 4.1 Introduction
Chapter 4 Layered Substrates 4.1 Introduction The significant result of the previous chapter is that guided mode (surface wave) losses can be avoided on substrates with thicknesses of an odd integral multiple
More informationDO STRATWARMS AFFECT 160M PROPAGATION? A Look at the North America to Europe Path
DO STRATWARMS AFFECT 160M PROPAGATION? A Look at the North America to Europe Path by Carl Luetzelschwab K9LA (this article appeared in the January 1998 issue of The Low Band Monitor) Stratwarms (stratospheric
More information6 - Planetarium. Q1) In what cardinal direction did the Sun rise? Be specific. Q2) Record the time of sunrise and sunset: /
Name: Partner(s), if applicable: 6 - Planetarium ASTR110L Purpose: To experience the motion of the Sun and the night sky at different times and different locations on Earth. Answer the questions in the
More informationApplication of polar cap absorption events to the calibration of riometer systems
RADIO SCIENCE, VOL. 37, NO. 3, 1035, 10.1029/2001RS002465, 2002 Application of polar cap absorption events to the calibration of riometer systems J. K. Hargreaves Department of Communication Systems, University
More informationResonant Matching Networks
Chapter 1 Resonant Matching Networks 1.1 Introduction Frequently power from a linear source has to be transferred into a load. If the load impedance may be adjusted, the maximum power theorem states that
More informationEnergy and Insolation Review 2
Energy and Insolation Review 2 The diagram below shows a container of water that is being heated. 1. The movement of water shown by the arrows is most likely caused by (1) density differences (2) insolation
More informationEnergy and Seasons A B1. 9. Which graph best represents the general relationship between latitude and average surface temperature?
Energy and Seasons A B1 1. Which type of surface absorbs the greatest amount of electromagnetic energy from the Sun? (1) smooth, shiny, and light colored (2) smooth, shiny, and dark colored (3) rough,
More informationThis page intentionally left blank!
This page intentionally left blank! Solar-Terrestrial Data Available on the k4msu.com Website The original title was going to be... Is KK4BKD a Spy Using k4msu.com to Send Secret Messages? Or, what else
More informationPRINCIPLES OF REMOTE SENSING. Electromagnetic Energy and Spectral Signatures
PRINCIPLES OF REMOTE SENSING Electromagnetic Energy and Spectral Signatures Remote sensing is the science and art of acquiring and analyzing information about objects or phenomena from a distance. As humans,
More informationPractice Seasons Moon Quiz
1. Which diagram represents the tilt of Earth's axis relative to the Sun's rays on December 15? A) B) C) D) 2. The diagram below represents Earth in space on the first day of a season. 5. Base your answer
More informationSome Remarks on Shielding. Herbert Kapitza (FLA) (using slides from a talk by Mike Thuot) DESY,
Some Remarks on Shielding Herbert Kapitza (FLA) (using slides from a talk by Mike Thuot) DESY, 09.10.2006 A shield may be used to confine the radiated field from a noise source. Shields are metallic partitions
More informationC) wavelength C) eastern horizon B) the angle of insolation is high B) increases, only D) thermosphere D) receive low-angle insolation
1. What is the basic difference between ultraviolet, visible, and infrared radiation? A) half-life B) temperature C) wavelength D) wave velocity 2. In New York State, the risk of sunburn is greatest between
More informationAT350 EXAM #1 September 23, 2003
AT350 EXAM #1 September 23, 2003 Name and ID: Enter your name and student ID number on the answer sheet and on this exam. Record your answers to the questions by using a No. 2 pencil to completely fill
More informationSolar photovoltaic energy production comparison of east, west, south-facing and tracked arrays
The Canadian Society for Bioengineering The Canadian society for engineering in agricultural, food, environmental, and biological systems. La Société Canadienne de Génie Agroalimentaire et de Bioingénierie
More informationRAPID growth in satellite-communications and mobile-communications
Calculate The Uncertainty Of N Measurements Simple modifications to the basic noise-figure equations can help in predicting uncertainties associated with test equipment. Duncan Boyd Senior Hardware Development
More informationAnswer Key for Exam C
Answer Key for Exam C 1 point each Choose the answer that best completes the question. Read each problem carefully and read through all the answers. Take your time. If a question is unclear, ask for clarification
More informationAnswer Key for Exam B
Answer Key for Exam B 1 point each Choose the answer that best completes the question. Read each problem carefully and read through all the answers. Take your time. If a question is unclear, ask for clarification
More informationChapter 31 Maxwell s Equations and Electromagnetic Waves. Copyright 2009 Pearson Education, Inc.
Chapter 31 Maxwell s Equations and Electromagnetic Waves Units of Chapter 31 Changing Electric Fields Produce Magnetic Fields; Ampère s Law and Displacement Current Gauss s Law for Magnetism Maxwell s
More informationCLASSICS. Handbook of Solar Radiation Data for India
Solar radiation data is necessary for calculating cooling load for buildings, prediction of local air temperature and for the estimating power that can be generated from photovoltaic cells. Solar radiation
More informationLecture # 04 January 27, 2010, Wednesday Energy & Radiation
Lecture # 04 January 27, 2010, Wednesday Energy & Radiation Kinds of energy Energy transfer mechanisms Radiation: electromagnetic spectrum, properties & principles Solar constant Atmospheric influence
More informationSunlight and its Properties Part I. EE 446/646 Y. Baghzouz
Sunlight and its Properties Part I EE 446/646 Y. Baghzouz The Sun a Thermonuclear Furnace The sun is a hot sphere of gas whose internal temperatures reach over 20 million deg. K. Nuclear fusion reaction
More informationSOLAR GEOMETRY (AND SOLAR RADIATION)
SOLAR GEOMETRY (AND SOLAR RADIATION) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 1 Solar Radiation Components glass will reflect some incoming radiation; absorb some; and transmit some SHGF
More informationSolutions to Lab Exercise #2: Solar Radiation & Temperature Part II: Exploring & Interpreting Data
METR 104: Our Dynamic Weather (w/lab) Solutions to Lab Exercise #2: Solar Radiation & Temperature Part II: Exploring & Interpreting Data (10 points) Dr. Dave Dempsey Dept. of Geosciences SFSU, Spring 2013
More informationHeat Transfer. Energy from the Sun. Introduction
Heat Transfer Energy from the Sun Introduction The sun rises in the east and sets in the west, but its exact path changes over the course of the year, which causes the seasons. In order to use the sun
More informationMarch 21. Observer located at 42 N. Horizon
March 21 Sun Observer located at 42 N Horizon 48 June 21 March 21 A 48 90 S 23.5 S 0 23.5 N 42 N 90 N Equator (June 21) C (March 21) B A 71.5 48 Horizon 24.5 Observer Sun 40 Observer Sun 22 Observer Sun
More informationQuest Chapter 28. Remember: We see by color addition. How do we get white with color addition? So, is it a color?
1 Why do we not list black and white as colors? 1. People usually think black and white should only reflect dark and light in a image. They cannot represent the colorful world. 2. Black should not be regarded
More informationSunlight and its Properties II. EE 446/646 Y. Baghzouz
Sunlight and its Properties II EE 446/646 Y. Baghzouz Solar Time (ST) and Civil (clock) Time (CT) There are two adjustments that need to be made in order to convert ST to CT: The first is the Longitude
More informationAdvanced Electronic Communication Systems. Lecture 4. Satellite Orbits (2) Dr.Eng. Basem ElHalawany
Advanced Electronic Communication Systems Lecture 4 Satellite Orbits (2) Dr.Eng. Basem ElHalawany Orbital (nonsynchronous) Satellites (cont.) Posigrade orbit or Prograde: If the satellite is orbiting in
More informationa. 0.5 AU b. 5 AU c. 50 AU d.* AU e AU
1 AST104 Sp04: WELCOME TO EXAM 1 Multiple Choice Questions: Mark the best answer choice. Read all answer choices before making selection. (No credit given when multiple answers are marked.) 1. A galaxy
More informationShielding Tutorial Gentex EME Lab
Shielding Tutorial Gentex EME Lab Shielding Course Outline: I. Why do we need shields? II. III. IV. Introduction to the Basic Shield Design Process A. Apertures B. Materials Corrosion Summations and Conclusions
More informationThe inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy
Energy Balance The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy Balance Electromagnetic Radiation Electromagnetic
More informationEarth-Sun Relationships. The Reasons for the Seasons
Earth-Sun Relationships The Reasons for the Seasons Solar Radiation The earth intercepts less than one two-billionth of the energy given off by the sun. However, the radiation is sufficient to provide
More informationYOUR NAME Sample Final Physics 1404 (Dr. Huang)), Correct answers are underlined.
YOUR NAME Sample Final Physics 1404 (Dr. Huang)), Correct answers are underlined. Useful constants: e=1.6 10-19 C, m e =9.1 10-31 kg, m p =1.67 10-27 kg, ε 0 =8.85 10-12 C 2 /N m 2, c=3 10 8 m/s k e =8.99
More informationTime Series Model of Photovoltaic Generation for Distribution Planning Analysis. Jorge Valenzuela
Time Series Model of Photovoltaic Generation for Distribution Planning Analysis Jorge Valenzuela Overview Introduction: The solar problem and our limitations Modeling What information do we have? Solar
More informationIn the News: &id= &m=
In the News: http://www.npr.org/templates/player/mediaplayer.html?action=1&t=1&islist=false &id=112755481&m=112805055 1 In the News: http://www.economist.com/scien cetechnology/displaystory.cfm?st ory_id=14302001
More information1 2 3 US Air Force 557 th Weather Wing maintains a website with many operational products both on terrestrial as on space weather. The operational holy grail for the military are stoplight charts, indicating
More informationqq k d Chapter 16 Electric and Magnetic Forces Electric charge Electric charges Negative (electron) Positive (proton)
Chapter 16 Electric and Magnetic Forces Electric charge Electric charges Negative (electron) Positive (proton) Electrons and protons in atoms/molecules Ions: atoms/molecules with excess of charge Ions
More informationSolar Time, Angles, and Irradiance Calculator: User Manual
Solar Time, Angles, and Irradiance Calculator: User Manual Circular 674 Thomas Jenkins and Gabriel Bolivar-Mendoza 1 Cooperative Extension Service Engineering New Mexico Resource Network College of Agricultural,
More informationCOMPARISON BETWEEN THE MEASURED AND PREDICTED PARAMETERS OF HF RADIO SIGNALS PROPAGATING ALONG THE MID-LATITUDE TROUGH AND
COMPARISON BETWEEN THE MEASURED AND PREDICTED PARAMETERS OF HF RADIO SIGNALS PROPAGATING ALONG THE MID-LATITUDE TROUGH AND WITHIN THE POLAR CAP A.J. Stocker, E.M. Warrington, and D.R. Siddle Department
More informationHEATING THE ATMOSPHERE
HEATING THE ATMOSPHERE Earth and Sun 99.9% of Earth s heat comes from Sun But
More informationPerformance of Antenna Measurement Setup
Performance of Antenna Measurement Setup Raul Monsalve SESE, Arizona State University November 27, 213 2 Description This report is divided into two parts: PART 1: Check of recovered instrumental S-parameters
More informationIntroduction to Acoustics Exercises
. 361-1-3291 Introduction to Acoustics Exercises 1 Fundamentals of acoustics 1. Show the effect of temperature on acoustic pressure. Hint: use the equation of state and the equation of state at equilibrium.
More informationCOMBINING GTD WITH MOM IN ANALYSING THE SCATTERING FROM THE LICEF ANTENNAS ON THE SMOS SATELLITE
Paper presented at European Conference on Antennas and Propagation (EuCAP 2006), Nice, France, November 6-10, 2006, 5 pages. COMBINING GTD WITH MOM IN ANALYSING THE SCATTERING FROM THE LICEF ANTENNAS ON
More informationFor further information, and additional background on the American Meteorological Society s Education Program, please contact:
Project ATMOSPHERE This guide is one of a series produced by Project ATMOSPHERE, an initiative of the American Meteorological Society. Project ATMOSPHERE has created and trained a network of resource agents
More informationWhat Is the Relationship Between Earth s Tilt and the Seasons?
Learning Set 2 Why Are There Differences in Temperature? Review Images and Graphics While reading about Earth s tilt and the seasons, pay particular attention to the graphics included. How do they help
More informationGrade 6 Standard 2 Unit Test Astronomy
Grade 6 Standard 2 Unit Test Astronomy Multiple Choice 1. Why does the air temperature rise in the summer? A. We are closer to the sun. B. The air becomes thicker and more dense. C. The sun s rays are
More informationHow to Adapt Your DX Contest Strategies for Low Solar Activity
How to Adapt Your DX Contest Strategies for Low Solar Activity How to Adapt Your DX Contest Strategies for Low Solar Activity Frank Donovan W3LPL Very Low Solar Activity through 2021 solar activity should
More informationPropagation Planning for Contests Using Propagation Predictions to Develop a Band Plan Carl Luetzelschwab K9LA
Propagation Planning for Contests Using Propagation Predictions to Develop a Band Plan Carl Luetzelschwab K9LA Propagation planning for a contest effort is quite similar to propagation planning for a DXpedition
More information